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• W2364088451 abstract "The upper half of one watershed and the lower half of another were deforested and maintained barren from 1965 to 1967. Forest on the remaining halves was cut in 1968. Water yield increases from both watersheds averaged almost 6 inches during the half de- forested stage and rose to over 10 inches after complete deforestation. The duratœon of the  flows greatly increased on both watersheds. Other hydrologic effects (instantaneous peak flows, stream temperature, specific conductance, and turbidity) were greater on the lower half deforested watershed. These results show again that forest cutting causes substantial increases in streamflow, but, more important, they provide some landmark values on hy- drologic effects of complete deforestatœon. To observe the quantity, regimen, and winter or early spring. It is a common, but quality of streamflow from deforested water- unnecessary, consequence of the harvesting of sheds and to compare hydrologic effects of timber that water draining from the cutover deforesting upper and lower slopes, the upper land is turbid and that this turbidity originates half of one watershed and the lower half of primarily on poorly designed forest roads another were cleared and maintained free of (Packer, 196.7). Ordinarily all of these hydro- regrowth. Three years later, the remaining logic effects are maximized by clear-cutting in forested halves of the watersheds were also which the greatest volume per acre of forest cleared. A third watershed was retained as a growth is harvested. forested control throughout the experiment. Most watershed experiments show that forest TI-IE EXPERIMENTAL WATERSHEDS, THEIR cutting increases annual streamflow in rough INSTRUMENTATION AND THEIR TREATMENT proportion to the amount of vegetation re- The experiments were conducted on the moved (Hibbert'1967). Because careful forest Fernow Experimental Forest near Parsons, cutting seldom affects infiltration rates, these West Virginia. The Forest is in the Allegheny streamflow increases are rarely accompanied by mountain section of the Appalachian plateau. increased overland flow (Hoover, 196.2). In- The predominant soil is Calvin silt loam (U.S. creased streamflows are attributed to decreased Department of Agriculture,, 1967) underlain evaporative losses (Lull and Reinhart, 1967) with fractured sandstone and shale, and the and, in mild climates, they tend to occur during elevation of the forest is about 2500 feet. A1- the growing season (Hibbert, 1967). The few though precipitation is well distributed during analyses published (Johnson and Meginnis, most years, high evaporative losses usually 1960; Reinhart eal., 1963; Rothacker, 1965) reduce the flow in small forest streams to very show that the harvesting of timber considerably low levels by late summer. Potential evapo- augments the normally low flows of late sum- transpiration was estimated to be 22 inches ruer and early fall but, outside the snowpack per year (Pattic and Goswami, 1968). The region, has little effect on peak flows .of late growing season is defined as May through Oc-" @default.
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• W2364088451 date "1971-01-01" @default.
• W2364088451 modified "2023-09-27" @default.
• W2364088451 title "Hydrologic Effects Deforesting Two Mountain Watersheds" @default.
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