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Hydrologic controls on seasonal and inter-annual variability of Congo River particulate organic matter source and reservoir age

机译:刚果河微粒有机质源和水库年龄季节性和年度季节性变异性的水文控制

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We present dissolved organic carbon (DOC) concentrations, particulate organic matter (POM) composition (delta C-13, delta N-15, Delta C-14, N/C), and particulate glycerol dialkyl glycerol tetraether (GDGT) distributions from a 34-month time-series near the mouth of the Congo River. An end-member mixing model using delta C-13 and N/C indicates that exported POM is consistently dominated by C-3 rainforest soil sources, with increasing contribution from C-3 vegetation and decreasing contribution from phytoplankton at high discharge. Large C-4 inputs are never observed despite covering approximate to 13% of the catchment. Low and variable Delta C-14 values during 2011 [annual mean= (-148 +/- 82) parts per thousand], when discharge from left-bank tributaries located in the southern hemisphere reached record lows, likely reflect a bias toward pre-aged POM derived from the Cuvette Congolaise swamp forest. In contrast, Delta C-14 values were stable near -50% between January and June 2013, when left-bank discharge was highest. We suggest that headwater POM is replaced and/or diluted by C-3 vegetation and pre-aged soils during transit through the Cuvette Congolaise, whereas left-bank tributaries export significantly less pre-aged material. GDGT distributions provide further evidence for seasonal and inter-annual variability in soil provenance. The cyclization of branched tetraethers and the GDGT-0 to crenarchaeol ratio are positively correlated with discharge (r >= 0.70; p-value <= 4.3 x10(-5)) due to the incorporation of swamp-forest soils when discharge from right-bank tributaries located in the northern hemisphere is high. Both metrics reach record lows during 2013, supporting our interpretation of increased left-bank contribution at this time. We conclude that hydrologic variability is a major control of POM provenance in the Congo River Basin and that tropical wetlands can be a significant POM source despite their small geographic coverage.
机译:我们呈现溶解的有机碳(DOC)浓度,颗粒状有机物(POM)组合物(Delta C-13,Delta N-15,Delta C-14,N / C),以及来自a的颗粒甘油二烷基甘油四醚(GDGT)分布在刚果河口附近34个月的时间系列。使用Delta C-13和N / C的端构件混合模型表明出口的POM始终由C-3雨林土壤来源占主导地位,随着C-3植被的贡献越来越高,从高放电下降了浮游植物的贡献。尽管覆盖了大致收集机的13%,但绝不会观察到大的C-4输入。 2011年期间的低和可变ΔC-14值[年平均值=(-148 +/- 82)零件],当从位于南半球的左岸支流达到历史小时的左岸支流中,可能反映了预先偏向老年POM源自比色皿刚果沼泽森林。相比之下,当左岸放电最高时,Delta C-14值在2013年1月至6月至2013年6月至6月之间稳定。我们建议在通过比色杯刚凝固期间被C-3植被和预先老化的土壤替换和/或稀释,而左岸支流出口显着较少的预先预测材料。 GDGT分布为土壤来源的季节性和年间变异性提供了进一步的证据。支化四醚的环化和GDGT-0至颅淀尾酚比与放电(R> = 0.70; p值<= 4.3×10(-5))呈正相关 - 由于右键排出时沼泽林土 - 位于北半球的银行支流很高。两项指标在2013年达到录制低点,支持我们此时对左岸贡献增加的解释。我们得出结论,水文变异性是刚果河流域POM源的主要控制,并且尽管他们小的地理覆盖率,但热带湿地可以成为一个重要的POM源。

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