Chemical and detrital features of Palouse River, Idaho, runoff flowage

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Chemical and detrital features of Palouse River, Idaho, runoff flowage Item Info

Title:: Chemical and detrital features of Palouse River, Idaho, runoff flowage
Authors:: Buscemi, Philip A.
Date Created (ISO Standard):: 1969
Description:: Some aspects of runoff flowage in the Palouse River, Latah County, Idaho, are described. Certain chemical features and variations in organic and inorganic content of suspended detritus are emphasized for a 20-mile length of this northern Idaho river as affected by spring runoff. A discussion of changes in seston fractions as functions of rainfall, snow melt, feeder stream inflow, and mill pond effect is presented. Variations in certain chemical factors may be used to pinpoint two major sources of runoff water (ground water or snow melt) in the Palouse River. Sedimentary organic deposits were highly variable along the stream concourse, reflecting pollution by localized lumbering and ranching activities. PDF available at http://www.jstor.org/stable/pdfplus/3543751.pdf
Subjects:: Runoff detritus Palouse River
IWRRI number:: DOI: 10.2307/3543751
Rights:: http://www.jstor.org/page/info/about/policies/terms.jsp
Publisher:: Wiley-Blackwell
Contributing Institution:: University of Idaho
Type:: Text
Format:: application/pdf
Cataloger:: Jodi Haire

Source

Preferred Citation:: "Chemical and detrital features of Palouse River, Idaho, runoff flowage", Idaho Waters Digital Library, University of Idaho Library Digital Collections, https://www.lib.uidaho.edu/digital/iwdl/items/iwdl-jstor_3543751.html

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