Exam 5: Soil Water: Characteristics and Behavior

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The water potential at the field capacity for most soils is in the range of -10 to -30 kPa.

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The following are characteristics of a water molecule.

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In which of the following situations would you expect downward movement of soil water through the profile to be most rapid?

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Osmotic and matric potentials are commonly negative because the soil water has a lower energy level than that of pure water.

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Water molecules have polarity primarily because each contains two H atoms and only one O atom.

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The property of cohesion in water stems from the attraction of water molecules for soil solids.

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The matric potential of soil water is _____.

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The water content in a soil is known to be .2 m3/m3 and the potential of pure water outside the system is assumed to be 0. If the soil is a clay loam you would calculate the soil water potential (in kPa) to be

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Although the total soil water content of a clay soil is about the same as a nearby well structured silt loam, the clay will likely provide more available water to plants because of its higher volume of small pores.

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Which of the following statements concerning applications or capabilities of soil moisture measuring devices is (are) true for the electrical resistance block?

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Plant roots gain access to soil water primarily by the growth of the roots into moist soil.

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The matric potential is due to the attraction of water molecules to soil solid surfaces.

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Soils high in organic matter commonly hold more available water than comparable soils with lower organic matter levels. This is most likely due to what characteristics of the high O.M. soils

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Unsaturated water flow _____________.

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The osmotic potential would likely be lowest in soils of which of the following orders

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Which of the following statements concerning applications or capabilities of soil moisture measuring devices is (are) true for the use of a drying oven and balance?

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Two soil samples, A & B, at different soil moisture levels are placed in contact with each other. Water will more likely move from soil A to soil B if their water potentials, expressed in kPa, are:

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Gypsum or nylon electrical resistance blocks are most useful in estimating the soil water content if the soil is quite dry.

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The hydrogen end of a water molecule is attracted to positively charged cations such as Na+ and Ca2+.

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The soil water potential is a measure of the potential of a soil to hold water.

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