Physical Geology
16th Edition
ISBN: 9781259916823
Author: Plummer, Charles C., CARLSON, Diane H., Hammersley, Lisa
Publisher: Mcgraw-hill Education,
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Chapter 5, Problem 10TYK
Summary Introduction
The structure of soil horizons that form in a humid climate and the way in which they form.
Introduction:
On studying the soil profile, it has been seen that soil arranges itself in the form of layers. The uppermost layers are usually dark, while the inner layers are lighter. There is a transitional arrangement of layers and no solid boundaries are seen between the layers. These layers are also called the horizons of soil.
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44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called
A) frost layer
B) permafrost
C) active layer
D) discontinuous permafrost
Use the attached piezometer map to make your own, clean version of the map, and indicate the elevation of the water table at all piezometer locations.
Draw equipotential lines (lines of equal water table elevation) using regular intervals – creating a contoured map of the water table.
Determine the direction of groundwater flow based on the horizontal gradient. Label the areas of recharge and discharge directly on your map.
Flow lines: Draw flow lines on your water table map. The lines should be at right angles to the equipotential lines and extend from the recharge area to the discharge area.
Hydraulic Gradient, Specific Discharge (Darcy Flux), Average Linear Velocity:
Using your water table map, estimate an average hydraulic gradient between two locations, call them locations A and B, one at the eastern-most and a second at the western-most extent of your dataset (note the north arrow on the map).
Calculate the specific discharge, q, between the two locations. For this calculation…
Calculate all the values of table 1:
Q in (L/day)
Q out (L/day)
Residence time (days)
Please show all steps
Chapter 5 Solutions
Physical Geology
Ch. 5 - Prob. 1TYKCh. 5 - Prob. 2TYKCh. 5 - Prob. 3TYKCh. 5 - Prob. 4TYKCh. 5 - Prob. 5TYKCh. 5 - Prob. 6TYKCh. 5 - Prob. 7TYKCh. 5 - Prob. 8TYKCh. 5 - Prob. 9TYKCh. 5 - Prob. 10TYK
Ch. 5 - Prob. 11TYKCh. 5 - Prob. 12TYKCh. 5 - Prob. 13TYKCh. 5 - Prob. 14TYKCh. 5 - Prob. 15TYKCh. 5 - Prob. 16TYKCh. 5 - Prob. 17TYKCh. 5 - Prob. 18TYKCh. 5 - Prob. 19TYKCh. 5 - Prob. 20TYKCh. 5 - Prob. 21TYKCh. 5 - Prob. 22TYKCh. 5 - Prob. 1EYKCh. 5 - Prob. 2EYKCh. 5 - Prob. 3EYKCh. 5 - Prob. 4EYK
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- 43) Glacial abrasion is when A) boulders are fragmented into smaller particles under the weight of the overlying ice. B) blocks of rocks are plucked from the underlying bedrock. C) rocks are carried at the base of a glacier and grind away at the underlying bedrock. D) debris fall onto the top of the glacier and are carried down glacier.arrow_forward34) Which of the following is true of soils? A) Soils rich in mineral matter are usually dark in colour. B) They usually require hours or days to form. C) Their development is affected by climate and organisms. D) Their properties are not affected by the type of rock from which they form. E) Older soils usually have fewer horizons than younger soils.arrow_forward44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called A) frost layer B) permafrost C) active layer D) discontinuous permafrostarrow_forward
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