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川西北高寒草甸不同放牧模式对土壤呼吸的影响
引用本文:阳小成,阿舍小虎,苗原,刘银占. 川西北高寒草甸不同放牧模式对土壤呼吸的影响[J]. 生态学报, 2016, 36(17): 5371-5378
作者姓名:阳小成  阿舍小虎  苗原  刘银占
作者单位:成都理工大学材料与化学化工学院, 成都 610059,成都理工大学材料与化学化工学院, 成都 610059;中国科学院成都生物研究所生态恢复重点实验室, 成都 610041,河南大学生命科学学院植物逆境实验室, 开封 475004,中国科学院成都生物研究所生态恢复重点实验室, 成都 610041;河南大学生命科学学院植物逆境实验室, 开封 475004
基金项目:国家自然科学基金项目(31000232,31200375);国家博士后科学基金项目(2012M520066,2013T60699);河南大学优秀青年培育基金(0000A40385)
摘    要:采用土壤二氧化碳(CO_2)通量自动测量系统,对不同放牧模式(全年禁牧、夏季放牧、冬季放牧和自由放牧)下川西北高寒草甸的土壤呼吸进行监测,比较了不同放牧模式下土壤呼吸的季节动态和温度敏感性。研究发现:1)放牧模式可以改变高寒草甸土壤呼吸的季节动态变化。禁牧、夏季放牧以及自由放牧样地的土壤呼吸在季节上的变化趋势基本相似,而冬季放牧样地的土壤呼吸最大值与前者相比明显向后推迟;2)放牧模式并不改变高寒草甸年平均土壤呼吸速率,但对不同季节土壤呼吸速率的影响不同;3)不同放牧模式可以改变土壤呼吸对温度的敏感性(Q_(10))。不同放牧模式下土壤呼吸Q_(10)值大小依次为:禁牧1a(8.13)冬季放牧(7.49)禁牧3a(5.46)夏季放牧(5.20)自由放牧(4.53)。该地区土壤呼吸的Q_(10)值均明显高于热带和其它温带草地土壤呼吸的Q_(10)值。结果表明,放牧模式是影响高寒草甸土壤碳排放的一个重要因素。此外,在未来全球气候变暖背景下,在生长季节无放牧干扰的高寒草甸可能比放牧干扰的高寒草甸释放出更多的CO_2到大气中。

关 键 词:草地生态系统  放牧  青藏高原  Q10  土壤碳通量
收稿时间:2015-02-12
修稿时间:2016-06-13

Response of soil respiration rate to grazing patterns in an alpine meadow, Northwestern Sichuan, China
YANG Xiaocheng,ASHE Xiaohu,MIAO Yuan and LIU Yinzhan. Response of soil respiration rate to grazing patterns in an alpine meadow, Northwestern Sichuan, China[J]. Acta Ecologica Sinica, 2016, 36(17): 5371-5378
Authors:YANG Xiaocheng  ASHE Xiaohu  MIAO Yuan  LIU Yinzhan
Affiliation:College of Material and Chemistry & Chemical Engineering, Chengdu University of Technology, Chengdu 610059, China,College of Material and Chemistry & Chemical Engineering, Chengdu University of Technology, Chengdu 610059, China;ECORES Lab, Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China,Key Laboratory of Plant Stress Biology, College of Life Sciences, Henan University, Kaifeng 475004, China and ECORES Lab, Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610041, China;Key Laboratory of Plant Stress Biology, College of Life Sciences, Henan University, Kaifeng 475004, China
Abstract:In this study, an automated soil CO2 flux system was used to measure soil respiration rates from 2008 to 2009 in an alpine meadow subjected to different grazing patterns (no grazing, grazing in summer, grazing in winter, and free grazing). We compared the seasonal dynamics and temperature sensitivity of soil respiration under the different grazing patterns, and found that 1) the seasonal dynamics of soil respiration were affected by grazing patterns. Soil respiration peaked later in the year in meadows subjected to winter grazing than in those in the no grazing, grazing in summer, and free grazing treatments; 2) the grazing pattern used affected seasonal variations in the rate of soil respiration, but not that of the mean annual rate of soil respiration; and 3) the sensitivity of soil respiration to soil temperature (Q10) at a depth of 5 cm was affected by variations in grazing pattern. The Q10 value was the highest under the no grazing for one year treatment, followed by, in descending order, the winter grazing, no grazing for three years, grazing in summer, and free grazing treatments. The Q10 value of the alpine meadow was higher than that of the tropical and other temperate grasslands. These results suggest that grazing pattern plays an important role in carbon release from soils in alpine meadows. Additionally, in the future, global warming may cause more carbon to be released from non-grazed meadows than from those under grazing pressure during the growing season.
Keywords:grassland ecosystem  grazing  Qinghai-Tibetan plateau  Q10 value  soil carbon flux
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