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首页> 外文期刊>Journal of Coastal Research: An International Forum for the Littoral Sciences >Examining the Distribution and Variation of Dissolved Carbon Species and Seasonal Carbon Exports within the Jiulongjiang River Basin (Southeast China)
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Examining the Distribution and Variation of Dissolved Carbon Species and Seasonal Carbon Exports within the Jiulongjiang River Basin (Southeast China)

机译:检查九龙江流域溶解碳物种和季节性碳出口的分布及变异(东南中国)

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The water chemistry, including major ions and dissolved carbon of Jiulongjiang River in SE China, were determined to examine the distributions and variations of dissolved carbon species. Dissolved inorganic carbon (DIC) concentrations in the river water were within the range of 7.50 to 49.04 mg/L (averaged 22.12 mg/L) in the wet season and from 8.83 to 84.91 mg/L (averaged 41.17 mg/L) in the dry season. Dissolved organic carbon (DOC) varied from 0.54 to 2.89 mg/L (averaged 1.04 mg/L) in the wet season and from 1.34 to 3.56 mg/L (averaged 2.34 mg/L) in the dry season. The concentrations of DIC were comparable among the three tributaries, whereas the DOC was significantly higher in the Xixi River and Nanxi River than the Beixi River. The calculations employing the mass balance method indicated that weathering process and anthropogenic inputs played an important role in the dissolved carbon production in the Jiulongjiang watershed. The DOC exhibited significant correlations with the rural area whereas the DIC did not show any significant correlations with land-use types, indicating that the DOC was closely related to agricultural activities. The carbon export fluxes from the Jiulongjiang River were calculated based on the discharge data. The DIC-C export reached to 1.2 x 10(5)t/y, whereas the DOC-C export was nearly 3.2 x 10(4)t/y. In addition, seasonal variation of carbon exports had been observed; because of the large water discharge in the wet season, more DIC and DOC were transported from the Jiulongjiang River in the wet season than in the dry season. The source analysis demonstrated natural processes account for the majority of carbon exports.
机译:确定水化学,包括九龙江在中国的主要离子和溶解碳,确定溶解碳物种的分布和变化。河水中溶解的无机碳(DIC)浓度在湿季节的7.50至49.04mg / L(平均为22.12mg / L)的范围内,并且在8.83至84.91 mg / L(平均为41.17 mg / L)。旱季。溶解的有机碳(DOC)在湿季等0.54至2.89mg / L(平均1.04mg / L),干燥季节的1.34至3.56mg / L(平均为2.34 mg / L)。 DIC的浓度在三个支流中是相当的,而DOC在西溪河和南溪河比贝西河河上显着高。采用质量平衡法的计算表明,风化过程和人为投入在九龙江流域的溶解碳生产中发挥着重要作用。该文件与农村地区表现出显着的相关性,而DIC没有显示与土地使用类型的任何显着相关性,表明DOC与农业活动密切相关。九龙江的碳出口通量基于放电数据计算。 DIC-C导出达到1.2 x 10(5)T / Y,而DOC-C导出近3.2×10(4)T / Y。此外,已观察到碳出口的季节性变化;由于潮湿季节的水放电大,潮湿季节的水流量和医生在潮湿的季节的运输比旱季。源分析证明了对大多数碳出口的自然过程。

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