首页> 外文期刊>Hydrology and Earth System Sciences >Changing suspended sediment in United States rivers and streams: linking sediment trends to changes in land use/cover, hydrology and climate
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Changing suspended sediment in United States rivers and streams: linking sediment trends to changes in land use/cover, hydrology and climate

机译:在美国河流和流中改变悬浮沉积物:将沉积物趋势与土地使用/封面,水文和气候的变化联系起来

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Sediment is one of the leading pollutants in rivers and streams across the United States (US) and the world. Between 1992 and 2012, concentrations of annual mean suspended sediment decreased at over half of the 137 stream sites assessed across the contiguous US. Increases occurred at less than 25 % of the sites, and the direction of change was uncertain at the remaining 25 %. Sediment trends were characterized using the Weighted Regressions on Time, Discharge, and Season (WRTDS) model, and decreases in sediment ranged from ?95 % to ?8.5 % of the 1992 concentration. To explore potential drivers of these changes, the sediment trends were (1)?parsed into two broad contributors of change, changes in land management versus changes in the streamflow regime, and (2)?grouped by land use of the watershed and correlated to concurrent changes in land use or land cover (land use/cover), hydrology and climate variables and static/long-term watershed characteristics. At 83 % of the sites, changes in land management (captured by changes in the concentration–streamflow relationship over time; C–Q relationship) contributed more to the change in the sediment trend than changes in the streamflow regime alone (i.e., any systematic change in the magnitude, frequency or timing of flows). However, at 50 % of the sites, changes in the streamflow regime contributed at least a 5 % change in sediment, and at 11 sites changes in the streamflow regime contributed over half the change in sediment, indicating that at many sites changes in streamflow were not the main driver of changes in sediment but were often an important supporting factor. Correlations between sediment trends and concurrent changes in land use/cover, hydrology and climate were often stronger at sites draining watersheds with more homogenous, human-related land uses (i.e., agricultural and urban lands) compared to mixed-use or undeveloped lands. At many sites, decreases in sediment occurred despite small-to-moderate increases in the amount of urban or agricultural land in the watershed, suggesting conservation efforts and best-management practices (BMPs) used to reduce sediment runoff to streams may be successful, up to a point, as lands are converted to urban and agricultural uses.
机译:沉积物是美国(美国)和世界各地的河流和溪流领先的污染物之一。在1992年至2012年期间,在整个邻近的美国评估的137个流网站的一半超过一半的半平均悬浮沉积浓度下降。增加发生在不到25%的地点,而变化的方向在其余25%的情况下不确定。使用对时间,放电和季节(WRTD)模型的加权回归的沉积物趋势,并且沉积物的减少范围为95%至1992年浓度的8.5%。为了探索这些变化的潜在驱动因素,沉积物趋势是(1)?分为两个广泛的变革贡献者,土地管理的变化与流流程制度的变化,(2)?通过土地利用分流和相关土地使用或陆地覆盖(土地使用/封面),水文和气候变量以及静态/长期流域特征的同时变化。在83%的地点,土地管理的变化(随着时间的推移浓缩 - 流式流出关系的变化; C-Q关系)贡献了沉积物趋势的变化,而不是单独的流流程中的变化(即,任何系统流动的幅度,频率或时序的变化)。但是,在> 50%的站点中,Stream流程制度的变化贡献了至少5%的沉积物变化,并且在11个站点中,流流程的变化贡献超过沉积物变化的一半,表明在许多网站中的流出变化不是沉积物变化的主要驱动因素,但往往是一个重要的支持因素。与混合使用或未开发的土地相比,沉积物趋势和土地利用/覆盖,水文和气候变化的相关性趋势与土地使用/覆盖的并发变化,水文和气候变化往往较强。在许多地点,尽管流域的城市或农业土地的数量小,但暗示保护努力和用于减少泥沙径流的最佳管理实践(BMP),可能会成功到了一点,因为土地被转变为城市和农业用途。

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