Water in The Soil-Plant System Flashcards

1
Q

Imports and exports of soil water

A

Rainfall, precipitation, evapotranspiration, groundwater flow…

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2
Q

What does water movement depend on?

A

Conc grad, gravitational, pressure, solute and matric

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3
Q

Porosity as a water store…

A

Adhesion/Cohesion properties of clay/colloidal material

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4
Q

Clay and humus in storage…

A

Determine surface are for which soil can be held

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5
Q

Pore in storage…

A

Amount/proportions/continuity

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6
Q

Water Potential

A

Relative energy level of water in a volume of soil, being 0 when saturated, water potential decreasing as soils dry

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7
Q

Modes of water movement…

A

Evapotranspiration
Soils gradients

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8
Q

What does soil water flow rate depend on?

A

Gradients in height, pressure, solutes and soil wetness, surface friction or poor constriction

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9
Q

Hydraulic Conductivity

A

Ease of water movement through pores

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10
Q

Saturated FLOW

A

Stronger capillary/surface forces in small pores, little flow until pressure forces movement, improving water holding capacity, impeding drainage

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11
Q

Darcy’s Law

A

This says flow of a liquid at any point is given by fluid pressure gradient, viscosity of the fluid and effective permeability

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12
Q

What is total water potential a sum of?

A

Gravity, pressure, matric and solutes

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13
Q

Importance of gravity/pressure?

A

Drives water movement, osmotic effect, suction or tension on water surfaces

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14
Q

Matric Potential

A

Binding of water to materials and enclosure in capillaries/other fine pores

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15
Q

Relationship of water potential and water content…

A

Proportional

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16
Q

Where are water vapor gradients most common?

A

Leaf/Soil surface
roots

17
Q

Where is saturated flow?

A

Dominates beneath water table, flooding soils, and irrigation/heavy rain infiltration

18
Q

Where is unsaturated flow?

A

Air obstructs it in largest pores, thus flows through the smallest pores remaining filled with water

19
Q

What does field capacity?

A

Upper limit of which water is useful to plants: permanent wilting point with further drying

20
Q

Where does transpiration dominate?

A

Drying soils, low evaporation due to uncoductivity and dryness, with large surface area allowing dominant transpiration

21
Q
A