首页> 外文期刊>Geophysical Research Letters >Paleoreconstruction of organic carbon inputs to an oxbow lake in the Mississippi River watershed: Effects of dam construction and land use change on regional inputs
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Paleoreconstruction of organic carbon inputs to an oxbow lake in the Mississippi River watershed: Effects of dam construction and land use change on regional inputs

机译:密西西比河流域的牛弓湖的有机碳输入的古建筑:大坝建设和土地利用变化对区域输入的影响

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摘要

We use a dated sediment core from Lake Whittington (USA) in the lower Mississippi River to reconstruct linkages in the carbon cycling and fluvial sediment dynamics over the past 80years. Organic carbon (OC) sources were characterized using bulk (C-13, ramped pyrolysis-oxidation (PyrOx) C-14, N-15, and TN:OC ratios) and compound-specific (lignin phenols and fatty acids, including C-13 and C-14 of the fatty acids) analyses. Damming of the Missouri River in the 1950s, other hydrological modifications to the river, and soil conservation measures resulted in reduced net OC export, in spite of increasing OC concentrations. Decreasing C-13 values coincided with increases in N-15, TN:OC ratios, long-chain fatty acids, and lignin-phenol concentrations, suggesting increased inputs of soil-derived OC dominated by C-3 vegetation, mainly resulting from changes in farming practices and crop distribution. However, ramped PyrOx C-14 showed no discernible differences downcore in thermochemical stability, indicating a limited impact on soil OC turnover.
机译:我们使用来自美国密西西比河下游惠廷顿湖(Lake Whittington)的过时沉积物核来重建过去80年碳循环和河流沉积物动力学之间的联系。有机碳(OC)的来源使用本体(C-13,倾斜的热解-氧化(PyrOx)C-14,N-15和TN:OC比率)和特定于化合物的化合物(木质素酚和脂肪酸,包括C-脂肪酸的13和C-14分析。尽管OC浓度增加,但1950年代密苏里河的筑坝,对该河的其他水文改造以及土壤保护措施导致OC净出口减少。 C-13值降低与N-15,TN:OC比,长链脂肪酸和木质素-酚浓度的升高同时发生,这表明由C-3植被主导的源自土壤的OC的输入增加,这主要是由于C-3植被的变化所致。耕作方式和农作物分配。但是,倾斜的PyrOx C-14在热化学稳定性上没有明显的差异,表明对土壤OC转化的影响有限。

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