首页> 外文期刊>Journal of the American Water Resources Association >CROPLAND RIPARIAN BUFFERS THROUGHOUT CHESAPEAKE BAY WATERSHED: SPATIAL PATTERNS AND EFFECTS ON NITRATE LOADS DELIVERED TO STREAMS
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CROPLAND RIPARIAN BUFFERS THROUGHOUT CHESAPEAKE BAY WATERSHED: SPATIAL PATTERNS AND EFFECTS ON NITRATE LOADS DELIVERED TO STREAMS

机译:切普萨克克湾水域中的科普兰RIPARIAN啤酒堡:空间格局及其对输送到河流的硝酸盐负荷的影响

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We used statistical models to provide the first empirical estimates of riparian buffer effects on the cropland nitrate load to streams throughout the Chesapeake Bay watershed. For each of 1,964 subbasins, we quantified the 1990 prevalence of cropland and riparian buffers. Cropland was considered buffered if the topographic flow path connecting it to a stream traversed a streamside forest or wetland. We applied a model that predicts stream nitrate concentration based on physiographic province and the watershed proportions of unbuffered and buffered cropland. We used another model to predict annual streamflow based on precipitation and temperature, and then multiplied the predicted flows and concentrations to estimate 1990 annual nitrate loads. Across the entire Chesapeake watershed, croplands released 92.3 Gg of nitrate nitrogen, but 19.8 Gg of that was removed by riparian buffers. At most, 29.4 Gg more might have been removed if buffer gaps were restored so that all cropland was buffered. The other 43.1 Gg of cropland load cannot be addressed with riparian buffers. The Coastal Plain physiographic province provided 52% of the existing buffer reduction of Bay-wide nitrate loads and 36% of potential additional removal from buffer restoration in cropland buffer gaps. Existing and restorable nitrate removal in buffers were lower in the other three major provinces because of less cropland, lower buffer prevalence, and lower average buffer nitrate removal efficiency.
机译:我们使用统计模型提供了河岸缓冲带对切萨皮克湾流域中溪流中农田硝酸盐负荷的初步经验估计。对于1,964个子流域中的每一个,我们都对1990年农田和河岸缓冲带的流行程度进行了量化。如果将农田与溪流相连的地形流动路径横过河岸森林或湿地,则认为农田已被缓冲。我们应用了一个模型,该模型根据地理省份以及未缓冲和缓冲农田的分水岭比例来预测河流硝酸盐浓度。我们使用另一个模型根据降水量和温度来预测年流量,然后将预测的流量和浓度相乘以估计1990年的硝酸盐负荷。在整个切萨皮克流域,农田释放了92.3 Gg的硝酸盐氮,但其中的19.8 Gg被河岸缓冲带清除了。如果恢复了缓冲间隙,则最多可以去除29.4 Gg,从而缓冲所有农田。其他的43.1 Gg农田负荷无法通过河岸缓冲带解决。沿海平原的地理省份为湾区硝酸盐负荷减少了现有缓冲区的52%,并为农田缓冲区的缓冲区中的缓冲区恢复提供了36%的潜在额外清除量。其他三个主要省份的缓冲液中现有和可恢复的硝酸盐去除率较低,这是因为耕地减少,缓冲液患病率降低以及平均缓冲液硝酸盐去除效率降低。

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