Item talk:Q73096
From geokb
{
"USGS Publications Warehouse": { "schema": { "@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Analysis of suspended-sediment concentrations and radioisotope levels in the Wild Rice River basin, northwestern Minnesota, 1973-98", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "wri014192", "url": "https://pubs.usgs.gov/publication/wri014192" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 33025 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/wri014192", "url": "https://doi.org/10.3133/wri014192" } ], "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Water-Resources Investigations Report" } ], "datePublished": "2001", "dateModified": "2018-03-05", "abstract": "We examined historical suspended-sediment data and activities of fallout radioisotopes (lead-210 [210Pb], cesium-137 [137Cs], and beryllium-7 [7Be]) associated with suspended sediments and source-area sediments (cultivated soils, bank material, and reference soils) in the Wild Rice River Basin, a tributary to the Red River of the North, to better understand sources of suspended sediment to streams in the region. Multiple linear regression analysis of suspended-sediment concentrations from the Wild Rice River at Twin Valley, Minnesota indicated significant relations between suspended-sediment concentrations and streamflow. Flow-adjusted sediment concentrations tended to be slightly higher in spring than summer-autumn. No temporal trends in concentration were observed during 1973-98. The fallout radioisotopes were nearly always detectable in suspended sediments during spring-summer 1998. Mean\u00a0210Pb and\u00a07Be activities in suspended sediment and surficial, cultivated soils were similar, perhaps indicating little dilution of suspended sediment from low-isotopic-activity bank sediments. In contrast, mean\u00a0137Cs activities in suspended sediment indicated a mixture of sediment originating from eroded soils and from eroded bank material, with bank material being a somewhat more important source upstream of Twin Valley, Minnesota; and approximately equal fractions of bank material and surficial soils contributing to the suspended load downstream at Hendrum, Minnesota. This study indicates that, to be effective, efforts to reduce sediment loading to the Wild Rice River should include measures to control soil erosion from cultivated fields.", "description": "iv, 21 p.", "publisher": { "@type": "Organization", "name": "U.S. Geological Survey" }, "author": [ { "@type": "Person", "name": "Brigham, Mark E. mbrigham@usgs.gov", "givenName": "Mark E.", "familyName": "Brigham", "email": "mbrigham@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-7412-6800", "url": "https://orcid.org/0000-0001-7412-6800" }, "affiliation": [ { "@type": "Organization", "name": "Minnesota Water Science Center", "url": "https://www.usgs.gov/centers/upper-midwest-water-science-center" } ] }, { "@type": "Person", "name": "McCullough, Carolyn J.", "givenName": "Carolyn J.", "familyName": "McCullough" }, { "@type": "Person", "name": "Wilkinson, Philip M.", "givenName": "Philip M.", "familyName": "Wilkinson" } ], "funder": [ { "@type": 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