2018
DOI: 10.1080/17480930.2018.1516938
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Predicting erosion at valley fills with two reclamation techniques in mountainous terrain

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Cited by 6 publications
(4 citation statements)
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“…5). Our findings are consistent with empirical modeling suggesting that the vegetated state of the post-MTR/VF landscape governs short-term erosion (Sears et al, 2020), and further points to shortterm vegetation recovery remaining a key control on sediment export over millennia.…”
Section: Topographic and Vegetation Controls On Post-mtr/vf Erosionsupporting
confidence: 89%
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“…5). Our findings are consistent with empirical modeling suggesting that the vegetated state of the post-MTR/VF landscape governs short-term erosion (Sears et al, 2020), and further points to shortterm vegetation recovery remaining a key control on sediment export over millennia.…”
Section: Topographic and Vegetation Controls On Post-mtr/vf Erosionsupporting
confidence: 89%
“…This suggests that as long as mine reclamation involves building valley fill landforms that have high slope and high drainage area, flowing water will leverage the resulting geomorphic disequilibrium to re-establish a drainage network, driving erosion of the valley fill surface that will outpace that of adjacent natural landforms. Even establishing engineered, armored channels along the margins of valley fills can in some cases prove ine↵ective at stopping gullying (Reed and Kite, 2020;Sears et al, 2020). Our work speaks to the potential importance of Geomorphic Landform Design (e.g., Hancock et al, 2003;Lowry et al, 2013;DePriest et al, 2015;Hancock et al, 2020a), the practice of building landforms that have slope-area distributions as similar as possible to the pre-mining landscape.…”
Section: Implications For Managementmentioning
confidence: 89%
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“…Vegetation e↵ects can be incorporated into models for post-MTR/VF landscape change in a bewildering array of ways: increases in the threshold stress for sediment entrainment by overland flow (e.g., Collins et al, 2004;Rengers et al, 2016); increases in soil cohesion and therefore stability of slopes (Schmidt et al, 2001;Simon and Collison, 2002); increases in land-surface roughness, infiltration, and interception of rainwater, reductions in the discharge, velocity, and erosive power of overland flow (Evans and Willgoose, 2000;Marston, 2010;Istanbulluoglu and Bras, 2005); and/or more generic decreases in land-surface erodibility (Evans and Willgoose, 2000;Istanbulluoglu and Bras, 2005;Sears et al, 2020;Bower et al, in review).…”
Section: Incorporating Erodibility Alterations Into Modelsmentioning
confidence: 99%