by: derrick griffin. it is a well-known fact that the dead sea located in jordan, israel is one of...
TRANSCRIPT
![Page 1: By: Derrick Griffin. It is a well-known fact that the Dead Sea located in Jordan, Israel is one of the saltiest lakes in the world, whose salinity is](https://reader035.vdocuments.site/reader035/viewer/2022062713/56649cbb5503460f94983893/html5/thumbnails/1.jpg)
Particulate Properties of the
Dead Sea Retrieved by the Physical Optics Method
By: Derrick Griffin
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It is a well-known fact that the Dead Sea located in Jordan, Israel is one of
the saltiest lakes in the world, whose salinity is approximately 30%. Such a
huge salinity makes it almost biologically lifeless. However this lake contains
large quantities of different minerals and some quantity of dissolved organic
matter. Minerals of the Dead Sea are important for medicinal and cosmetics
purposes. Unfortunately, the Dead Sea is slowly drying up and soon it will
no longer be around in years to come. We can help preserve the Dead Sea
and it’s important that we use its wealth more rationally to prevent or delay
its death. Thus it is imperative that we find answers to the following
questions: Which minerals are exactly dispersed within the water? What are
the minerals concentration and their vertical and horizontal space
distribution? We must find if this solution is unique and stable?
Abstract
Ocean Optics Team
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2004 Optical Expedition Scientific Team
Absorption & Attenuation & Number of Wavelengths
Particulate Attenuation as cpart = apart + bpart.
Introduction
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Which method did I use to conduct my research?
What are the benefits of using the Optical method?
Methods
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Data Visualization
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Data CollectionDepth
(m)ap(412) ap(440) bp(412) bp(440) cp(412) cp(440) bbp(660)
1.5 0.142 0.097 1.104 1.080 1.246 1.1771.076E-
02
1.5 0.137 0.094 1.109 1.084 1.246 1.1791.081E-
02
1.5 0.136 0.092 1.129 1.111 1.265 1.2031.081E-
02
1.5 0.143 0.099 1.142 1.118 1.285 1.2171.080E-
02
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Dead Sea
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Dead Sea
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What problems are we trying to solve?
What are our parameters?
Statement Of The Problem
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Depth_min (m) Depth_max (m) Depth_mean (m)1.5 10.000 5.810 20.000 15.020 30.000 25.030 40.000 35.040 50.000 45.050 100.000 75.0
100 150.000 125.0150 200.000 175.0200 250.000 225.0250 286.317 268.2
Setup Of The Problem
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How did we solve our research problem?
Did we make any assumptions about our solution?
Solution Of The Problem
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g m
0.741 3.736
0.761 3.755
0.687 3.679
0.628 3.616
0.512 3.488
0.486 3.459
0.391 3.344
0.417 3.376
0.496 3.471
0.498 3.472
Solution Of The Problem
€
μ =γ + 3 − 0.5exp(−6γ )
0.1 1 10 1001E-09
1E-08
1E-07
1E-06
1E-05
1E-04
1E-03
1E-02
1E-01
1E+00
1E+01
1E+02
(0.2, 10, 3)(0.2, 50, 3)(0.2, 10, 4)(0.2, 50, 4)(1, 10, 3)(1, 50, 3)(1, 10, 4)
D (mm)
f(D
) (m
m-1
)
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Solution Of The Problem
np(660)1.1041.1071.1161.1381.1351.1331.1301.1301.1321.132
€
npart =1 + Bpart0.5377+ 0.4867(μ −3)2
1.4676 + 2.2950(μ − 3)2 + 2.3113(μ − 3)4[ ]
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kp(555) kp(555)
1.313E-03 1.017E-03
1.253E-03 9.797E-04
1.809E-03 1.524E-03
2.485E-03 3.105E-03
9.727E-04 2.686E-03
7.273E-04 2.493E-03
5.712E-04 2.403E-03
5.311E-04 2.376E-03
7.166E-04 2.333E-03
6.960E-04 2.321E-03
Solution Of The Problem
€
ρ '(λ ) =4πD32nw(λ )kpart(λ )
λ
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D32 D32
1.517 0.9531.426 0.9211.675 1.0072.063 1.1272.961 1.3663.236 1.4324.327 1.6703.986 1.5993.184 1.4193.224 1.429
Solution Of The Problem
€
D32 =
D3 f (D )dDD min
D max,
∫
D2 f (D )dDD min
D max,
∫ =
(μ − 3)(Dmax4−μ −Dmin
4−μ )
(μ − 4)(Dmax3−μ −Dmin
3−μ )
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(0.555)r (0.555)r
2.466 1.550
2.402 1.552
3.035 1.824
4.481 2.447
6.256 2.885
6.734 2.979
8.792 3.394
8.116 3.256
6.611 2.947
6.666 2.954
Solution Of The Problem
€
ρ(λ ) =2πD32nw(λ )(npart −1)
λ
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Solution Of The Problem
CV(Qa) CV(Qa)
4.773E-07 6.088E-074.467E-07 5.653E-073.577E-07 4.173E-072.997E-07 2.354E-077.058E-07 2.580E-079.146E-07 2.706E-071.296E-06 3.135E-071.322E-06 3.012E-078.610E-07 2.676E-078.836E-07 2.683E-07
€
Qa =1 +2exp(−ρ ')
ρ '+
2[exp(−ρ ') −1]
ρ '( )2
€
Qc = 2 − 4 exp(−ρ tan ξ )cosξ sin(ρ − ξ )
ρ+
cosξ
ρ
⎛
⎝ ⎜
⎞
⎠ ⎟
2
cos(ρ − 2ξ ) ⎡
⎣ ⎢ ⎢
⎤
⎦ ⎥ ⎥+ 4
cosξ
ρ
⎛
⎝ ⎜
⎞
⎠ ⎟
2
cos2ξ
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Npart (mL-3) Npart (mL-3)
5.716E+06 4.452E+063.500E+06 2.788E+067.300E+06 4.947E+061.374E+07 5.623E+068.592E+07 1.338E+071.362E+08 1.629E+073.542E+08 2.897E+073.060E+08 2.483E+071.236E+08 1.569E+071.305E+08 1.605E+07
Solution Of The Problem
€
Npart =6
π Cv
(μ −4)(Dmax1−μ −Dmin
1−μ )
(μ −1)(Dmax4−μ −Dmin
4−μ )
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rpart (kg/l) rpart (kg/l)
2.25 2.25
2.28 2.28
2.33 2.33
2.49 2.49
2.46 2.46
2.45 2.45
2.43 2.43
2.43 2.43
2.45 2.45
2.44 2.44
Solution Of The Problem
€
ρpart =npart −0.7717
0.1475.
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TSM (g/m^3) TSM (g/m^3)
1.074E+00 1.370E+001.017E+00 1.287E+008.339E-01 9.728E-017.452E-01 5.854E-011.737E+00 6.349E-012.239E+00 6.623E-013.144E+00 7.607E-013.210E+00 7.314E-012.106E+00 6.544E-012.158E+00 6.552E-01
Solution Of The Problem
€
TSM = ρ partCv
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ap(412)
0.110
0.100
0.096
0.092
0.091
0.087
0.090
0.088
0.082
0.082
Displaying Absorption
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cp(412)
1.2801.2391.0790.8260.8700.8910.9530.9380.8850.885
Displaying Attenuation
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bp(412)
1.171
1.140
0.982
0.734
0.780
0.804
0.862
0.850
0.803
0.803
Displaying Backscattering
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Mathematical Solution
Not a unique solution
Where the parameters met?
Results
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Create Code to compute all 1748 Values
Provide more accurate visual of data
Future Work
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The Ocean Optics Team would like to give special thanks to Dr. Hayden, our mentors Dr. Sokoletsky, Je’aime Powell, Jeff Wood, and all faculty and staff who have helped me attain valuable resources that can be utilized in my future endeavours.
Acknowledgments
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Boss, E., W. S. Pegau, W. D. Gardner, J. R. V. Zaneveld, A. H.Barnard, M. S. Twardowski, G. C. Chang, and T. D. Dickey. 2001. The spectral particulate attenuation and particle size distribution in the bottom boundary layer of a continental shelf, J. Geophys. Res. 106: 9509–9516.
Hulst van de, H. C. 1981. Light Scattering by Small Particles. Dover Publ. Inc., New York, 470 pp. Mitchell, D. L. 2002. Effective diameter in radiative transfer: General definition, applications, and
limitations. J. Atmospheric Sciences. 59: 2330-2346. Morel, A. and A. Bricaud. 1981. Theoretical results concerning light absorption in a discrete medium and
application to specific absorption of phytoplankton. Deep-Sea Res. 28: 1375-1393. Morel, A. and A. Bricaud. 1986. Inherent optical properties of algal cells including picoplankton:
Theoretical and experimental results, pp. 521-559. In: Can. Bull. Fish. Aquat. Sci. 214. Twardowski, M. S., E. Boss, J. B. Macdonald, W. S. Pegau, A. H. Barnard, and J. R. V. Zaneveld. 1999.
Retrieving particle composition from the backscattering ratio and spectral attenuation in marine waters. URL http://argon.oce.orst.edu/biooptics/ members/twardowski/bbn_txt.pdf.
Woźniak, B. and D. Stramski. 2004. Modeling the optical properties of mineral particles suspended in seawater and their influence on ocean reflectance and chlorophyll estimation from remote sensing algorithms. Applied Optics. 43: 3489-3503.
Garber, R. A. 1980. The Sedimentology of the Dead Sea. Ph.D. Thesis, Rensselaer Polytechnic Institute, Troy, New York, USA, 169 pp
Gavrieli, I. 1997. Halite deposition in the Dead Sea: 1960-1993. pp. 161-170. In: Niemi, T., Ben- Avraham, Z., and Gat, J. R. (Eds.). The Dead Sea - The Lake and its Setting. Oxford University Press, Oxford, U.K.
Gertman, I., and A. Hecht. 2002. The Dead Sea hydrography from 1992 to 2000. J. Mar. Syst. 35: 169-181.
Sokoletsky L. Boss E. Gildor H. Department of Environmental Sciences and Energy Research, The Weizmann Institute of Science, Rehovot 76100, Israel. School of Marine Sciences, University of Maine, Orono, ME 04469
References
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QUESTIONS?