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淋溶过程对亚高山针叶林土壤碳、氮海拔分布特征的影响 被引量:1

Effects of leaching process on characteristics of altitudinal distribution of soil carbon and nitrogen in subalpine coniferous forest
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摘要 为揭示淋溶过程在山地养分循环中的重要作用,研究了贡嘎山东坡海拔2600~3200 m针叶林土壤碳(C)、氮(N)的海拔分布特征,分析了不同海拔4个样点的针叶林土壤C、N含量及碳氮比(C/N),并结合其他土壤物理、化学和生物指标探讨了淋溶过程对土壤C、N海拔分布特征的影响。结果显示:分解强烈的凋落物层(O H层)的C、N含量和碳氮比(C/N)随海拔升高有降低趋势。由于凋落物碳(C lit)含量分别与O H层C、N含量显著正相关(P<0.05),因此,O H层C、N海拔分布特征主要由C lit输入量控制。与O H层相比,矿质土层(A、B和C层)中C、N含量及C/N并未发现明显的梯度变化趋势。A层C、N含量在2781 m样点较低,而B和C层C、N含量均在2781 m样点最高。天然降雨中C、N含量明显低于壤中流中C、N含量,展现了淋溶作用对C、N空间分布的影响。上述结果表明,淋溶过程对西南亚高山针叶林土壤C、N空间分布格局具有不可忽略的影响。 In order to reveal the importance of leaching on mountainous nutrients cycling,the characteristics of altitude distribution of soil C and N in the coniferous forest at an altitude of 2600-3200 m on the eastern slope of the Gongga mountain were studied.The soil C,N content and C/N of the conifers at 4 sampling points at different altitudes were analyzed.Combined with other soil physical,chemical and biological indicators,the effects of the leaching process on the characteristics of altitudinal distribution of soil C and N were explored.The results showed that the spatial distributions of C,N contents and C/N in the humified litter horizon(O H horizon)exhibited a similar decreasing trend with the increase of altitude.Since the content of C in litters(C lit)was positively correlated with soil C and N in the O H horizon(P<0.05),the production of C lit was the main factor affecting the altitudinal distributions of soil C and N in the O H horizon.The obvious altitudinal trend was not observed for soil C,N contents and C/N in the mineral horizons(A,B and C horizon).The contents of soil C and N in the A horizon were lower than those in the 2781 m site,while the maximums were for the B and C horizon in this site.The contents of soil C and N in the rainfall were significantly lower than those in the interflow,which showed the effects of leaching on the spatial distributions of soil C and N.It is indicated that the effects of leaching process on the spatial distributions of soil C and N in subalpine coniferous forest in Southwest Asia can not be ignored.
作者 何晓丽 吴艳宏 周俊 马婷婷 HE Xiaoli;WU Yanhong;ZHOU Jun;MA Tingting(College of Resource,Environment and Tourism,Hubei University of Arts and Science,Xiangyang 441053,China;Chengdu Institute of Mountain Hazards and Environment,Chinese Academy of Sciences/Ministry of Water Resources,Chengdu 610041,China)
出处 《华中农业大学学报》 CAS CSCD 北大核心 2021年第1期187-194,共8页 Journal of Huazhong Agricultural University
基金 国家自然科学基金项目(41630751,41877011) 湖北省高等学校优秀中青年科技创新团队计划项目(T2020016) 湖北文理学院学科开放基金项目(XK2020063)。
关键词 碳、氮海拔分布特征 淋溶过程 针叶林土壤 亚高山 山地养分循环 C、N生物地球化学循环 C,N altitudinal distributions leaching coniferous forest soils subalpine mountain nutrient cycling C,N biogeochemical cycles
作者简介 何晓丽,E-mail:xlhe@hbuas.edu.cn;通信作者:吴艳宏,E-mail:yhwu@imde.ac.cn。
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