How would 20 g of atrazine be distributed between a water and sediment layer in a ditch that is 50 m long, 3 m wide, and 100 cm deep. The layer of water is approximately 5 cm deep. Assume the system is in equillibrium.

How would 20 g of atrazine be distributed between a water and sediment layer in a ditch that is 50 m long, 3 m wide, and 100 cm deep. The layer of water is approximately 5 cm deep. Assume the system is in equillibrium.

Principles of Geotechnical Engineering (MindTap Course List)

9th Edition

ISBN:9781305970939

Author:Braja M. Das, Khaled Sobhan

Publisher:Braja M. Das, Khaled Sobhan

Chapter7: Permeability

Section: Chapter Questions

Problem 7.23P

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Principles of Seepage

In hydrology, when water flows down in a pore or crack of unsaturated soil due to gravity, the deep layer of soil is called seepage. It is the slow movement of water in the soil layer. Seepage is mainly found near hydraulic structures and is responsible for the stability of earthen-type hydraulic structures.

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