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模拟降水对荒漠草原生态系统碳交换的影响
引用本文:崔媛媛,白柳,王梓晗,赵宏宇,宝音贺西格,李治国,韩国栋,王忠武.模拟降水对荒漠草原生态系统碳交换的影响[J].草业科学,2022,39(1):3-9.
作者姓名:崔媛媛  白柳  王梓晗  赵宏宇  宝音贺西格  李治国  韩国栋  王忠武
作者单位:内蒙古农业大学草原与资源环境学院, 内蒙古 呼和浩特 010011;内蒙古自治区农牧业科学院, 内蒙古 呼和浩特 010031
基金项目:国家重点研发计划项目(2016YFC0500504)%内蒙古自治区重大科技专项(ZDZX2018020)%国家自然科学基金(31560140%31760143)%内蒙古自治区科技成果转化项目(2019CG069%2020CG0013)
摘    要:全球降水格局的改变势必会影响陆地生态系统的各项功能,而草地碳汇功能对水分的变化极为敏感.为探究不同降水梯度对生态系统碳交换产生的影响,于内蒙古四子王旗荒漠草原设置模拟降水试验(减水50%、自然降水、增水50%和增水100%),在2017年5月至9月,每隔15?d采用Li-6400便携式光合仪和密闭式箱法测定生态系统净碳...

关 键 词:降水梯度  土壤含水量  土壤温度  地上生物量  生态系统净碳交换  生态系统呼吸通量  总生态系统生产力

Effect of simulated precipitation on the ecosystem carbon exchange in a desert steppe
CUI Yuanyuan,BAI Liu,WANG Zihan,ZHAO Hongyu,Baoyinhexige,LI Zhiguo,HAN Guodong,WANG Zhongwu.Effect of simulated precipitation on the ecosystem carbon exchange in a desert steppe[J].Pratacultural Science,2022,39(1):3-9.
Authors:CUI Yuanyuan  BAI Liu  WANG Zihan  ZHAO Hongyu  Baoyinhexige  LI Zhiguo  HAN Guodong  WANG Zhongwu
Institution:(College of Grassland Resources and Environmental Science,Inner Mongolia Agricultural University,Huhhot 010011,Inner Mongolia,China;Inner Mongolia Academy of Agricultural and Animal Husbandry Science,Huhhot 010031,Inner Mongolia,China)
Abstract:Changes in global precipitation patterns are bound to affect the functions of terrestrial ecosystems. The carbon sink function of grasslands is very sensitive to changes in the soil water content. To study the effects of precipitation on ecosystem carbon exchange in a desert steppe ecosystem, four different precipitation gradients were set up in a desert grassland using a random group design (50% reduced precipitation, natural precipitation, and 50% and 100% increased precipitation), and each precipitation gradient had three replicates. The net ecosystem carbon exchange (NEE), ecosystem respiration (ER), and gross ecosystem productivity (GEP), were measured during the growing season of 2017 using the portable optical LI-6400 and the static chamber method. The results showed that: 1) Soil moisture content and above-ground biomass significantly increased, and soil temperature significantly decreased, in treatments with increasing water availability (P < 0.05). 2) Under 50% water reduction, NEE was the carbon source; whereas under natural precipitation, and 50% and 100% increased precipitation, NEE was a carbon sink (P < 0.05). Furthermore, with an increase in precipitation, ER and GEP increased significantly (P < 0.05). The determination coefficient of GEP and soil water content was greater than that of ER and soil water content. 3) The correlation coefficient between NEE and soil temperature was the largest, so was the correlation coefficient between ER, GEP, and above-ground biomass. The results indicate that water can promote ecosystem carbon exchange in a desert steppe by increasing the above-ground biomass and reducing the soil temperature.
Keywords:precipitation gradient  soil moisture content  soil temperature  above-ground biomass  net ecosystem carbon exchange  ecosystem respiration  gross ecosystem productivity
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