Item talk:Q244786
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Sedimentation in mountain streams: A review of methods of measurement", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70173427", "url": "https://pubs.usgs.gov/publication/70173427" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70173427 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.4236/nr.2013.41011", "url": "https://doi.org/10.4236/nr.2013.41011" } ], "journal": { "@type": "Periodical", "name": "Natural Resources", "volumeNumber": "4", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Natural Resources" } ], "datePublished": "2013", "dateModified": "2016-06-20", "abstract": "The goal of this review paper is to provide a list of methods and devices used to measure sediment accumulation in wadeable streams dominated by cobble and gravel substrate. Quantitative measures of stream sedimentation are useful to monitor and study anthropogenic impacts on stream biota, and stream sedimentation is measurable with multiple sampling methods. Evaluation of sedimentation can be made by measuring the concentration of suspended sediment, or turbidity, and by determining the amount of deposited sediment, or sedimentation on the streambed. Measurements of deposited sediments are more time consuming and labor intensive than measurements of suspended sediments. Traditional techniques for characterizing sediment composition in streams include core sampling, the shovel method, visual estimation along transects, and sediment traps. 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