Moisture and energy conditions within a sloping soil mass during drainage. Hewlett, undefined & A. R. Hibbert, J. D. 1963.
Moisture and energy conditions within a sloping soil mass during drainage. [pdf]Paper  abstract   bibtex   
A model of a sloping soil profile is used to show that slow, unsaturated flow of soil moisture above the water table furnishes much of the sustained streamflow between storms in mountain land.
@article{hewlett_moisture_1963,
	title = {Moisture and energy conditions within a sloping soil mass during drainage.},
	url = {http://cwt33.ecology.uga.edu/publications/859.pdf},
	abstract = {A model of a sloping soil profile is used to show that slow, unsaturated flow of soil moisture above the water table furnishes much of the sustained streamflow between storms in mountain land.},
	author = {Hewlett, {and} A. R. Hibbert, J. D.},
	year = {1963},
	keywords = {CWT}
}
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