College Earth SUPPLEMENTAL EXERCISES Earth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyah 3. From Table 3, what conclusion can you make about h oils filtration rate?

Applications and Investigations in Earth Science (9th Edition)
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Chapter1: The Study Of Minerals
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Use the following information to answer question three in the pictures
College
Earth SUPPLEMENTAL EXERCISES
Earth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyahoga Community College
3. From Table 3, what conclusion can you make about how soil texture affects steady-state
oils filtration rate?
Transcribed Image Text:College Earth SUPPLEMENTAL EXERCISES Earth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyahoga Community College 3. From Table 3, what conclusion can you make about how soil texture affects steady-state oils filtration rate?
Restricted infiltration and ponding result in poor soil aeration. This leads to poor root function, poor
plant growth, nitrogen volatilization, reduced availability of nutrients for plant use, and reduced cycling
of nutrients by soil organisms.
The soil infiltration rate is most affected by conditions near the soil surface, and the rate can change
drastically as a result of management. Infiltration is rapid through large continuous pores at the soil
surface, and it slows as pores become smaller. Steady-state infiltration rates typically occur when the
soil is nearly saturated. These rates are given for various textural classes in table 3. They are
average values and should not be generalized for all soil types.
Table 3.-Steady-state infiltration rates*
(Soils are wet deep into the profile. Values should be used only for comparing to the infiltration rate of the second inch of
water applied.) *Hillel, 1982.
Soil texture & type Steady-state infiltration rate (in/hr)
Sand
>0.8
Sandy and silty soils 0.4-0.8
Loam
Clayey soils
0.2-0.4
0.04-0.2
Sodic clayey soils <0.04
12
Edited from D. Steer, The Good Earth. Also created by K. Sasowsky (Sup. Ex.3, 7, 6a, parts of Sup. Ex. A&B, part, 24, 25, 38, Sup. Alt. Energy 1 and 2, Sup. Switch
the Energy Project Discussion Questions); copyrights retained by authors, 2021.
Transcribed Image Text:Restricted infiltration and ponding result in poor soil aeration. This leads to poor root function, poor plant growth, nitrogen volatilization, reduced availability of nutrients for plant use, and reduced cycling of nutrients by soil organisms. The soil infiltration rate is most affected by conditions near the soil surface, and the rate can change drastically as a result of management. Infiltration is rapid through large continuous pores at the soil surface, and it slows as pores become smaller. Steady-state infiltration rates typically occur when the soil is nearly saturated. These rates are given for various textural classes in table 3. They are average values and should not be generalized for all soil types. Table 3.-Steady-state infiltration rates* (Soils are wet deep into the profile. Values should be used only for comparing to the infiltration rate of the second inch of water applied.) *Hillel, 1982. Soil texture & type Steady-state infiltration rate (in/hr) Sand >0.8 Sandy and silty soils 0.4-0.8 Loam Clayey soils 0.2-0.4 0.04-0.2 Sodic clayey soils <0.04 12 Edited from D. Steer, The Good Earth. Also created by K. Sasowsky (Sup. Ex.3, 7, 6a, parts of Sup. Ex. A&B, part, 24, 25, 38, Sup. Alt. Energy 1 and 2, Sup. Switch the Energy Project Discussion Questions); copyrights retained by authors, 2021.
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