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The Effects of Land Use and Human Activities on Carbon Cycling in Texas Rivers.

机译:土地利用和人类活动对德克萨斯河碳循环的影响。

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摘要

I investigated how land use and human activities affect the sources and cycling of carbon (C) in subtropical rivers. Annually rivers receive a large amount of terrestrial C, process a portion of this C and return it to the atmosphere as CO2. The rest is transported to the ocean. Land use and human activities can affect the sources and fate of terrestrial C in rivers. However, studies on these effects are limited, especially in the humid subtropics.;I combined measurements of the partial pressure of dissolved CO 2 (pCO2), C isotopes (13C and 14C) and solid-state 13C nuclear magnetic resonance (NMR) to study C cycling in three subtropical rivers in Texas, two small rivers (Buffalo Bayou and Spring Creek) and a midsized river (the Brazos).;My pCO2 data show that small humid subtropical rivers are likely a large source of atmospheric CO2 in the global C cycle. My measurements on pCO2, C isotopic and chemical composition of dissolved inorganic C (DIC) and particulate organic C (POC) revealed four types of effects of land use and human activities on river C cycling. First, oyster shells and crushed carbonate minerals used in road construction are being dissolved and slowly drained into Buffalo Bayou and the lower Brazos and may be a source of river CO2 released to the atmosphere. Second, river damming and nutrient input from urban treated wastewater stimulate algal growth and reduce CO2 evasion of the middle Brazos. Third, urban treated wastewater discharge is adding old POC to the middle Brazos and decomposition of the old POC adds to the old riverine DIC pool. Fourth, agricultural activities coupled with high precipitation enhance loss of old organic C (OC) from deep soils to the lower Brazos, and decomposition of the old soil OC contributes to the old CO2 evaded.;I document for the first time the river C cycling effects of the use of carbonate minerals in construction and the riverine discharge of urban wastewater. Results presented here indicate the need to study disturbed river systems to better constrain the global C budget.
机译:我调查了土地利用和人类活动如何影响亚热带河流中碳(C)的来源和循环。每年,河流收到大量的陆地碳,处理掉一部分碳,然后以二氧化碳的形式返回大气。其余的被运到海洋。土地利用和人类活动会影响河流中陆地碳的来源和命运。但是,关于这些效应的研究非常有限,尤其是在亚热带湿润地区。我结合测量了溶解的CO 2(pCO2),C同位素(13C和14C)和固态13C核磁共振(NMR)的分压,研究了得克萨斯州的三条亚热带河流,两条小河流(布法罗河口和春溪)和一条中型河流(布拉索斯)的碳循环。我的pCO2数据显示,潮湿的亚热带小河流可能是全球大气CO2的主要来源C循环。我对pCO2,C同位素和溶解性无机C(DIC)和颗粒有机C(POC)的化学成分的测量揭示了土地利用和人类活动对河流C循环的四种影响。首先,用于道路建设的牡蛎壳和压碎的碳酸盐矿物被溶解并缓慢排入布法罗河口和下布拉索斯州,并且可能是释放到大气中的二氧化碳的来源。其次,河流水坝建设和城市处理废水中的养分输入刺激了藻类的生长并减少了中布拉索斯的CO2逃逸。第三,城市处理后的废水排放正在中间的Brazos中添加了旧的POC,而旧的POC的分解又增加了旧的河流DIC库。第四,农业活动与高降水量一起增加了从深层土壤到较低的Brazos的旧有机碳(OC)的损失,旧土壤OC的分解导致旧的CO2逃逸。碳酸盐矿物在建筑中的作用以及城市废水的河边排放。这里给出的结果表明需要研究受干扰的河流系统,以更好地限制全球碳预算。

著录项

  • 作者

    Zeng, Fan-Wei.;

  • 作者单位

    Rice University.;

  • 授予单位 Rice University.;
  • 学科 Biogeochemistry.;Environmental Sciences.;Geochemistry.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 140 p.
  • 总页数 140
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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