西北半湿润/半干旱地区土壤无机氮同位素组成及对生态环境、气候条件的响应

氮同位素 土壤 生态系统 气候条件 西北地区
刘卫国 2014-01 项目
The nitrogen cycle in the natural ecosystem is one of the most important processes in the global climate change and biogeochimestry cycles. The nitrogen isotope is becoming one of the primary methods to trace nitrogen cycle and response to climate change. This project intend to systematically study the elemental and bulk nitrogen of the soil under the different ecosystem and climate conditions during the nitrogen cycle in the ecosystem (plant-soil-water), especially to research the soil inorganic nitrogen (nitrate and ammonium) isotope variation. Meanwhile, this project intends to discuss the soil inorganic nitrogen isotope responding to the different ecosystem types and climate conditions. In this way, the soil and plant nitrogen isotope variation mechanism during biogeochemistry cycle processes may be realized, and thoroughly understood the potential relationship between soil and plant nitrogen isotope composition with the environmental humidity (or precipitation) and the temperature variation. The primary study contents in this project are the problems that international researchers do not well understand of nitrogen cycle and nitrogen geochemical in ecosystem. By this project, we will thoroughly understand the nitrogen isotope variation under different ecosystem in the semi-arid area. In addition, this research may be provide more theory mechanisms by using nitrogen isotope to trace nitrogen cycle during biogeochemistry processes.
自然生态系统氮循环过程是全球气候变化和生物地球化学循环的重要内容。利用氮同位素示踪自然生态系统的氮循环及对气候变化的响应正在成为主要的研究方法之一。本申请拟通过对西北地区不同生态系统和气候条件下土壤总氮、无机氮元素和同位素的系统研究,更深入探讨生态系统(植物-土壤-水)氮循环过程的氮同位素组成变化,特别是土壤无机(硝态和氨态氮)氮同位素组成变化;探讨不同生态系统下,土壤无机氮同位素对生态类型和气候环境的响应关系;试图认识氮生物地球化学循环过程植物和土壤氮同位素变化的机制。同时,深入理解植物和土壤氮同位素组成和环境湿度(或降水)、温度变化关系的可能内在因素。本申请所涉及的问题是目前国际上生态系统氮循环和氮同位素地球化学研究一直未能很好开展的重要内容。本课题的进行将会为深入认识半干旱地区不同生态系统氮同位素组成变化,为利用氮同位素示踪氮生物地球化学过程研究提供更多的机制理解。