Characteristics of CO_2 in unsaturated zone(～90 m) of loess tableland, Northwest China  

作　　者：Chao Song Guilin Han Yingchun Shi Congqiang Liu Pan Wang 

机构地区：[1]School of Water Resources and Environment, China University of Geosciences (Beijing) [2]The Institute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences

出　　处：《Acta Geochimica》2017年第3期489-493,共5页地球化学学报（英文）

基　　金：supported jointly by National Natural Science Foundation of China(41403107,41325010);the Basic Science Research Fund from the Institute of Hydrogeology and Environmental Geology(SK201208);and the China Geological Survey Projects(12120113005900)

摘　　要：In order to observe CO_2 characteristics in the unsaturated zone of loess tableland and further understand the carbon cycle,a series of tubes for gas monitoring and sampling were installed in an approximately 90-m deep Qiushe loess section of Lingtai County,Northwestern China.The results show that the concentration of CO_2 was higher in loess than in the atmosphere,reaching a maximum of 6970 lmol·mol^(-1).CO_2 concentrations in loess were higher in summer than in winter.The CO_2 in loess was related to organic carbon decomposed by microbes,and to the CaCO_3–H_2O–CO_2 system in the interface between the saturated and unsaturated zones.In order to observe CO2 characteristics in the unsaturated zone of loess tableland and further understand the carbon cycle,a series of tubes for gas monitoring and sampling were installed in an approximately 90-m deep Qiushe loess section of Lingtai County,Northwestern China.The results show that the concentration of CO2 was higher in loess than in the atmosphere,reaching a maximum of 6970 lmol·mol^-1.CO2 concentrations in loess were higher in summer than in winter.The CO2 in loess was related to organic carbon decomposed by microbes,and to the CaCO3–H2O–CO2 system in the interface between the saturated and unsaturated zones.

关 键 词：Unsaturated zone Soil CO2 Carbon stock in deep loess Quantitative paleoclimate reconstruction LOESS 

分 类 号：P593[天文地球—地球化学]