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首页> 外文期刊>Environmental Research Letters >The role of precipitation type, intensity, and spatial distribution in source water quality after wildfire
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The role of precipitation type, intensity, and spatial distribution in source water quality after wildfire

机译:野火后降水类型,强度和空间分布在源水水质中的作用

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Storms following wildfires are known to impair drinking water supplies in the southwestern United States, yet our understanding of the role of precipitation in post-wildfire water quality is far from complete. We quantitatively assessed water-quality impacts of different hydrologic events in the Colorado Front Range and found that for a three-year period, substantial hydrologic and geochemical responses downstream of a burned area were primarily driven by convective storms with a 30 min rainfall intensity 10 mm h?1. These storms, which typically occur several times each year in July–September, are often small in area, short-lived, and highly variable in intensity and geographic distribution. Thus, a rain gage network with high temporal resolution and spatial density, together with high-resolution stream sampling, are required to adequately characterize post-wildfire responses. We measured total suspended sediment, dissolved organic carbon (DOC), nitrate, and manganese concentrations that were 10–156 times higher downstream of a burned area compared to upstream during relatively common (50% annual exceedance probability) rainstorms, and water quality was sufficiently impaired to pose water-treatment concerns. Short-term water-quality impairment was driven primarily by increased surface runoff during higher intensity convective storms that caused erosion in the burned area and transport of sediment and chemical constituents to streams. Annual sediment yields downstream of the burned area were controlled by storm events and subsequent remobilization, whereas DOC yields were closely linked to annual runoff and thus were more dependent on interannual variation in spring runoff. Nitrate yields were highest in the third year post-wildfire. Results from this study quantitatively demonstrate that water quality can be altered for several years after wildfire. Because the southwestern US is prone to wildfires and high-intensity rain storms, the role of storms in post-wildfire water-quality impacts must be considered when assessing water-quality vulnerability.
机译:在美国西南部,因野火引起的风暴会损害饮用水供应,但我们对降水在野火后水质中的作用的了解还远远不够。我们定量评估了科罗拉多前锋山脉不同水文事件对水质的影响,发现在三年期间,燃烧区下游的大量水文和地球化学响应主要是由对流风暴驱动的,降雨强度大于30分钟且> 10毫米h?1。这些风暴通常在每年的7月至9月发生几次,通常面积小,寿命短,强度和地理分布变化很大。因此,需要具有高时间分辨率和空间密度的雨量计网络,以及高分辨率的溪流采样,以充分表征野火后的响应。在相对常见(每年超过50%的暴雨)暴雨期间,我们测量的总悬浮沉积物,溶解有机碳(DOC),硝酸盐和锰的浓度是燃烧区域下游比上游上游高10-156倍,并且水质足够削弱了对水处理的关注。短期水质损害主要是由于高强度对流风暴期间地表径流增加所致,造成暴风雪烧毁地区以及沉积物和化学成分向河流输送。燃烧区下游的年沉积物产量受风暴事件和随后的迁移的控制,而DOC的产量与年径流量密切相关,因此更多地取决于春季径流量的年际变化。野火后第三年硝酸盐产量最高。这项研究的结果定量地证明了野火后几年内水质可以改变。由于美国西南部容易发生野火和高强度的暴雨,因此在评估水质脆弱性时,必须考虑暴风雨对野火后水质影响的作用。

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