Item talk:Q262940
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "River channel response to dam removals on the lower Penobscot River, Maine, United States", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70227619", "url": "https://pubs.usgs.gov/publication/70227619" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70227619 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1002/rra.3700", "url": "https://doi.org/10.1002/rra.3700" } ], "journal": { "@type": "Periodical", "name": "River Research and Applications", "volumeNumber": "36", "issueNumber": "9" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "River Research and Applications" } ], "datePublished": "2020", "dateModified": "2022-01-21", "abstract": "Most geomorphology studies of dam removals have focused on sites with appreciable quantities of stored sediments. There is great interest in channel responses to sediment releases because of potential effects on aquatic and riparian habitats and human uses of these areas. Yet, behind many dams in the Northeast U.S. and other regions of the world only minor accumulations of sediment are present because of small impoundments, run\u2010of\u2010river dam design and management (inflow \u2248 outflow), low watershed sediment yield, and/or channel beds dominated by coarse sediment and/or bedrock. The two lowermost dams on the Penobscot River in Maine, United States, removed in 2012\u20132013, exemplified those conditions. Great Works and Veazie dams were about 6 and 10 m high, respectively. Pre\u2010project geophysical surveys showed coarse substrates dominated the reservoir beds and little sediment was stored in either impoundment\u2014functions of reach geology, late Quaternary history, and upstream dams. Repeat cross\u2010section surveys in each impoundment, as well as the upstream and downstream reaches, were completed from 2009 to 2015 to evaluate channel morphology responses to the removals. Bed\u2010sediment grain size and turbidity were also measured to characterize changes in bed texture and suspended sediment. Pre\u2010 and post\u2010removal survey comparisons confirmed the expectation that bed elevations, channel shapes, and channel positions would not change substantially. Changes were often within, or close to, our estimated random measurement error. Our study shows that large\u2010scale physical changes are likely to be minimal when impoundments storing relatively little sediment are removed from erosion\u2010resistant streambeds. Many dams eligible for removal have these characteristics, making these observations an important case study that is largely unrepresented in the dam removal literature.", "description": "12 p.", "publisher": { "@type": "Organization", "name": "Wiley" }, "author": [ { "@type": "Person", "name": "Collins, Mathias J.", "givenName": "Mathias J.", "familyName": "Collins" }, { "@type": "Person", "name": "Lombard, Pamela J.", "givenName": "Pamela J.", "familyName": "Lombard", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-0983-1906", "url": "https://orcid.org/0000-0002-0983-1906" }, "affiliation": [ { "@type": "Organization", "name": "New England Water Science Center", "url": "https://www.usgs.gov/centers/new-england-water-science-center" } ] }, { "@type": "Person", "name": "Kelley, Alice R.", "givenName": "Alice R.", "familyName": "Kelley", "affiliation": [ { "@type": "Organization", "name": "University of Maine Orono" } ] } ], "funder": [ { "@type": "Organization", "name": "New England Water Science Center", "url": "https://www.usgs.gov/centers/new-england-water-science-center" } ], "spatialCoverage": [ { "@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/4074035" }, { "@type": "Place", "additionalType": "state", "name": "Maine" }, { "@type": "Place", "additionalType": "unknown", "name": "Penobscot River", "url": "https://geonames.org/4974993" }, { "@type": "Place", "geo": [ { "@type": "GeoShape", "additionalProperty": { "@type": "PropertyValue", "name": "GeoJSON", "value": { "type": "FeatureCollection", "features": [ { "type": "Feature", "properties": {}, "geometry": { "type": "Polygon", "coordinates": [ [ [ -68.71879577636719, 44.825682303800384 ], [ -68.70986938476562, 44.81350585216505 ], [ -68.68377685546875, 44.82324721919215 ], [ -68.6920166015625, 44.83736927811443 ], [ -68.66661071777344, 44.85684230221507 ], [ -68.66111755371094, 44.872415981701394 ], [ 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