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1974 Nonflood-Stage Chemical Loads of the Buffalo River, Arkansas

Year: 1976

Type: article

Abstract: Dissolved Ca, Mg, Na, K, Fe, Mn, and Zn loads of the Buffalo River generally show trends along the river attributable to changes in geology and vary with the season because of concentration by evapotranspiration and dilution by rain. Suspended material element loads show neither seasonal trends nor trends along the river. The Fe load for the river is predominantly in the suspended material, the Mn load is divided approximately evenly between dissolved and suspended material, and Ca, Mg, Na, K, and Zn are predominantly in the dissolved load.

Source: Journal of the Arkansas Academy of Science

Authors: Kenneth F. Steele, George H. Wagner

Language: English

Topic: Water Quality and Resources Studies

Subfield: Water Science and Technology

Field: Environmental Science

Domain: Physical Sciences

SDG: Clean water and sanitation

Open Access status: green

Funders: U.S. Department of the Interior, Water Resources Research Institute, North Carolina State University, National Park Service

Award: G2964458679

OpenAlex ID: W2621490924

FWCI:

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