roots and root-soil relations swes 316 section g

30
Roots and Root-Soil Relations SWES 316 Section G

Upload: osvaldo-toney

Post on 15-Dec-2015

215 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Roots and Root-Soil Relations SWES 316 Section G

Roots and Root-Soil Relations

SWES 316

Section G

Page 2: Roots and Root-Soil Relations SWES 316 Section G

Functions of Roots

• Absorption

• Anchorage

• Storage

Page 3: Roots and Root-Soil Relations SWES 316 Section G

Root Systems

• Tap vs. fibrous root systems

Page 4: Roots and Root-Soil Relations SWES 316 Section G

Root Systems

• Roots may occupy about 1% of total soil volume (with actively growing crops)

• In wildlands (e.g. forest, grassland), roots may represent up to 50% of total plant mass (roots + shoots)

• In agriculture, roots may represent about 25% of total plant mass

Page 5: Roots and Root-Soil Relations SWES 316 Section G

Depth of Root Systems

• Lettuce 30 cm• Cotton 120-150 cm• Alfalfa 250-300 cm• Turf 60-90 cm• Mesquite 50 m ?????

• Regardless of root system depth, the most important roots for nutrient and water uptake are usually found in the top 15-20 cm of soil.

Page 6: Roots and Root-Soil Relations SWES 316 Section G

Root Morphology

• Longitudinal– Meristematic zone– Elongation zone– Maturation zone– Mature zone

• Cross-sectional– Epidermis– Cortex– Endodermis– Stele

Page 7: Roots and Root-Soil Relations SWES 316 Section G

Root Morphology

{MeristematicZone

{ElongationZone

{MaturationZone

MatureZone

Cross-section of maturation zone

Page 8: Roots and Root-Soil Relations SWES 316 Section G

Functions

• Root cap– Protection of meristem– Secretion of mucigel– Initiation of symbiotic relationships

• Elongation Zone– Elongation of cells forces root through the

soil• Maturation zone

– Root Hairs– Major zone of water and nutrient uptake

Page 9: Roots and Root-Soil Relations SWES 316 Section G

Root Hairs

• Single-cell extensions of epidermal cells• Tremendously important for providing

surface area for water and nutrient uptake

• Produced in the maturation zone• Sites of infection by pathogens, N fixing

bacteria, and mycorrhizae

Page 10: Roots and Root-Soil Relations SWES 316 Section G

Root Hairs

• Root hairs can account for 2/3 of total root surface area.

• Root hairs are fragile and susceptible to breakage as soils dry.

Germinatingradish seedlingwith root hairs.

Page 11: Roots and Root-Soil Relations SWES 316 Section G

Size of Roots

• Fine lateral roots are 0.1 to 0.2 mm in diameter.

• Root hairs are 0.01 to 0.05 mm in diameter.

• Soil “micropores” are considered to be those <0.08 mm in diameter.

• Therefore, root hairs are important for accessing water and nutrients in micropores.

Page 12: Roots and Root-Soil Relations SWES 316 Section G

Mature Roots

• The root epidermis and endodermis become covered with a waxy substance known as “suberin”.

• Function:Water and nutrient uptake rates are lower in mature root zones than in immature:– Lower permeability– Formation of aerenchyma (air pockets)

Protects the root from desiccation

Page 13: Roots and Root-Soil Relations SWES 316 Section G

Cross-section of mature zone

Page 14: Roots and Root-Soil Relations SWES 316 Section G

Aerenchyma

EasternGamagrassroots

Page 15: Roots and Root-Soil Relations SWES 316 Section G

Driptubing

Lettuce

Page 16: Roots and Root-Soil Relations SWES 316 Section G

Implications of Root Morphology• The youngest part of the root is more permeable

to water and nutrients than is the older part (behind the maturation zone).

• Most nutrients are taken up in the younger root zone (‘feeder roots’) with abundant root hairs.

• Excessive soil drying and mechanical disturbance will damage young roots, reduce nutrient uptake.

Page 17: Roots and Root-Soil Relations SWES 316 Section G

The Rhizosphere

• Definition: a zone of soil where microbial activity is influenced by roots

• Why? Border cells, root leakage and secretion of organic compounds

• May extend to about 2 mm from root surface.

Page 18: Roots and Root-Soil Relations SWES 316 Section G

The Rhizosphere

Properties:– Higher available C for microbial growth– Higher microbial population and activity– Lower pH than “bulk” soil– Lower O2 than “bulk” soil

– Altered nutrient availability for plants

Page 19: Roots and Root-Soil Relations SWES 316 Section G

Organic C in the Rhizosphere (Rhizodeposition)

• Plants release simple and complex carbohydrates, nucleic acids, enzymes into the rhizosphere

• These compounds are used by microorganisms as sources of C and energy.

• Up to 30% of plant C fixed in photosynthesis may be released from roots.

Page 20: Roots and Root-Soil Relations SWES 316 Section G

Importance of the Rhizosphere

• A healthy rhizosphere will help plants by:– Increasing nutrient availability– Suppressing pathogens– Increasing water availability

• However, the effects of agricultural management on the rhizosphere are still largely unknown.

Page 21: Roots and Root-Soil Relations SWES 316 Section G

Mycorrhizae

Ectomycorrhizae

Endomycorrhizae

Page 22: Roots and Root-Soil Relations SWES 316 Section G

Mycorrhizae

Many of the mushrooms you see in the forest are

mycorrhizal fruiting bodies.

Page 23: Roots and Root-Soil Relations SWES 316 Section G

Mycorrhizae

• A fungal-root symbiosis– increase root length and surface area– help plants to take up nutrients that are “immobile”

in soil (e.g. P)– inhibit heavy metal uptake– iIncrease water uptake by roots– are vital for the growth and survival of plants where

nutrients are likely to be limiting, and/or where heavy metals are problems

Page 24: Roots and Root-Soil Relations SWES 316 Section G

Managing Mycorrhizae

• About 80% of all plants have mycorrhizael associations.

• Innoculation (addition) with mycorrhizae is often used for nursery and forestry plantings.

• Addition of mycorrhizae to agricultural soils has shown few benefits so far:– Difficulty of establishing Endo fungi

Page 25: Roots and Root-Soil Relations SWES 316 Section G

Nitrogen Fixation

• Definition: The conversion of atmospheric N2 to forms usable by plants.

• Certain bacteria and actinomycetes can carry out N fixation.

• The most important N fixation occurs through a symbiotic relationship between legume roots and bacteria.

Page 26: Roots and Root-Soil Relations SWES 316 Section G

Legume Root Nodules

Within nodules, bacteria of the genus Rhizobium reduce N2 toNH3. The NH3 is then used byThe plant as an N source.

Page 27: Roots and Root-Soil Relations SWES 316 Section G

Nitrogen Fixation

• Legumes commonly form N-fixation symbioses

• N fixation is not free– may cost the plant up to 30% of the C it

captures from the atmosphere in photosynthesis

• Rate of N fixation is inversely proportional to available N in the soil.

Page 28: Roots and Root-Soil Relations SWES 316 Section G

Importance of N Fixation

• Legume crops can derive virtually all their N requirement through N fixation.

• In crop rotations, legume crop residues can be incorporated into the soil. Upon decomposition, N is released.

• Legumes and non-legumes can be grown together—in this case 20-50% of the N fixed in the legume may become available to the non-legume.

Page 29: Roots and Root-Soil Relations SWES 316 Section G

Final Thoughts on Roots

• Root system is responsible for water and nutrient uptake.

• The youngest part of the root system is responsible for much of this uptake– Root hairs are critical, fragile and can be easily

damaged by compaction, tillage, etc.

• The root system is dynamic and will respond to changes in soil conditions.

Page 30: Roots and Root-Soil Relations SWES 316 Section G

Final Thoughts (2)

• The root is part of a microbial community known as the rhizosphere

• A healthy rhizosphere is important for plant health– There’s a lot about it we don’t know yet

• Mycorrhizae - water, nutrients, pathogen protection

• Rhizobia - N fixation