Final Study Guide - Soil Water Flashcards

1
Q

What is soil water potential and how is it related to the water content?

A

Soil-water potential is a measure of the potential energy per unit mass, volume, or weight of soil water, compared with that of pure, free water

The lower the water content, the harder it is to pull water out of the soil. The higher water content results in higher, less negative water potential, while lower water content results in lower, more negative water potential

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2
Q

What are the forces (potentials) driving water potential in soils?

A

Ψtotal = Ψg + Ψm + Ψo + Ψp

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3
Q

What is the water potential at: saturation, field capacity, permanent wilting point?

A

Saturation: 0 bar
Field capacity: -0.1 to -0.3 bar
Permanent wilting point: -15 bar

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4
Q

How is available water calculated? Why is this a more useful value for plant growth than field capacity and wilting point?

A

Available water = field capacity - permanent wilting point

More useful than either because it shows the amount of soil water in soil that is available for plants to use

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5
Q

How does texture drive available soil water content? What texture will have higher content of plant available water: sandy, loamy or clay loam?

A

Coarse textured soils have the least PAW because they mostly have large pores with limited ability to retain water

Fine textured soils have moderate PAW because they have many micropores, though much of the water held in them is unavailable

Loamy textured soils have the most PAW because they have a mix between micro and macropores

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6
Q

How does soil structure drive plant available water content?

A

It can increase plant available water by increasing/decreasing porosity to a point

It also affects how water infiltrates and percolates through soil

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7
Q

What is infiltration?

A

A process by which water enters the soil pore spaces and becomes soil water

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8
Q

How does soil texture drive saturated hydraulic conductivity? Which texture has higher saturated hydraulic conductivity? Sand, silt loam or silty clay?

A

Saturated hydraulic conductivity: When infiltration rate becomes constant due to saturation

Sandy soils have the highest saturated hydraulic conductivity

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9
Q

What is runoff?

A

Water that runs off of soil surface (instead of infiltration)

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10
Q

What is percolation?

A

Movement of water through the soil profile

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11
Q

Water flows from _____ (higher/lower) to ______ (higher/ lower) total potential energy

A

Water flows from higher to lower total potential energy

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12
Q

How to measure saturated flow (Darcy’s Law) and unsaturated flow

What potentials are considered in both?

A

Saturated flow: Gravity and pressure
Unsaturated flow: Matric

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13
Q

What causes preferential flow paths, what are impacts

A

Various factors, which can include soil fauna, plant roots, cracks in soil, and various other reasons

This means water does not saturate soil uniformly

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14
Q

What is relationship between water flow in soil and in plant?

A

Water moves from soil to plant because it moves from higher (less negative) to lower (more negative) water potential

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15
Q

What is soil water budget and what factors influence it?

A

Imagine soil water budget as a bucket model.

S = (P + I) - (R + ET + D)

P: Precipitation
I: Irrigation
ET: Evapotranspiration
R: Runoff
D: Deep percolation = discharge

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16
Q

Understand benefits and negative impacts of irrigation: trade-offs

A

Surface: $750-1100, high to low labor, 20-50% efficiency
Sprinkler: $1000-4000, medium to low labor, 60-70% efficient
Microirrigation: $1300-5000, low labor, 80-90% efficient

17
Q

What are major types and applications of irrigation technologies

A

Surface irrigation: furrow and flood
Pressurized irrigation: sprinklers and micro-irrigation

18
Q

How to understand/calculate water use efficiency

A

Water use efficiency = crop yield (kg)/water consumption (m^3)

19
Q

How can we conserve water on farms?

A

More efficient systems
Irrigation scheduling
Planning ahead