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Effects of precipitation, air temperature, and land use on organic carbon discharges from rhode river watersheds

机译:降水、气温和土地利用对罗德河流域有机碳排放的影响

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We studied discharges of organic carbon from eight contiguous small watersheds on the Atlantic Coastal Plain in Maryland for up to 24 yr. Six of these watersheds were second or third order with mixed-land-use, while two were first order (one completely forested and one highly dominated by cropland). These watersheds have perched aquifers, so all groundwater discharges as well as surface runoff were measured at V-notch weirs and flumes, which included volume-integrating flow-proportional samplers. Interannual variations in annual and seasonal precipitation during this study spanned approximately the range of 160 yr weather records in the region. Annual total organic carbon (TOC) area yields from the overall Rhode River watershed varied 8-fold, correlations with precipitation were highly significant, and a power function regression explained 54 of the variance in annual TOC fluxes. TOC fluxes were higher from upland forest than mixed land use, and highest from the cropland-dominated watershed. The fluxes from first order watersheds were more variable with precipitation. In the spring, TOC fluxes were highest and most correlated with precipitation, compared to other seasons. Precipitation volume also explained much of the variance in annual and spring TOC concentrations from upland forest and cropland, with concentrations three to five times higher in very wet years than in very dry years. Variation in winter and summer air temperature was correlated with TOC concentrations from forested watersheds, and linear regressions explained 19 to 42 of the variance in TOC. A regression model was used to construct graphical and tabular summaries. Particulate organic carbon and dissolved organic carbon (DOC) concentrations and the ratio of DOC to TOC were highly correlated with water discharge for a second order, mixed land use watershed, and power function regressions explained 21 to 43 of the variance. For the first order, single-land-use watersheds the ratio of DOC to TOC was also highly correlated with discharge. References: 56
机译:我们研究了马里兰州大西洋沿岸平原上八个连续的小流域的有机碳排放长达 24 年。其中6个流域为二阶或三阶混合土地利用,2个为一级流域(1个完全森林覆盖,1个以耕地为主)。这些流域有栖息的含水层,因此所有地下水排放和地表径流都是在V型缺口堰和水槽处测量的,其中包括体积积分流量比例采样器。在这项研究中,年降水量和季节性降水量的年际变化大约跨越了该地区160年天气记录的范围。整个罗德河流域的年总有机碳(TOC)产量变化了8倍,与降水的相关性非常显著,幂函数回归解释了年TOC通量方差的54%。高地林的TOC通量高于混合土地利用,以耕地为主的流域的TOC通量最高。一级流域的通量随降水的变化而变化更大。与其他季节相比,春季TOC通量最高,与降水的相关性最大。降水量也解释了高地森林和农田的年度和春季TOC浓度的差异,非常潮湿年份的浓度比非常干旱年份高三到五倍。冬季和夏季气温的变化与森林流域的TOC浓度相关,线性回归解释了TOC方差的19%至42%。回归模型用于构建图形和表格摘要。颗粒有机碳和溶解有机碳(DOC)浓度以及DOC与TOC的比值与二阶水排放高度相关,混合土地利用流域和幂函数回归解释了21%-43%的方差。对于一阶,单一土地利用流域,DOC与TOC的比值也与流量高度相关。[参考文献: 56]

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