首 页 网络介绍 CERN新闻 规章制度 在研项目 论文与出版物 学术动态 生态知识 人员招聘 人员组成 English

    论文与出版物
   SCI论文目录
   SCI论文全文(PDF文件)
   核心期刊论文目录
   出版物目录
   研究报告目录

 核心期刊论文目录
Concentrations and exports of solutes from surface runoff in Houzhai Karst Basin,southwest China
------------------------------------------------------------------------------------------
出 版 社:Chemical Geology  
发表时间:2012  
台  站: 鼎湖山森林生态系统定位研究站  
作  者:闫俊华等  
点 击 率:367774
------------------------------------------------------------------------------------------
关 键 字(英文):Karst,Chemical export,Surface runoff,Dissolved inorganic carbon  
摘  要(英文):Chemical concentrations and export rates from surface water were analyzed in Houzhai Karst Basin (HKB, area 80.65km2 in total), southwest China, for the past two decades from 1986 to 2007. Surface water chemistry was dominated by ions of calcium (Ca2+), magnesium (Mg2+), bicarbonate (HCO3−) and sulfate (SO4 2−),which together made up 96% (by weight) of the total dissolved solids measured in this study. Seasonal variability of chemical export rates was positively correlated with surface runoff discharge, with the concentrations generally diluting at high discharge. From 1986 to 2007, as a result of the responses of karst weathering to climatic factors, the concentrations of Ca2+, Mg2+, HCO3−, and SO42− slowly increased in surface water. By contrast, changes in the concentrations of sodium (Na+), potassium (K+), and chloride (Cl−) showed a slowly decreasing pattern. We also found that the annual dissolved inorganic carbon (DIC) flux ranged from 10.1 to 34.1gCm−2 yr−1, with an average value of 24.2gCm−2 yr−1. Rainfall had the most important influence on DIC flux, although water pH may greatly affect the proportions of the three fractions (CO2,HCO3−, CO3 2−) of DIC. High water temperature in the wet season may reduce the solubility of CO2 in water and consequently affect DIC export rate, but this effect is much smaller than that of rainfall. Based on the chemical mass balance in surface water, our results indicate that high concentrations of SO4 2− by the large gypsum (CaSO4·2H2O) dissolution offset some anions such as HCO3− in karst water, which can partly explain why carbon uptake is often overestimated by the empirical model using concentrations of HCO3− in this karst water. It is concluded that the fluvial flux of DIC from karst water is important to the regional or national carbon budgets.  
------------------------------------------------------------------------------------------
闫俊华-2012-Chemical Geology-Concentrations and exports of solutes from surface runoff in Houzhai Karst Basin,southwest China.pdf
相关文章:
屋顶绿化生态系统箱的研制
南亚热带森林植被恢复演替序列的土壤有机碳氮矿化
盆栽荷木、肖蒲桃和黄果厚壳桂幼苗对土壤温室气体排放影响的培育实验研究
鼎湖山主要林下层植物光合生理特性对模拟氮沉降的响应
鼎湖山五种植被类型群落生物量及其径级分配特征
1981-2000年广东省净初级生产力的时空格局.
几种植物在生长过程中对人工湿地污水处理效果的影响
Sewage treatment with constructed wetlnd of multiplayer plants configuration in south china
广州城郊环境梯度下马尾松针叶元素质量分数变化特征.
Heavy metal levels in barks of Pinus massonian.
相关文章分页:  共 201 页 2006 条记录 9 3[161][162][163][164][165][166][167][168][169][170]4 :

[关闭窗口]
中国生态系统研究网络 版权所有
| 网络介绍 | 联系方式 | 网站地图 |