radioactive cesium accumulation in seaweeds by the fukushima 1 nuclear power plant accident—two...

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JPR SYMPOSIUM Current status and future control of cesium contamination in plants and algae in Fukushima Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity Hiroshi Kawai Akira Kitamura Mari Mimura Tetsuro Mimura Tomoya Tahara Daiki Aida Kenji Sato Hideaki Sasaki Received: 31 July 2013 / Accepted: 25 September 2013 / Published online: 6 December 2013 Ó The Botanical Society of Japan and Springer Japan 2013 Abstract Accumulations of radionuclides in marine macroalgae (seaweeds) resulting from the Fukushima 1 Nuclear Power Plant (F1NPP) accident in March 2011 have been monitored for two years using high-purity germanium detectors. Algal specimens were collected seasonally by snorkeling at Nagasaki, Iwaki, Fukushima Prefecture (Pref.), Japan, ca. 50 km perimeter from the F1NPP. Additional collections were done at Soma, Hironocho, Hisanohama and Shioyazaki in Fukushima Pref. as well as at Chiba Pref. and Hyogo Pref. as controls. In May 2011, specimens of most macroalgal species showed 137 Cs levels greater than 3,000 Bq kg -1 at Shioyazaki and Nagasaki. The highest 137 Cs level recorded 7371.20 ± 173.95 Bq kg -1 in Undaria pinnatifida (Harvey) Suringar on 2 May 2011, whereas seawater collected at the same time at Shioyazaki and Nagasaki measured 8.41 ± 3.21 and 9.74 ± 3.43 Bq L -1 , respectively. The concentration fac- tor of marine macroalgae was estimated to be ca. 8–50, depending on taxa and considering a weight ratio of wet/ dry samples of ca. 10. 137 Cs level declined remarkably during the following 5–6 months. In contrast, the 137 Cs level remained rather stable during the following 12–16 months, and maintained the range of 10–110 Bq kg -1 . Contamination was still detectable in many samples in March 2013, 24 months after the most significant pollution. Keywords 134 Cs Á 137 Cs Á F1NPP Á 40 K Á Radionuclide accumulation Á Seaweeds Introduction Radioactive contamination of the coastal seawater fol- lowing the Fukushima 1 Nuclear Power Plant (F1NPP) accident was the most significant artificial radioactive liquid release into the sea ever known, on a short time and space scale basis (Buesseler et al. 2011; Linsley et al. 2005). The amount of radionuclides discharged from the F1NPP immediate after the accident was estimated to be 5–10 PBq to the atmosphere and 3–6 PBq to the sea, the latter being caused by direct leakages of the contaminated cooling water (Estournel et al. 2012; Kawamura et al. 2011; Miyazawa et al. 2012; Tsumune et al. 2012). The seawater contamination has become severe by (1) a deposition from an atmospheric contamination plume, (2) direct, artificial releases of highly contaminated waters into the sea, and (3) the transport of radiopollutants into the sea by surface water leaching through contaminated soil or by Fukushima Daiichi Nuclear Power Station is cited as Fukushima 1 Nuclear Power Plant in the present manuscript. H. Kawai (&) Kobe University Research Center for Inland Seas, Rokkodai, Nadaku, Kobe 657-8501, Japan e-mail: [email protected] A. Kitamura Graduate School of Maritime Science, Fukae, Higashinada, Kobe 658-0022, Japan M. Mimura Á T. Mimura Graduate School of Science, Kobe University Rokkodai, Rokkodai, Nadaku, Kobe 657-8501, Japan T. Tahara Iwaki Community Reconstruction Center, Iwaki Meisei University, Iwaki, Fukushima 970-8551, Japan D. Aida Á K. Sato Á H. Sasaki Faculty of Science and Technology, Iwaki Meisei University, Iwaki, Fukushima 970-8551, Japan 123 J Plant Res (2014) 127:23–42 DOI 10.1007/s10265-013-0603-1

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Page 1: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

JPR SYMPOSIUM Current status and future control of cesium contaminationin plants and algae in Fukushima

Radioactive cesium accumulation in seaweeds by the Fukushima 1Nuclear Power Plant accident—two years’ monitoring at Iwakiand its vicinity

Hiroshi Kawai • Akira Kitamura • Mari Mimura •

Tetsuro Mimura • Tomoya Tahara •

Daiki Aida • Kenji Sato • Hideaki Sasaki

Received: 31 July 2013 / Accepted: 25 September 2013 / Published online: 6 December 2013

� The Botanical Society of Japan and Springer Japan 2013

Abstract Accumulations of radionuclides in marine

macroalgae (seaweeds) resulting from the Fukushima 1

Nuclear Power Plant (F1NPP) accident in March 2011 have

been monitored for two years using high-purity germanium

detectors. Algal specimens were collected seasonally by

snorkeling at Nagasaki, Iwaki, Fukushima Prefecture

(Pref.), Japan, ca. 50 km perimeter from the F1NPP.

Additional collections were done at Soma, Hironocho,

Hisanohama and Shioyazaki in Fukushima Pref. as well as

at Chiba Pref. and Hyogo Pref. as controls. In May 2011,

specimens of most macroalgal species showed 137Cs levels

greater than 3,000 Bq kg-1 at Shioyazaki and Nagasaki.

The highest 137Cs level recorded 7371.20 ± 173.95

Bq kg-1 in Undaria pinnatifida (Harvey) Suringar on 2

May 2011, whereas seawater collected at the same time at

Shioyazaki and Nagasaki measured 8.41 ± 3.21 and

9.74 ± 3.43 Bq L-1, respectively. The concentration fac-

tor of marine macroalgae was estimated to be ca. 8–50,

depending on taxa and considering a weight ratio of wet/

dry samples of ca. 10. 137Cs level declined remarkably

during the following 5–6 months. In contrast, the 137Cs

level remained rather stable during the following 12–16

months, and maintained the range of 10–110 Bq kg-1.

Contamination was still detectable in many samples

in March 2013, 24 months after the most significant

pollution.

Keywords 134Cs � 137Cs � F1NPP � 40K �Radionuclide accumulation � Seaweeds

Introduction

Radioactive contamination of the coastal seawater fol-

lowing the Fukushima 1 Nuclear Power Plant (F1NPP)

accident was the most significant artificial radioactive

liquid release into the sea ever known, on a short time and

space scale basis (Buesseler et al. 2011; Linsley et al.

2005). The amount of radionuclides discharged from the

F1NPP immediate after the accident was estimated to be

5–10 PBq to the atmosphere and 3–6 PBq to the sea, the

latter being caused by direct leakages of the contaminated

cooling water (Estournel et al. 2012; Kawamura et al.

2011; Miyazawa et al. 2012; Tsumune et al. 2012).

The seawater contamination has become severe by (1) a

deposition from an atmospheric contamination plume, (2)

direct, artificial releases of highly contaminated waters into

the sea, and (3) the transport of radiopollutants into the sea

by surface water leaching through contaminated soil or by

Fukushima Daiichi Nuclear Power Station is cited as Fukushima 1

Nuclear Power Plant in the present manuscript.

H. Kawai (&)

Kobe University Research Center for Inland Seas, Rokkodai,

Nadaku, Kobe 657-8501, Japan

e-mail: [email protected]

A. Kitamura

Graduate School of Maritime Science, Fukae, Higashinada,

Kobe 658-0022, Japan

M. Mimura � T. Mimura

Graduate School of Science, Kobe University Rokkodai,

Rokkodai, Nadaku, Kobe 657-8501, Japan

T. Tahara

Iwaki Community Reconstruction Center, Iwaki Meisei

University, Iwaki, Fukushima 970-8551, Japan

D. Aida � K. Sato � H. Sasaki

Faculty of Science and Technology, Iwaki Meisei University,

Iwaki, Fukushima 970-8551, Japan

123

J Plant Res (2014) 127:23–42

DOI 10.1007/s10265-013-0603-1

Page 2: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

river systems. The first case was most serious during mid-

March 2011, and the second from late March to early April

2011. The contaminated seawater may be diluted or has

been transported offshore by currents. Along the coast,

however, a significant portion of the radioactive Cs and

other radioactive substances are believed to have been

absorbed by coastal organisms or bound to suspended

particles, causing a deposition of radiopolluted sediments

on the sea bottom. The concentration of radionuclides

reached the maximum in mid-April 2011, but it thereafter

declined exponentially. However, in addition to the inflow

through the river systems, artificial release of radionuclides

from F1NPP is reported to have continued at least until

2012 (Kanda 2013).

Among the radionuclides discharged by the accident, the

effects of 134Cs and 137Cs are most serious because of their

high levels and long decay periods. These radionuclides are

considered to most substantially contribute to the contam-

ination of marine organisms due to the contaminated sea-

water. Marine macroalgae (so-called seaweeds) grow by

absorbing nutrient salts and other minerals directly from

seawater at the surface of their thalli. Cs? is soluble in

seawater, and algal cells are thought to absorb Cs? through

certain K? transporters (Kanter et al. 2010; Zhu and

Smolders 2000), resulting in Cs? accumulation within the

cells.

The concentration factors (CFs) of marine macroalgae

for 137Cs were reported to vary considerably from species

to species (Coughtrey and Thorne 1983; Pentreath 1976;

Tateda and Koyanagi 1994), but IAEA (2004) recom-

mended the value of 50. Marine macroalgae may also

capture the ions in phycocolloids such as alginate, fucan,

agar, and carrageenan, although the affinity of Cs? for

these phycocolloids is not well-established (Morris et al.

1980). Marine macroalgae are primary producers in

coastal ecosystems, and diverse benthic animals as well as

fishes feed on them. Therefore, the radioactive contami-

nation of marine macroalgae will be transferred to con-

sumer animals through the food chain, and may become

concentrated by biological accumulation.

Prior to the accident, the concentrations of 137Cs in the

surface water of the Pacific Ocean were in the range of

1–4 Bq m-3 (Ikeuchi 2003; Nakanishi et al. 2010; Povinec

et al. 2004), which mainly resulted from global fallout due

to atmospheric nuclear weapon tests. Tateda and Koyanagi

(1994) have reported the background concentrations of137Cs in representative green, red and brown marine mac-

roalgae, e.g. Ulva pertusa Kjellman, Neodilsea yendoana

Tokida, Saccharina religiosa (Miyabe) C.E. Lane, C.

Mayes, Druehl & G.W. Saunders (=Laminaria religiosa

Miyabe), Sargassum horneri (Turner) C. Agardh, S. thun-

bergii (Mertens ex Roth) Kuntze, in the range of ca.

0.03–037 Bq kg wet weight-1. Later, Morita et al. (2010)

have compared the level of 90Sr and 137Cs in Undaria

pinnatifida collected from three representative areas

(Nagasaki Pref., Kanagawa Pref. and Niigata Pref.) in

Japan and in Saccharina longissima (Miyabe) C.E. Lane,

C. Mayes, Druehl & G.W. Saunders (=Laminaria longiss-

ima Miyabe) from Hokkaido during a 1998–2008 period

and reported 137Cs levels of 0.03–0.08 and

0.05–0.09 Bq kg wet weight-1 for U. pinnatifida and

S. longissima, respectively. Morita et al. (2010) also

compared concentrations of 90Sr and 137Cs in some addi-

tional kelp and Sargassum species and reported 137Cs

concentrations of 0.02–0.34 kg wet weight-1.

Several agencies have conducted investigations to

measure the radioactive quantities of major fishery organ-

isms after the F1NPP accident. Some algal taxa have been

included in the target species, e.g., Pyropia (Porphyra),

Saccharina (Laminaria), Eisenia, Gloiopeltis, Monostro-

ma, but the number of species was rather limited, and

rather biased in respect to phylogenetic diversity, habitat,

and life history (e.g., intertidal vs. subtidal, annual vs.

perennial). In addition, measurement protocols were not

standardized among the investigations, and the detection

levels were sometimes rather high (e.g., [ 20 Bq kg-1 for

fresh specimens: http://www.jfa.maff.go.jp/e/inspection/

index.html) depending on the available facilities. There-

fore, it was difficult to compare the data to clarify the

general fate of radioactive contamination in marine mac-

roalgae, and to discuss the differences in the CFs for ra-

dionuclides among the taxa.

In the present study, we aimed to monitor the level of

radionuclides including 134Cs, 137Cs and 40K based on a

standardized protocol using high-purity germanium detec-

tors and to undertake multi-seasonal sampling as much as

possible.

Materials and methods

Specimens were seasonally collected by snorkeling at

Nagasaki, Fukushima Pref., ca. 50 km distant from the

F1NPP (Fig. 1). Additional specimens were collected at the

following localities: Hironocho, Hisanohama, Shioyazaki

and Soma (Fukushima Pref.); Iwanuma (Miyagi Pref.);

Kamogawa and Katsuura (Chiba Pref.); and Iwaya (Hyogo

Pref.) (Fig. 1). The list of the specimens is shown in Table 1

(measurements made at Kobe University) and Table 2

(measurements made at Iwaki Meisei University).

For the measurements at Kobe University, sorted spec-

imens were identified based on their morphology, prelim-

inarily air-dried overnight using a fan at room temperature,

and then dried in an oven at 90–100 �C for 8 h. The weight

ratios of wet/dry samples were roughly 10, and this value

was used in the comparisons of literature data based on wet

24 J Plant Res (2014) 127:23–42

123

Page 3: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

samples, and concentration factors. Dried specimens were

preliminarily broken into fragments manually, and powdered

using a blender (Waring J-SPEC 7011BUJ, Conair Corp.,

Stamford, CT, USA). Powdered specimens were packed in

U-8 sample cups (56 mm ø and 68 mm high) and used for

measurement. The protocol of radioactivity measurements is

described in Mimura et al. (2014). In Tables 1 and 2, ‘‘Error’’

is the overall error estimated by the analyzing software from

systematic errors in the system together with the standard

deviation of the counting. Seawaters collected at the coasts of

Nagasaki and Shioyazaki in May 2011 were filled in U-8

sample cups and used for measurements without evaporation.

For the measurements at Iwaki Meisei University, sorted

specimens were identified based on their morphology,

washed with fresh water and pre-dried at room tempera-

ture. Dried specimens were desiccated in an oven at 60 �C

for 48 h, powdered using a blender, and packed in U-8

sample cups. 134Cs and 137Cs were measured using a

GEM40P4-76 germanium detector (Seiko EG & G, Tokyo,

Japan) following the manufacturer’s instructions.

The first collections (May 2011) of the macroalgal

specimens were kept frozen at -20 �C until drying.

However, this protocol resulted in some loss of radioac-

tivity in meltwater (dripping). Accordingly, in order to

assess the loss of radioactivity during thawing, some

specimens (collected in July 2011) were either frozen

before drying or directly dried, and the radioactivity was

compared between these drying protocols. In addition, the

radioactivity of the meltwater obtained from the thawed

specimens was also measured.

Statistical problems

In some radioactivity measurements, such as for macroal-

gal samples, we could not obtain a sufficient amount of

samples that allow us to ensure statistical reliance of the

measurement. There was also a limitation in the total

running time on a germanium detector. In other cases, the

total volume of collected samples was not large enough to

fill the U-8 sample cup, resulting in rather low detection

signals. For all these experiments, only data are presented

with notification that the precision of data was not statis-

tically tested.

Results

The 134Cs:137Cs ratios of examined specimens were plotted

according to time series (Fig. 2). The ratio reduced to ca.

0.6 after two years, which agreed well with the expected

value by natural decay (0.79 after one year, and 0.64 after

two years).

Results of the measurements at Kobe University (134Cs,137Cs and 40K) and Iwaki Meisei University (134Cs and137Cs) are listed in Table 1 and Table 2, respectively. On 2

May and 6 May 2011 (Shioyazaki and Nagasaki, about

50 km from F1NPP), specimens of most macroalgal spe-

cies, i.e., Ulva pertusa, U. linza Linnaeus, Scytosiphon

lomentaria (Lyngbye) Link, Eisenia bicyclis (Kjellman)

Setchell, Undaria pinnatifida, Sargassum muticum (Yendo)

Fensholt, and S. thunbergii, showed 137Cs levels greater

than 3,000 Bq kg-1 (Figs. 3, 4). The highest 137Cs level

was 7,371.20 ± 173.95 Bq kg-1 in Undaria pinnatifida

(Fig. 3; sample code k010 in Table 1). The 134Cs:137Cs

ratio was ca. 0.97. Exceptionally, Gloiopeltis furcata

(Postels & Ruprecht) J. Agardh showed a relatively lower

value of 767.37 ± 32.90 Bq kg-1 (Fig. 4; sample code

k014 in Table 1). Seawater collected on May 2 at Shi-

oyazaki (Fig. 3) and Nagasaki (Fig. 4) measured

8.41 ± 3.21 and 9.74 ± 3.43 Bq L-1, respectively. In

control samples from Awaji Island in May 2011, 137Cs

levels were below the detectable level of 0.001–0.002 in

Undaria pinnatifida, Sargassum muticum, and Ulva pertusa

(Table 1).137Cs levels remarkably declined at Nagasaki within the

following 5–6 months. In July 2011, 137Cs ranged from ca.

300–600 Bq kg-1 (Fig. 5), declined to 40–200 Bq kg-1 in

October 2011 (Fig. 6) and became lower than 100 Bq kg-1

in most samples in July 2012 (Fig. 7) and December 2012

(Fig. 8). However, 137Cs was still detectable in the range of

10–100 Bq kg-1 in many samples in March 2013,

24 months after the date of highest records (Fig. 9).

The progression of 137Cs levels differed in different

taxa. In the green alga Ulva pertusa, which has very short

lifetime (ephemeral species), 137Cs levels clearly declined

during the summer of 2011, but remained in the range of

10–110 Bq kg-1 from winter 2011 to spring 2013

(Fig. 10). 40K was somewhat higher in May 2011 samples,

Fig. 1 Locations of the collection sites of the specimens investigated

in the present study

J Plant Res (2014) 127:23–42 25

123

Page 4: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

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um

horn

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asak

i,Iw

aki,

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port

ion,

dir

ectl

ydri

ed

340.7

721.6

50.0

18

321.1

526.7

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4,7

83.7

0525.7

91.2

80

k019

9Ju

ly2011

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

japonic

a

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed426.8

737.5

20.1

36

425.3

245.3

40.0

97

n.d

.n.d

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38

k020

9Ju

ly2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

yam

adae

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed499.6

225.7

10.0

64

498.7

433.7

10.0

61

1,8

71.4

0446.7

51.2

95

k023

9Ju

ly2011

Phae

ophyce

aeL

amin

aria

les

Undari

a

pin

nati

fida

Nag

asak

i,Iw

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Fer

tile

thal

li,

froze

n

278.3

816.8

90.0

45

292.4

021.8

80.0

38

1,9

87.9

0355.5

20.9

76

26 J Plant Res (2014) 127:23–42

123

Page 5: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

1co

nti

nu

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Sam

ple

code

Coll

ecti

on

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Tax

onom

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of

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it

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kg

-1

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k024

17

May

2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

muti

cum

Iway

a,A

waj

iIs

l.,

Hyogo

Dir

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ydri

edn.d

.0.0

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02

n.d

.0.0

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03

2,7

68.8

025.0

4–

k025

17

May

2011

Phae

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aeL

amin

aria

les

Undari

a

pin

nati

fida

Iway

a,A

waj

iIs

l.,

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Dir

ectl

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edn.d

.0.0

00.0

01

n.d

.0.0

00.0

01

1,8

41.8

034.1

50.0

29

k026

31

May

2011

Phae

ophyce

aeE

ctoca

rpal

ess.

l.C

olp

om

enia

sinuosa

Iway

a,A

waj

iIs

l.,

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Dir

ectl

ydri

edn.d

.0.0

00.0

01

n.d

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01

496.5

045.3

00.0

42

k027

31

May

2011

Ulv

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aeU

lval

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lva

per

tusa

Iway

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waj

iIs

l.,

Hyogo

Dir

ectl

ydri

edn.d

.0.0

00.0

01

n.d

.0.0

00.0

01

1,1

47.6

042.5

30.0

37

k028

30

May

2011

Phae

ophyce

aeE

ctoca

rpal

ess.

l.Scy

tosi

phon

lom

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ria

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l.,

Hyogo

Dir

ectl

ydri

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.0.0

00.0

07

n.d

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00.0

05

1,9

55.9

0188.0

90.1

76

k029

6S

epte

mber

2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

aki,

Iwak

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Dir

ectl

ydri

ed681.8

620.6

80.0

43

773.2

230.8

30.0

34

2,1

15.4

0278.5

80.7

03

k030

6S

epte

mber

2011

Ulv

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aeU

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per

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Nag

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Dir

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202.8

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19

k031

6S

epte

mber

2011

Phae

ophyce

aeL

amin

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Sacc

hari

na

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a

Nag

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Juven

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lus,

dir

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ydri

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193.7

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97

230.3

136.7

10.0

86

4,2

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0860.9

82.3

89

k032

6S

epte

mber

2011

Phae

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aeL

amin

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les

Undari

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pin

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Nag

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i,Iw

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Old

sporo

phyll

,

dir

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ydri

ed

255.0

231.3

80.1

21

224.3

436.2

60.1

08

n.d

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16

k035

14

Oct

ober

2011

Rhodophyce

aeG

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esH

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asi

ati

caN

agas

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Iwak

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Fukush

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Dir

ectl

ydri

ed114.0

428.8

80.0

45

161.9

628.9

10.0

39

2,4

23.0

01144.6

01.1

08

k036

14

Oct

ober

2011

Ulv

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aeU

lval

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lva

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i,Iw

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Dir

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ed36.5

64.7

50.0

06

43.0

56.6

70.0

07

1,0

13.1

0194.7

90.1

77

k037

14

Oct

ober

2011

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

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a

Nag

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i,Iw

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Dir

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44.2

00.0

05

67.4

16.0

90.0

05

1,1

20.3

0158.4

40.1

37

k038

14

Oct

ober

2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

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Iwak

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Dir

ectl

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ed51.4

29.6

70.0

14

64.2

910.7

40.0

13

1,3

80.3

0372.9

80.3

48

k039

14

Oct

ober

2011

Phae

ophyce

aeL

amin

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les

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bic

ycli

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Mat

ure

thal

li,

dir

ectl

ydri

ed

105.9

94.7

80.0

04

114.0

06.6

60.0

04

995.0

4126.9

00.1

09

k040

14

Oct

ober

2011

Rhodophyce

aeG

igar

tinal

esN

eodil

sea

yendoana

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed53.9

26.2

10.0

09

68.4

68.4

30.0

07

1,5

50.9

0264.1

90.2

33

k041

14

Oct

ober

2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

yam

adae

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed200.1

714.0

10.0

13

229.2

017.5

40.0

12

1,5

22.6

0401.8

20.3

80

k042

14

Oct

ober

2011

Rhodophyce

aeG

igar

tinal

esA

hnfe

ltio

psi

s

para

doxa

Nag

asak

i,Iw

aki,

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ima

Dir

ectl

ydri

ed59.9

15.3

30.0

07

86.6

57.6

80.0

06

761.0

2184.2

20.1

70

k043

14

Oct

ober

2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

aki,

Iwak

i,

Fukush

ima

Juven

ile

thal

li,

dir

ectl

ydri

ed

59.5

76.3

30.0

08

69.1

58.2

50.0

08

1,7

42.1

0259.7

90.2

26

k045

14

Oct

ober

2011

Rhodophyce

aeC

eram

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sC

hondri

a

crass

icauli

s

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed121.4

07.2

30.0

06

111.8

19.1

80.0

08

2,7

72.7

0244.7

40.1

92

k046

2M

ay2011

Sea

wat

erS

hio

yaz

aki,

Iwak

i,

Fukush

ima

Sea

wat

er9.5

42.2

50.0

04

8.4

13.2

10.0

03

n.d

.n.d

.0.0

96

k047

2M

ay2011

Sea

wat

erN

agas

aki,

Iwak

i,

Fukush

ima

Sea

wat

er11.2

72.1

50.0

03

9.7

43.4

30.0

03

n.d

.n.d

.0.0

94

J Plant Res (2014) 127:23–42 27

123

Page 6: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

1co

nti

nu

ed

Sam

ple

code

Coll

ecti

on

dat

e

Tax

onom

yL

oca

lity

Note

(sam

ple

pre

par

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n

and

nat

ure

of

sam

ple

s)

134C

s137C

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ssO

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Spec

ies

Bq

kg

-1

Err

or

Det

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lim

it

Bq

kg

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lim

it

Bq

kg

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Err

or

Det

ect.

lim

it

k048

9Ju

ly2011

Mel

twat

er(d

rippin

g)

Nag

asak

i,Iw

aki,

Fukush

ima

Fro

mU

ndari

a

pin

nati

fida

39.4

83.1

00.0

03

42.2

14.0

50.0

03

340.4

597.7

80.0

91

k049

9Ju

ly2011

Mel

twat

er(d

rippin

g)

Nag

asak

i,Iw

aki,

Fukush

ima

Fro

m

Scy

tosi

phon

lom

enta

ria

344.7

18.6

30.0

05

383.0

912.0

10.0

05

n.d

.n.d

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20

k050

9Ju

ly2011

Mel

twat

er(d

rippin

g)

Shio

yaz

aki,

Iwak

i,

Fukush

ima

Fro

m

Sarg

ass

um

thunber

gii

402.9

78.8

60.0

05

436.7

212.1

40.0

04

502.6

5116.1

40.1

08

k051

9Ju

ly2011

Mel

twat

er(d

rippin

g)

Shio

yaz

aki,

Iwak

i,

Fukush

ima

Fro

mE

isen

ia

bic

ycli

s

697.8

711.1

90.0

06

809.5

016.2

00.0

05

440.8

3113.3

20.1

06

k052

5D

ecem

ber

2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

aki,

Iwak

i,

Fukush

ima

Juven

ile

thal

li,

dir

ectl

ydri

ed

54.3

87.1

30.0

09

69.8

412.2

70.0

09

2,5

12.0

0310.2

00.2

32

k053

5D

ecem

ber

2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

aki,

Iwak

i,

Fukush

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Mat

ure

thal

li,

dir

ectl

ydri

ed

96.8

48.5

20.0

07

106.1

112.0

00.0

10

2,2

58.5

0275.4

00.2

10

k054

5D

ecem

ber

2011

Rhodophyce

aeG

igar

tinal

esN

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sea

yendoana

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

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ed45.3

07.3

00.0

10

40.5

813.3

20.0

12

1,0

82.4

0281.8

00.2

49

k056

5D

ecem

ber

2011

Rhodophyce

aeC

ora

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ales

Call

iart

hro

nsp

.N

agas

aki,

Iwak

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Fukush

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Dir

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ydri

ed25.5

65.1

70.0

07

34.1

08.9

50.0

07

n.d

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97

k057

5D

ecem

ber

2011

Rhodophyce

aeC

eram

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sD

asy

ase

ssil

isN

agas

aki,

Iwak

i,

Fukush

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Dir

ectl

ydri

ed219.4

322.2

80.0

22

234.5

929.3

30.0

21

4,1

01.2

0705.2

10.5

92

k058

5D

ecem

ber

2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

yam

adae

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

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ed70.4

97.9

30.0

07

82.2

211.7

40.0

10

2,0

37.5

0297.7

00.2

34

k059

5D

ecem

ber

2011

Rhodophyce

aeG

igar

tinal

esA

hnfe

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psi

s

para

doxa

Nag

asak

i,Iw

aki,

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Dir

ectl

ydri

ed100.8

59.7

20.0

10

92.0

711.7

50.0

09

468.7

1261.3

10.2

48

k060

5D

ecem

ber

2011

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

japonic

a

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed67.1

47.0

70.0

07

78.8

210.2

10.0

08

1,7

93.1

0259.9

50.2

09

k061

5D

ecem

ber

2011

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

japonic

a

Nag

asak

i,Iw

aki,

Fukush

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Dir

ectl

ydri

ed57.1

28.5

10.0

11

59.3

413.5

30.0

11

2,2

79.1

0351.1

70.2

83

k062

5D

ecem

ber

2011

Phae

ophyce

aeR

alfs

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sA

nali

pus

japonic

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Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

edn.d

.0.0

00.0

48

197.2

041.7

00.0

42

n.d

.n.d

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85

k063

5D

ecem

ber

2011

Rhodophyce

aeG

igar

tinal

esG

loio

pel

tis

furc

ata

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed51.7

710.0

60.0

08

53.6

511.7

10.0

11

592.8

7309.5

70.2

96

k064

7M

arch

2012

Phae

ophyce

aeF

uca

les

Sarg

ass

um

horn

eri

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed133.8

723.4

70.0

31

187.5

830.5

40.0

23

2,0

15.0

0856.6

00.8

31

k065

7M

arch

2012

Rhodophyce

aeB

angia

les

Bangia

fusc

opurp

ure

a

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed160.5

18.9

80.0

09

226.2

213.8

00.0

09

936.7

0256.6

00.2

40

k066

7M

arch

2012

Ulv

ophyce

aeU

lval

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lva

linza

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

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ed66.2

510.3

00.0

16

85.1

614.6

00.0

15

1,8

65.0

0443.3

00.4

08

k067

7M

arch

2012

Phae

ophyce

aeF

uca

les

Sarg

ass

um

thunber

gii

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed106.3

76.4

00.0

07

137.0

39.2

40.0

06

1,6

54.0

0208.1

00.1

78

k068

7M

arch

2012

Phae

ophyce

aeE

ctoca

rpal

ess.

l.Scy

tosi

phon

lom

enta

ria

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed82.4

87.8

60.0

08

115.5

910.5

50.0

09

2,4

42.0

0285.5

00.2

37

28 J Plant Res (2014) 127:23–42

123

Page 7: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

1co

nti

nu

ed

Sam

ple

code

Coll

ecti

on

dat

e

Tax

onom

yL

oca

lity

Note

(sam

ple

pre

par

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n

and

nat

ure

of

sam

ple

s)

134C

s137C

s40K

Cla

ssO

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Spec

ies

Bq

kg

-1

Err

or

Det

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lim

it

Bq

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-1

Err

or

Det

ect.

lim

it

Bq

kg

-1

Err

or

Det

ect.

lim

it

k069

7M

arch

2012

Rhodophyce

aeB

angia

les

Pyr

opia

yezo

ensi

s

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed24.4

74.7

80.0

08

51.0

69.6

10.0

08

1,1

95.0

0252.3

00.2

30

k070

7M

arch

2012

Phae

ophyce

aeE

ctoca

rpal

ess.

l.P

etalo

nia

fasc

iaN

agas

aki,

Iwak

i,

Fukush

ima

Dir

ectl

ydri

ed53.6

88.5

90.0

13

84.3

712.5

00.0

14

3,1

59.0

0446.9

00.3

81

k071

7M

arch

2012

Ulv

ophyce

aeU

lval

esM

onost

rom

a

nit

idum

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed46.9

99.5

80.0

17

69.7

110.9

90.0

13

1,6

14.0

0412.7

00.4

00

k072

7M

arch

2012

Phae

ophyce

aeR

alfs

iale

sA

nali

pus

japonic

us

Nag

asak

i,Iw

aki,

Fukush

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Dir

ectl

ydri

ed76.4

85.7

10.0

06

105.7

78.0

00.0

05

1,0

64.0

0184.9

00.1

64

k073

7M

arch

2012

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Rhodophyce

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k084

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Rhodophyce

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k088

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k089

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85

J Plant Res (2014) 127:23–42 29

123

Page 8: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

1co

nti

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Sam

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07

k091

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l2012

Phae

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k092

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Apri

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2012

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May

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May

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May

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23

May

2012

Phae

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23

May

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Phae

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23

May

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k109

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703.1

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73

30 J Plant Res (2014) 127:23–42

123

Page 9: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

1co

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Sam

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Coll

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23

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2012

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23

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May

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23

May

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Rhodophyce

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Mat

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May

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10

Dec

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2012

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Dec

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Dec

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Phae

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Dec

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2012

Phae

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Dec

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2012

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Dec

ember

2012

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657.2

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Dec

ember

2012

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Dec

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2012

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Dec

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2012

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06

J Plant Res (2014) 127:23–42 31

123

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Ta

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ember

2012

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22.4

90.0

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9.4

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1,1

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16

k135

10

Dec

ember

2012

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9.8

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604.9

481.6

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76

k138

10

Dec

ember

2012

Rhodophyce

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14

92.3

312.2

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13

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76

k139

10

Dec

ember

2012

Rhodophyce

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688.5

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k140

10

Dec

ember

2012

Rhodophyce

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514.6

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10

Dec

ember

2012

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Dir

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24.6

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47.8

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0213.1

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k142

9D

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2012

Phae

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592.6

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k143

9D

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2012

Rhodophyce

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His

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03

59.7

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1,1

49.1

097.5

90.0

86

k144

9D

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2012

Rhodophyce

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Dir

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33.5

10.0

04

36.8

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70.0

04

1,2

57.7

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10.1

10

k145

9D

ecem

ber

2012

Phae

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aeF

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Sarg

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His

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74.2

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209.8

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04

1,5

03.3

01290.7

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13

k146

9D

ecem

ber

2012

Phae

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aeF

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Sarg

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His

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Dir

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ed21.4

91.8

60.0

03

34.7

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70.0

03

4,2

06.9

0116.5

20.0

78

k147

9D

ecem

ber

2012

Phae

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aeE

ctoca

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His

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Dir

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74.8

80.0

04

363.6

57.7

00.0

03

3,0

25.4

0122.4

80.0

93

k148

9D

ecem

ber

2012

Phae

ophyce

aeL

amin

aria

les

Sacc

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na

japonic

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His

anoham

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Dir

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ed33.5

52.7

10.0

03

60.8

735.8

20.0

03

3,4

79.6

0118.9

00.0

86

k149

9D

ecem

ber

2012

Phae

ophyce

aeL

amin

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les

Sacc

hari

na

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a

His

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Dir

ectl

ydri

ed34.0

32.8

20.0

03

54.7

43.6

10.0

03

3,2

18.6

0122.4

60.0

91

k150

9D

ecem

ber

2012

Rhodophyce

aeC

eram

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sC

hondri

a

crass

icauli

s

His

anoham

a,

Iwak

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Fukush

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Dir

ectl

ydri

ed42.0

54.2

70.0

05

58.6

06.1

80.0

05

3,9

37.1

0186.6

40.1

47

k151

16

Mar

ch

2013

Phae

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aeF

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Sarg

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horn

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Nag

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i,Iw

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Fukush

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Dir

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edn.d

.0.0

00.0

03

10.6

43.1

10.0

03

2,2

50.8

0108.2

80.0

85

k152

16

Mar

ch

2013

Phae

ophyce

aeF

uca

les

Sarg

ass

um

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Nag

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i,Iw

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Dir

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ed9.6

92.3

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05

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14.5

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04

840.9

4140.7

40.1

32

32 J Plant Res (2014) 127:23–42

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Ta

ble

1co

nti

nu

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Sam

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Coll

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k153

16

Mar

ch

2013

Ulv

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Dir

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91.8

70.0

03

19.1

23.2

40.0

03

1,4

53.1

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20.1

03

k154

16

Mar

ch

2013

Phae

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edn.d

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07.1

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03

1,2

74.5

091.3

20.0

79

k155

16

Mar

ch

2013

Phae

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aeF

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Sarg

ass

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thunber

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Nag

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i,Iw

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Dir

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22.3

50.0

03

20.9

02.8

80.0

03

1,7

38.2

0124.2

20.1

06

k156

16

Mar

ch

2013

Rhodophyce

aeG

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tinal

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psi

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flabel

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rmis

Nag

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i,Iw

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Dir

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ydri

ed16.7

13.7

70.0

08

22.8

07.5

30.0

07

1,3

49.4

0230.5

10.2

17

k158

16

Mar

ch

2013

Rhodophyce

aeR

hodym

enia

les

Lom

enta

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date

nsi

s

Nag

asak

i,Iw

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Fukush

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Dir

ectl

ydri

ed34.7

73.0

80.0

04

60.4

74.4

30.0

04

993.4

2130.8

60.1

21

k159

16

Mar

ch

2013

Phae

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aeD

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les

Pach

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Nag

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i,Iw

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Dir

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34.9

40.0

07

38.1

15.3

50.0

07

1,4

94.5

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10.2

16

k160

16

Mar

ch

2013

Ulv

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aeC

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Cla

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Nag

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i,Iw

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Dir

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ed50.8

85.2

30.0

06

75.1

16.1

00.0

06

1,0

29.2

0190.0

50.1

79

k161

16

Mar

ch

2013

Ulv

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aeU

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Dir

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64.5

80.0

06

67.0

55.6

60.0

06

1,2

18.0

0182.8

20.1

72

k162

16

Mar

ch

2013

Ulv

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Chaet

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04

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70.0

04

3,3

97.3

0168.2

80.1

34

k164

16

Mar

ch

2013

Rhodophyce

aeG

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para

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Nag

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Dir

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ydri

ed11.3

12.1

30.0

02

16.8

52.1

80.0

02

902.5

385.4

50.0

76

k165

16

Mar

ch

2013

Rhodophyce

aeG

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pel

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Nag

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Dir

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edn.d

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03

n.d

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03

534.6

6105.2

80.1

00

k166

16

Mar

ch

2013

Rhodophyce

aeG

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Nag

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Dir

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edn.d

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00.0

04

n.d

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04

601.2

6125.9

20.1

20

k167

16

Mar

ch

2013

Rhodophyce

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Nag

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Dir

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edn.d

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03

7.4

21.9

70.0

03

503.2

785.2

00.0

81

k169

16

Mar

ch

2013

Rhodophyce

aeG

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tinal

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nis

Nag

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i,Iw

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Fukush

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Dir

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ydri

ed27.5

34.4

10.0

04

48.0

14.0

60.0

04

533.0

0133.3

70.1

28

k170

16

Mar

ch

2013

Rhodophyce

aeG

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affi

nis

Nag

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i,Iw

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Dir

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ed12.2

02.4

20.0

04

13.5

13.6

00.0

03

377.6

5107.9

40.1

05

k171

16

Mar

ch

2013

Phae

ophyce

aeR

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Nag

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i,Iw

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Fukush

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Dir

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ydri

ed13.1

22.5

80.0

06

36.3

55.0

30.0

05

931.9

0180.1

70.1

72

k173

16

Mar

ch

2013

Rhodophyce

aeC

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hondri

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Nag

asak

i,Iw

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Fukush

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Dir

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ydri

ed12.1

42.4

80.0

04

15.7

73.9

20.0

04

4,2

77.6

0152.0

70.1

10

k174

16

Mar

ch

2013

Phae

ophyce

aeL

amin

aria

les

Undari

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pin

nati

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Nag

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i,Iw

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Dir

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ydri

ed6.7

02.1

10.0

03

n.d

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00.0

29

1,3

52.8

0100.0

10.0

86

k175

16

Mar

ch

2013

Phae

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aeL

amin

aria

les

Undari

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pin

nati

fida

Nag

asak

i,Iw

aki,

Fukush

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Dir

ectl

ydri

ed5.2

92.1

00.0

03

11.2

72.9

60.0

03

1,8

08.8

0102.7

10.0

84

k176

16

Mar

ch

2013

Ulv

ophyce

aeC

ladophora

les

Cla

dophora

alb

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Nag

asak

i,Iw

aki,

Fukush

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Dir

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ydri

ed62.1

35.3

00.0

06

113.1

98.7

50.0

06

1,5

73.6

0205.1

20.1

90

k177

16

Mar

ch

2013

Rhodophyce

aeG

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la

japonic

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Nag

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i,Iw

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Fukush

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Dir

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00.0

04

8.2

42.3

30.0

04

771.8

2109.9

90.1

03

J Plant Res (2014) 127:23–42 33

123

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Ta

ble

1co

nti

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Sam

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Coll

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k178

16

Mar

ch

2013

Ulv

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i,Iw

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Fukush

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Dir

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53.5

60.0

05

60.4

85.1

30.0

05

1,3

62.2

0161.8

70.1

48

k179

16

Mar

ch

2013

Ulv

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aeU

lval

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lva

per

tusa

Hir

ono,

Futa

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Dir

ectl

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ed26.0

64.6

00.0

07

58.1

75.7

40.0

06

1,0

16.7

0201.4

60.1

92

k180

16

Mar

ch

2013

Rhodophyce

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Hir

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Dir

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32.0

00.0

03

13.8

13.0

90.0

03

537.8

890.5

30.0

86

k183

16

Mar

ch

2013

Rhodophyce

aeB

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Pyr

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yezo

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Hir

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Dir

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edn.d

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00.0

05

11.2

62.8

80.0

04

759.9

0146.3

30.1

39

k184

16

Mar

ch

2013

Ulv

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Futa

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Dir

ectl

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ed78.6

46.2

20.0

08

139.6

28.7

50.0

07

828.0

8230.7

20.2

24

k185

16

Mar

ch

2013

Phae

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l.P

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Dir

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00.0

05

21.6

93.2

60.0

04

1,3

94.7

0138.4

80.1

25

k186

16

Mar

ch

2013

Rhodophyce

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sea

longis

sim

a

Hir

ono,

Futa

ba,

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ima

Dir

ectl

ydri

ed7.0

82.5

90.0

03

14.3

63.2

50.0

03

1,7

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20.0

96

k187

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Mar

ch

2013

Rhodophyce

aeG

igar

tinal

esG

loio

pel

tis

furc

ata

Hir

ono,

Futa

ba,

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ima

Dir

ectl

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ed14.6

32.8

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05

18.1

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05

437.2

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k188

16

Mar

ch

2013

Rhodophyce

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igar

tinal

esG

loio

pel

tis

furc

ata

Hir

ono,

Futa

ba,

Fukush

ima

Dir

ectl

ydri

ed9.0

42.4

20.0

05

24.5

73.7

10.0

05

542.1

2143.0

30.1

38

k189

16

Mar

ch

2013

Phae

ophyce

aeR

alfs

iale

sA

nali

pus

japonic

us

Hir

ono,

Futa

ba,

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ima

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ectl

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ed22.1

02.3

00.0

03

36.3

63.0

20.0

03

1,1

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k190

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ch

2013

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eram

iale

sC

hondri

a

crass

icauli

s

Hir

ono,

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ba,

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ima

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ectl

ydri

ed29.8

22.8

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49.9

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50.0

03

3,0

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0126.9

80.0

97

k191

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Mar

ch

2013

Phae

ophyce

aeL

amin

aria

les

Undari

a

pin

nati

fida

Hir

ono,

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ba,

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ima

Dir

ectl

ydri

edn.d

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03

11.9

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1,3

13.6

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77

Val

ues

of

det

ecti

on

lim

itin

Bq

kg

-1.

n.d

.m

eans

not

det

ecta

ble

(blo

wth

edet

ecti

on

lim

it).

Err

or

mea

ns

over

all

erro

res

tim

ated

by

the

anal

yzi

ng

soft

war

efr

om

syst

emat

icer

rors

inth

esy

stem

toget

her

wit

hth

est

andar

ddev

iati

on

of

the

counti

ng

34 J Plant Res (2014) 127:23–42

123

Page 13: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Ta

ble

2L

ist

of

sam

ple

sex

amin

edat

Iwak

iM

eise

iU

niv

ersi

ty,

and

the

resu

lts

of

134C

san

d137C

sm

easu

rem

ents

Sam

ple

code

Coll

ecti

on

dat

e

Tax

onom

yL

oca

lity

Note

(sam

ple

pre

par

atio

nan

d

nat

ure

of

sam

ple

s)

134C

s137C

s

Cla

ssO

rder

Spec

ies

Bq

kg

-1

Err

or

Det

ect.

lim

it

Bq

kg

-1

Err

or

Det

ect.

lim

it

IMU

001

2M

ay2011

Phae

ophyce

aeD

icty

ota

les

Spato

glo

ssum

paci

ficu

mS

hio

yaz

aki,

Iwak

i,F

ukush

ima

Fro

zen

5,2

00

138

156

9,4

30

179

133

IMU

002

2M

ay2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

yam

adae

Shio

yaz

aki,

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i,F

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ima

Fro

zen

1,2

10

25.2

25.8

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80

31.5

19.9

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003

6M

ay2011

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

japonic

aN

agas

aki,

Iwak

i,F

ukush

ima

Fro

zen

3,9

10

116

144

6,0

20

138

108

IMU

004

6M

ay2011

Phae

ophyce

aeL

amin

aria

les

Eis

enia

bic

ycli

sN

agas

aki,

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i,F

ukush

ima

Fro

zen

3,6

70

96.5

107

5,9

80

119

89.2

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005

6M

ay2011

Rhodophyce

aeG

igar

tinal

esG

rate

loupia

lance

ola

taN

agas

aki,

Iwak

i,F

ukush

ima

Fro

zen

2,9

20

123

159

4,3

90

146

144

IMU

006

9Ju

ly2011

Phae

ophyce

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ota

les

Dic

tyota

dic

hoto

ma

Nag

asak

i,Iw

aki,

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zen

556

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167

1,1

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148

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007

9Ju

ly2011

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ctoca

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ess.

l.C

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om

enia

sinuosa

Nag

asak

i,Iw

aki,

Fukush

ima

Fro

zen

720

163

446

1,3

90

189

434

IMU

008

9Ju

ly2011

Phae

ophyce

aeE

ctoca

rpal

ess.

l.Scy

tosi

phon

lom

enta

ria

Nag

asak

i,Iw

aki,

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ima

Fro

zen

590

53.4

98.5

1,0

80

68.3

101

IMU

009

9Ju

ly2011

Phae

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aeD

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are

stia

ligula

taN

agas

aki,

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zen

154

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011.3

255

9.9

811.5

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010

9Ju

ly2011

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aeL

amin

aria

les

Eis

enia

bic

ycli

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zen

676

16.0

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011

9Ju

ly2011

Rhodophyce

aeG

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tinal

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hondru

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llatu

sN

agas

aki,

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i,F

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Fro

zen

288

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174

333

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164

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012

9Ju

ly2011

Rhodophyce

aeG

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rate

loupia

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aN

agas

aki,

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i,F

ukush

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Fro

zen

569

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102

1,0

30

58.8

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IMU

013

9Ju

ly2011

Rhodophyce

aeG

igar

tinal

esA

hnfe

ltio

psi

spara

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Nag

asak

i,Iw

aki,

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ima

Fro

zen

174

13.2

23.3

339

17.4

22.9

IMU

014

9Ju

ly2011

Rhodophyce

aeR

hodym

enia

les

Gast

rocl

oniu

mpaci

ficu

mN

agas

aki,

Iwak

i,F

ukush

ima

Fro

zen

733

43.8

70.2

1,1

90

53.1

64.5

IMU

015

14

Oct

ober

2011

Phae

ophyce

aeF

uca

les

Sarg

ass

um

horn

eri

Nag

asak

i,Iw

aki,

Fukush

ima

Fro

zen

267

62.3

172

470

66.2

147

IMU

016

4Ju

ly2012

Phae

ophyce

aeR

alfs

iale

sA

nali

pus

japonic

us

Nag

asak

i,Iw

aki,

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ima

Dir

ectl

ydri

ed54.2

6.3

013.8

87.8

7.5

213.7

IMU

017

4Ju

ly2012

Phae

ophyce

aeD

icty

ota

les

Dic

tyota

dic

hoto

ma

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed113

8.2

014.8

150

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114.7

IMU

018

4Ju

ly2012

Phae

ophyce

aeE

ctoca

rpal

ess.

l.L

eath

esia

dif

form

isN

agas

aki,

Iwak

i,F

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ima

Dir

ectl

ydri

ed128

10.4

20.7

213

12.2

18.5

IMU

019

4Ju

ly2012

Phae

ophyce

aeE

ctoca

rpal

ess.

l.Scy

tosi

phon

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enta

ria

Nag

asak

i,Iw

aki,

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ima

Dir

ectl

ydri

edn.d

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51.0

56.3

15.8

45.7

IMU

020

4Ju

ly2012

Phae

ophyce

aeE

ctoca

rpal

ess.

l.T

inocl

adia

crass

aN

agas

aki,

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Dir

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ed27.3

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38.7

9.6

227.0

IMU

021

4Ju

ly2012

Phae

ophyce

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uca

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ass

um

confu

sum

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asak

i,Iw

aki,

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ima

Dir

ectl

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ed15.5

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30.0

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0

IMU

022

4Ju

ly2012

Phae

ophyce

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uca

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ass

um

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eri

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i,Iw

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ly2012

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um

thunber

gii

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i,Iw

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0

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024

4Ju

ly2012

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i,Iw

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025

4Ju

ly2012

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4Ju

ly2012

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aria

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bic

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aki,

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IMU

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4Ju

ly2012

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per

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asak

i,Iw

aki,

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ima

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ed15.3

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211.0

IMU

028

4Ju

ly2012

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ophyce

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om

orp

ha

monil

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aN

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aki,

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312.7

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029

4Ju

ly2012

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odia

les

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mlu

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aki,

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ly2012

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i,Iw

aki,

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ima

Dir

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ed72.4

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86.7

8.9

619.5

IMU

031

4Ju

ly2012

Rhodophyce

aeC

ora

llin

ales

Cora

llin

apil

uli

fera

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

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ed36.2

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67.2

963.9

4.6

37.8

7

IMU

032

4Ju

ly2012

Rhodophyce

aeC

ora

llin

ales

Call

iart

hro

nye

ssoen

seN

agas

aki,

Iwak

i,F

ukush

ima

Dir

ectl

ydri

ed14.7

3.5

39.8

222.1

3.8

39.4

5

IMU

033

4Ju

ly2012

Rhodophyce

aeG

igar

tinal

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us

inte

rmed

ius

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed38.9

6.0

414.9

54.2

6.6

414.7

IMU

034

4Ju

ly2012

Rhodophyce

aeG

igar

tinal

esC

hondru

soce

llatu

sN

agas

aki,

Iwak

i,F

ukush

ima

Dir

ectl

ydri

ed23.2

4.0

710.3

40.6

4.8

710.4

IMU

035

4Ju

ly2012

Rhodophyce

aeG

igar

tinal

esA

hnfe

ltio

psi

spara

doxa

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed27.9

35.9

8.2

247.0

4.5

49.1

5

IMU

036

4Ju

ly2012

Rhodophyce

aeC

eram

iale

sC

hondri

acr

ass

icauli

sN

agas

aki,

Iwak

i,F

ukush

ima

Dir

ectl

ydri

ed69.0

7.6

916.4

105

8.8

115.4

IMU

037

4Ju

ly2012

Rhodophyce

aeC

eram

iale

sL

aure

nci

aoka

mura

eN

agas

aki,

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Dir

ectl

ydri

ed129

7.2

911.3

239

9.5

99.8

4

J Plant Res (2014) 127:23–42 35

123

Page 14: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

but was rather constant in the other samples (ca.

1,000–1,500 Bq kg-1). The annual brown algae Undaria

pinnatifida (Fig. 11) and Sargassum horneri (data not

shown) showed similar patterns of 137Cs progression: they

showed rapid decline in the first year, and continuously

declined until March 2013. The 40K level of Undaria

pinnatifida of the specimens from Chiba Pref. and Hyogo

Pref. were 1,840–1,990 Bq kg-1 (Fig. 11).Ta

ble

2co

nti

nu

ed

Sam

ple

code

Coll

ecti

on

dat

e

Tax

onom

yL

oca

lity

Note

(sam

ple

pre

par

atio

nan

d

nat

ure

of

sam

ple

s)

134C

s137C

s

Cla

ssO

rder

Spec

ies

Bq

kg

-1

Err

or

Det

ect.

lim

it

Bq

kg

-1

Err

or

Det

ect.

lim

it

IMU

038

10

Dec

ember

2012

Phae

ophyce

aeF

uca

les

Sarg

ass

um

horn

eri

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed16.3

4.6

913.6

n.d

.0

16.0

IMU

039

10

Dec

ember

2012

Phae

ophyce

aeF

uca

les

Sarg

ass

um

sili

quast

rum

Nag

asak

i,Iw

aki,

Fukush

ima

Dir

ectl

ydri

ed60.5

7.0

416.2

118

8.3

713.1

IMU

040

10

Dec

ember

2012

Phae

ophyce

aeL

amin

aria

les

Sacc

hari

na

japonic

aN

agas

aki,

Iwak

i,F

ukush

ima

Dir

ectl

ydri

ed26.2

5.2

313.8

47.5

6.2

213.9

Val

ues

of

det

ecti

on

lim

itin

Bq

kg

-1.

n.d

.m

eans

not

det

ecta

ble

(blo

wth

edet

ecti

on

lim

it).

Err

or

mea

ns

over

all

erro

res

tim

ated

by

the

anal

yzi

ng

soft

war

efr

om

syst

emat

icer

rors

inth

esy

stem

toget

her

wit

hth

est

andar

d

dev

iati

on

of

the

counti

ng

Fig. 2 Evolution of 134Cs/137Cs ratio of the specimens examined.

Dotted line indicates the theoretical expected value by the sponta-

neous decay of 134Cs and 137Cs

Fig. 3 Quantities of 134Cs and 137Cs of diverse marine macroalgae

and seawater collected in May 2011 at Shioyazaki, Iwaki, Fukushima

Pref., Japan. Measurement unit for seawater is Bq kg-1 (wet weight).

Asterisks show data by the measurement at Iwaki Meisei University

36 J Plant Res (2014) 127:23–42

123

Page 15: Radioactive cesium accumulation in seaweeds by the Fukushima 1 Nuclear Power Plant accident—two years’ monitoring at Iwaki and its vicinity

Perennial brown algae such as Eisenia bicyclis

(Fig. 12) and Sargassum yamadae (Fig. 13), which are

important elements of algal beds in the area, also showed

similar progressions in 137Cs levels, although the level of40K (ca. 1,500–2,000 Bq kg-1) was generally higher than

in Ulva pertusa (Fig. 11). The 40K levels of Eisenia bi-

cyclis and Sargassum yamadae of the specimens from

Chiba Pref. were 1,650–1,750 and 1,180 Bq kg-1,

respectively, and were comparable to those in Fukushima

Pref. (Figs. 12, 13). Unfortunately, there were few species

of red algae that could be collected seasonally. Ahnfelti-

opsis paradoxa (Suringar) Masuda (Fig. 14) showed a

clear decrease in 137Cs levels in 2011, but it was also still

in a detectable range of ca. 10 Bq kg-1 in March 2013.40K levels were in the range of 800–1,000 Bq kg-1,

which was comparable to Ulva (green alga) and consid-

erably lower than Undaria, Eisenia and Sargassum)

(brown algae).

Discussion

137Cs concentrations in seawater off the eastern Japan coast

prior to the accident were in the same order of magnitude

as other surface oceanic waters, between 1 and 3 Bq m-3

for 137Cs (Nakanishi et al. 2010). After the accident,

measured concentrations in a 30 km perimeter around the

plant exceeded 10 Bq L-1 (or 10,000,000 Bq m-3) (Bailly

du Bois et al. 2012).

The 137Cs levels in seawater at the coast of Iwaki

(Shioyazaki and Nagasaki) one month after the mass dis-

charge of high concentration contaminated water in April

measured ca. 8–10 Bq L-1 in our own measurements

(Fig. 4). These values agree well with the report of Bailly

du Bois et al. (2012). The coast around Shioyazaki and

Nagasaki was estimated to have been exposed up to ca.

60 Bq L-1 for about two weeks (15 April–1 May 2011)

according to the estimated geographical distribution of the137Cs in Bailly du Bois et al. (2012).

The influence of the radioactive liquid effluents escaping

directly from the nuclear power plant was particularly sig-

nificant from 26 March to 8 April 2011 in the vicinity of the

plant. Concentrations measured after 10 April 2011 declined

in the vicinity of the plant. The perennial brown alga Eisenia

bicyclis also showed a similar pattern, but in the red alga

Ahnfeltiopsis paradoxa the levels stayed about the same

during December 2012 and March 2013. In contrast, the

concentration of 40K was relatively stable throughout the

period, in accordance with the assumption that it is not of

anthropogenic origin because the levels were comparable to

those of the specimens from Chiba Pref. and Hyogo Pref.

Given that the seawater 137Cs levels were in the range of

10–60 Bq L-1 at Shioyazaki and Nagasaki in April 2011

[according to our data and those by Bailly du Bois et al.

Fig. 4 Quantities of 134Cs and 137Cs of diverse marine macroalgae

and seawater collected in May 2011 at Nagasaki, Iwaki, Fukushima

Pref., Japan. Measurement unit for seawater is Bq kg-1 (wet weight).

Asterisks show data by the measurement at Iwaki Meisei University

Fig. 5 Quantities of 134Cs and 137Cs of diverse marine macroalgae

collected in July 2011 at Nagasaki, Iwaki, Fukushima Pref., Japan.

Asterisks show data by the measurement at Iwaki Meisei University

J Plant Res (2014) 127:23–42 37

123

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Fig. 6 Quantities of 134Cs and 137Cs of diverse marine macroalgae

collected in October 2011 at Nagasaki, Iwaki, Fukushima Pref.,

Japan. Asterisks show data by the measurement at Iwaki Meisei

University

Fig. 7 Quantities of 134Cs and 137Cs of diverse marine macroalgae

collected in July 2012 at Nagasaki, Iwaki, Fukushima Pref., Japan.

Asterisks show data by the measurement at Iwaki Meisei University

Fig. 8 Quantities of 134Cs and 137Cs of diverse marine macroalgae

and seawater collected in December 2012 at Nagasaki, Iwaki,

Fukushima Pref., Japan. Asterisks show data by the measurement at

Iwaki Meisei University

Fig. 9 Quantities of 134Cs and 137Cs of diverse marine macroalgae

and seawater collected in March 2013 at Nagasaki, Iwaki, Fukushima

Pref., Japan

38 J Plant Res (2014) 127:23–42

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(2012)], and that seaweeds collected in May 2011 con-

tained an average 137Cs level of ca. 5,000 Bq kg-1, the

seaweeds are considered to have accumulated 137Cs in their

tissues by 8–50 folds compared to their environment

(80–500 folds in dry samples, given the wet/dry mass ratio

of 10). These CF values must be certainly underestimated

because some part (or a large part) of the algal tissue of the

specimens collected in early May 2011 (2 May and 6 May

2011) had already been grown up before the exposure to

the highly radiopolluted seawater. In general, the growth

rate of seaweeds differs depending on the species; even in

rather fast growing species, such as Ulva spp. and Undaria

pinnatifida, their growth period is longer than one month;

and many species grow up in 3–4 months.

The above CF values of ca. 8–50 agree well with the

known CF values of ca. 30–50 in marine macroalgae

(IAEA 2004). Considering the underestimation in our data

as mentioned above, macroalgal CF may be somewhat

higher than the IAEA standard. This could be caused if

the local concentration of 137Cs in polluted seawater

during the seaweed growth period (e.g., during later April

2011) were higher than that on the collection dates after

May 2011.

The 137Cs levels of the specimens directly dried after

collection (air-dried and then heated; e.g., k001, k004 in

Table 1), and those frozen before drying (frozen, thawed,

air-dried and then heated; e.g., k017, k023) were roughly

comparable. Meltwater from the frozen algal tissues (k048–

Fig. 10 Evolution of 134Cs, 137Cs and 40K quantities in the annual

green alga Ulva pertusa at Nagasaki, Iwaki, Fukushima Pref., Japan

Fig. 11 Evolution of 134Cs, 137Cs and 40K quantities in the annual

brown alga Undaria pinnatifida at Nagasaki, Iwaki, Fukushima Pref.,

Japan

Fig. 12 Evolution of 134Cs, 137Cs and 40K quantities in the perennial

brown alga Eisenia bicyclis at Nagasaki, Iwaki, Fukushima Pref.,

Japan

Fig. 13 Evolution of 134Cs, 137Cs and 40K quantities in the perennial

brown alga Sargassum yamadae at Nagasaki, Iwaki, Fukushima Pref.,

Japan

J Plant Res (2014) 127:23–42 39

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k051) contained significantly higher concentrations of 137Cs

compared to the thawed tissue, although the levels were

rather variable depending on the taxa (ca. 40 Bq L-1 in

Undaria pinnatifida to ca. 800 Bq L-1 in Eisenia bicyclis).

The 137Cs concentrations in meltwater was much higher

than that in ambient seawater, which was below the detec-

tion level of ca. 1 Bq L-1 in early July 2011, and was

comparable to that in fresh algal tissues, which was esti-

mated from the present measurements of directly dried

specimens. Thus, we concluded that the measurements

based on dried specimens after the freezing process may

underestimate the 137Cs concentrations in fresh algal tissues.

We showed that the radioactive Cs levels in marine

macroalgae decline rather rapidly during the summer of

2011. This may be ascribed to the fact that the marine

macroalgae grow and turnover rapidly during this period.

The growth periods of a number of annual taxa [e.g.,

Scytosiphon lomentaria, Monostroma nitidum Wittrock,

Ulva spp., Pyropia (Porphyra) spp.] are less than six

months irrespective of their life history patterns (see below;

Fig. 15). Many taxa have life histories with alternation of

heteromorphic sporophytes and gametophytes [e.g., Un-

daria pinnatifida, Scytosiphon lomentaria, Monostroma

nitidum, Pyropia yezoensis (Roth) C. Agardh] and their

macroscopic generations disappear during summer and

autumn (Bold and Wynne 1985; Graham and Wilcox 2000;

Hori 1993, 1994). In these cases, even though the thallus

tissues had absorbed a large amount of radionuclides dur-

ing development (i.e., late March–April 2011), they were

replaced by new tissues, resulting in lower or null radio-

nuclide concentrations before summer and autumn 2011.

Some of the taxa with heteromorphic life history have

perennial macroscopic thalli, and these thalli persist during

summer (e.g., Eisenia bicyclis, Saccharina japonica).

However, they show intercalary growth with a growth zone

in the transitional zone between blade and stipe, and the

older parts of the thalli (blade) become gradually lost from

the tip within several months (Bold and Wynne 1985).

Many others, e.g., Ulva spp., Dictyota dichotoma (Hudson)

J.V. Lamouroux, Spatoglossum crissum J. Tanaka, Chondrus

spp., Gloiopeltis furcate, and Ahnfeltiopsis paradoxa, have

life histories with alternation between isomorphic macro-

scopic generations. However, the growth period of a genera-

tion is generally less than 6 months as mentioned above.

A few taxa, e.g., Codium spp. and Sargassum spp., lack

alternation of generations in their life history. Among

them, Sargassum horneri is a winter-spring annual, and

S. yamadae is a perennial species growing during a spring–

summer term. Therefore, most of the macroalgae (and the

tissues constituting their thalli) collected later than autumn

2011 grew by absorbing ambient nutrients including Cs

Fig. 14 Evolution of 134Cs, 137Cs and 40K quantities in the perennial

red alga Ahnfeltiopsis paradoxa at Nagasaki, Iwaki, Fukushima Pref.,

Japan

Fig. 15 Schematic presentation

of growth period (phenology) of

representative marine

macroalgae at Iwaki and its

vicinity

40 J Plant Res (2014) 127:23–42

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after a rapid decline of the radionuclide concentrations in

seawater. However, it is noteworthy that the levels of 134Cs as

well as 137Cs have remained more or less stable since winter

2012, and were still detectable in spring 2013 in most marine

macroalgae (ca. 8–140 Bq kg-1 for 137Cs in dried speci-

mens). Considering the CF values of Cs in marine macroalgae,

i.e., 8–50 in our study and 50 in the IAEA report, the 137Cs

level in ambient seawater of marine macroalgae habitats was

considered to have retained at the minimum the level of ca.

0.02–0.3 Bq L-1 (based on CF 50). The detection limit of134Cs and 137Cs in seawater differs remarkably depending on

analytical facilities: ca. 0.0008 Bq L-1, http://www1.kaiho.

mlit.go.jp/KANKYO/press/press20121106.pdf; 0.025 Bq

L-1, http://www.env.go.jp/guide/budget/h25/h25-gaiyo/011.

pdf; and 1.2 Bq L-1, http://radioactivity.nsr.go.jp/ja/

contents/8000/7638/24/278_i_0531.pdf. The concentration

in seawater (0.02–0.3 Bq L-1) is critical for the direct

detection of radionuclides in some analytical facilities.

It has been suggested that marine macroalgal metal

loads can be used as markers to track the geographical

distributions of the metal concentrations in coastal seawa-

ters, e.g., Ulva spp. (Caliceti et al. 2002; Haritonidis and

Malea1999), Undaria pinnatifida (Yamada et al. 2007).

Similarly, the bio-monitoring of coastal 137Cs using sea-

weeds must be very useful because marine macroalgae in

general are shown to avidly accumulate 137Cs in their tis-

sues (CF = ca. 8–50), whereas they grow rather rapidly

and, hence, turnover rapidly, so that they exert no influence

of bioconcentration through the food chain.

Acknowledgments We are grateful to E.C. Henry (Reed Maricul-

ture) for his valuable comments on the manuscript, Chiyo Komiyama

and Tomoko Kotani (Kobe University) for technical support in the

measurements of radionuclides and data analyses, Toshiaki Wada,

Tadashi Iwasaki, Naoto Hirakawa (Fukushima Prefectural Fisheries

Experimental Station), Masataka Ohta (Marine Ecology Research

Institute) and Norio Kikuchi (Natural History Museum and Institute,

Chiba) for assistance in the field collections. The project was sup-

ported by the research grant of Organization of Advanced Science and

Technology, Kobe University.

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