College Earth SUPPLEMENTAL EXERCISES Earth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyah 3. From Table 3, what conclusion can you make about h oils filtration rate?
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)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
Related questions
Question
Use the following information to answer question three in the pictures

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?

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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