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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Sources and transport of carbon and nitrogen in the River Sava watershed, a major tributary of the River Danube
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Sources and transport of carbon and nitrogen in the River Sava watershed, a major tributary of the River Danube

机译:萨瓦河流域(多瑙河的主要支流)的碳和氮的来源和运输

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Carbon and nitrogen dynamics were examined throughout the River Sava watershed, a major tributary of the River Danube, in 2005 and 2006. The River Sava exported 2.1 x 10(11) mol C/yr as dissolved inorganic carbon (DIC), and emitted 2.5 x 10(10) mol C/yr as CO2 to the atmosphere. Stable carbon isotope ratios indicate that up to 42% of DIC originated from carbonate weathering and similar to 23% from degradation of organic matter. Loads of dissolved and particulate organic carbon increased with discharge and export rates were calculated to be 2.1 x 10(10) mol C/yr and up to 4.1 x 10(9) mol C/yr, respectively. Isotopic compositions (delta C-13 and delta N-15) and C/N ratios indicated that soil organic matter was the dominant source of particulate organic matter for 59% of the samples. Eighteen percent of the samples were dominated by plankton, 12% by periodic inputs of fresh terrestrial plant detritus with C/N >15, and about 11% of the samples were dominated by the contribution of aquatic vascular plants. Nitrate inputs were controlled by land use in the River Sava watershed. delta N-15(NO3) values <6 parts per thousand were found in predominantly forested watersheds, while values >6 parts per thousand typically represented watersheds with a higher percentage of agricultural and/or urban land use. Elevated delta N-15(NO3) values (up to +25.5 parts per thousand) at some sites were probably due to the combined effects of low-flow and inputs from sewage and/or animal waste. (c) 2008 Elsevier Ltd. All rights reserved.
机译:在2005年和2006年,在整个多瑙河的主要支流萨瓦河分水岭上研究了碳和氮的动态。萨瓦河以溶解无机碳(DIC)的形式每年输出2.1 x 10(11)mol C / yr,排放了2.5 x 10(10)mol C / yr,以二氧化碳计。稳定的碳同位素比表明,高达42%的DIC来自碳酸盐风化作用,而23%来自有机物的降解。溶解和颗粒有机碳的负荷随排放和出口速度的增加而增加,分别为2.1 x 10(10)mol C / yr和高达4.1 x 10(9)mol C / yr。同位素组成(δC-13和δN-15)和C / N比表明,土壤有机质是59%样品中颗粒有机质的主要来源。 18%的样品以浮游生物为主,C / N> 15的新鲜陆生植物碎屑的定期输入占12%,水生维管植物的贡献占大约11%。硝酸盐投入量由萨瓦河流域的土地利用控制。在主要森林流域中发现Delta N-15(NO3)值<千分之六,而值>千分之六通常代表具有较高农业和/或城市土地利用百分比的流域。在某些地点,δN-15(NO3)值升高(高达+25.5千分之一),可能是由于低流量和污水和/或动物粪便的投入造成的综合影响。 (c)2008 Elsevier Ltd.保留所有权利。

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