Chapter 4 Flashcards
(85 cards)
The water content and the rate of water movement in soils depend to a large extent on ___ and ___
soil type and soil structure.
have a relatively low surface particles may be 1 mm or more in diameter
Sandy Soils
have a relatively low surface area per gram of soil and have large spaces or channels between particles
Sandy Soils
have particles that are smaller than 2 µm in diameter
clay Soils
have much greater surface areas and smaller channels between particles
clay soils
with the aid of organic substances such as ___(decomposing organic matter), clay particles may aggregate into “___” that help improve soil ___ and ____
of water
humus;
crumbs;
aeration and infiltration
Water in the soil may exist as a __adhering to the surface of the soil particles, or it may
fill the entire channel between particles
film
- the spaces in between particles are large that water drains from them;
water remains only on the soil particle surfaces and at interstices between soil
particles
sandy soils
- water does not freely drain from them and is held more tightly
clay soils
- the moisture-holding capacity of soils.
Field capacity
___is the water content of a soil after it has been saturated with water and
excess water has been allowed to drain away.
Field capacity
these soils have a large field capacity
clay soils or soils with humus
clay soils might retain ___ by volume a few days after being saturated unlike
sandy soils, which retain ___ by volume after saturation
40% water; 3% water
A ____ in Soil Water Lowers Soil Water Potential
Negative Hydrostatic Pressure
Soil has water potentials and can be dissected into two components:
o Osmotic Potential
o Hydrostatic Pressure
the osmotic potential of soil water is generally ___ because solute
concentrations are ___
negligible; low
for wet soils, Ψp is very close to ___
▪ as a soil dries out, Ψp ___ and can become quite ___
zero;
decreases; negative
The soil is a mixture of (4)
particles
(sand, clay, silt, and organic material), water, dissolved solutes, and air.
At the air–water
interfaces, this recession causes the surface of the soil solution to develop ______
(curved interfaces between air and water marked in the figure by arrows), and brings the
solution into___ by surface tension.
concave menisci;
tension (negative pressure)
Because of ___, water tends to cling to the surfaces of
soil particles, so a large ___between soil water and soil air develops.
adhesive forces; surface area
As the water content of the soil decreases, the water recedes into the interstices
between soil particles, and the air–water surface develops ___
curved air–water interfaces.
The value of Ψp in soil water can become quite ___ because the ___ of
curvature of air–water surfaces may become __ in drying soils
negative; radius; very small
Water moves through soils predominantly by ___driven by a ___
bulk flow;
pressure gradient.
The rate of water flow in soils depends on two factors:
Size of the pressure gradient through the soil;
Soil hydraulic conductivity