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不同耕作方式下土壤水分状况对土壤呼吸的初期影响
引用本文:张延,梁爱珍,张晓平,陈升龙,孙冰洁,刘四义. 不同耕作方式下土壤水分状况对土壤呼吸的初期影响[J]. 环境科学, 2016, 37(3): 1106-1113
作者姓名:张延  梁爱珍  张晓平  陈升龙  孙冰洁  刘四义
作者单位:中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院大学, 北京 100049;中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院大学, 北京 100049;中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院大学, 北京 100049;中国科学院东北地理与农业生态研究所, 长春 130102;中国科学院大学, 北京 100049
基金项目:国家自然科学基金项目(31170483);中国科学院重点部署项目(KZZD-EW-TZ-16-02);中国科学院东北地理与农业生态研究所"优秀青年人才"基金项目(DLSYQ12003);中国科学院青年创新促进会项目(2015183)
摘    要:以2001年在东北典型黑土上进行的保护性耕作长期定位试验下免耕、垄作及常规耕作土壤进行了室内培养实验,按照田间持水量(water-holding capacity,WHC)的30%、60%、90%、120%、150%、180%、210%、240%、270%设定了9个水分梯度,并分别对其二氧化碳(CO_2)排放量进行了22 d的短期观测,以研究不同耕作方式下土壤水分状况对土壤呼吸的初期影响.结果表明:1干土条件下在加水培养初期,3种耕作方式均产生了明显的激发效应,并且土壤呼吸速率与土壤含水量间存在正相关关系.2除干旱(30%WHC)及淹水(240%WHC、270%WHC)条件下,3种耕作方式CO_2排放通量分别为免耕垄作常规耕作.3对不同耕作方式下土壤水分状况及CO_2排放通量进行了方程拟合,在30%~270%WHC条件下,免耕的CO_2排放通量与水分状况拟合为二次回归方程,而垄作与常规耕作则是线性回归方程.在30%~210%WHC条件下,免耕与垄作下土壤CO_2排放通量与水分状况均可拟合为较好的对数方程,可决系数R~2分别为0.966、0.956.

关 键 词:耕作方式  土壤水分  土壤呼吸  CO2排放通量  拟合方程
收稿时间:2015-06-25
修稿时间:2015-11-04

Priming Effects of Soil Moisture on Soil Respiration Under Different Tillage Practices
ZHANG Yan,LIANG Ai-zhen,ZHANG Xiao-ping,CHEN Sheng-long,SUN Bing-jie and LIU Si-yi. Priming Effects of Soil Moisture on Soil Respiration Under Different Tillage Practices[J]. Chinese Journal of Environmental Science, 2016, 37(3): 1106-1113
Authors:ZHANG Yan  LIANG Ai-zhen  ZHANG Xiao-ping  CHEN Sheng-long  SUN Bing-jie  LIU Si-yi
Affiliation:Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;University of Chinese Academy of Sciences, Beijing 100049, China;Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;University of Chinese Academy of Sciences, Beijing 100049, China;Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;University of Chinese Academy of Sciences, Beijing 100049, China;Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:In the early stage of an incubation experiment, soil respiration has a sensitive response to different levels of soil moisture. To investigate the effects of soil moisture on soil respiration under different tillage practices, we designed an incubation trial using air-dried soil samples collected from tillage experiment station established on black soils in 2001. The tillage experiment consisted of no-tillage (NT), ridge tillage (RT), and conventional tillage (CT). According to field capacity (water-holding capacity, WHC), we set nine moisture levels including 30%, 60%, 90%, 120%, 150%, 180%, 210%, 240%, 270%WHC. During the 22-day short-term incubation, soil CO2 emission was measured. In the early stage of incubation, the priming effects occurred under all tillage practices. There were positive correlations between soil respiration and soil moisture. In addition to drought and flood conditions, soil CO2 fluxes followed the order of NT > RT > CT. We fitted the relationship between soil moisture and soil CO2 fluxes under different tillage practices. In the range of 30%-270% WHC, soil CO2 fluxes and soil moisture fitted a quadratic regression equation under NT, and linear regression equations under RT and CT. Under the conditions of 30%-210% WHC of both NT and RT, soil CO2 fluxes and soil moisture were well fitted by the logarithmic equation with fitting coefficient R2=0.966 and 0.956, respectively.
Keywords:tillage practices  soil moisture  soil respiration  carbon dioxide fluxes  fitting equation
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