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干旱地区不同农业和自然生态系统的土壤呼吸。

Soil respiration in different agricultural and natural ecosystems in an arid region.

机构信息

Key Laboratory of Resource Plants, Beijing Botanical Garden, West China Subalpine Botanical Garden, Institute of Botany, Chinese Academy of Sciences, Xiangshan, Beijing, China.

出版信息

PLoS One. 2012;7(10):e48011. doi: 10.1371/journal.pone.0048011. Epub 2012 Oct 17.

Abstract

The variation of different ecosystems on the terrestrial carbon balance is predicted to be large. We investigated a typical arid region with widespread saline/alkaline soils, and evaluated soil respiration of different agricultural and natural ecosystems. Soil respiration for five ecosystems together with soil temperature, soil moisture, soil pH, soil electric conductivity and soil organic carbon content were investigated in the field. Comparing with the natural ecosystems, the mean seasonal soil respiration rates of the agricultural ecosystems were 96%-386% higher and agricultural ecosystems exhibited lower CO(2) absorption by the saline/alkaline soil. Soil temperature and moisture together explained 48%, 86%, 84%, 54% and 54% of the seasonal variations of soil respiration in the five ecosystems, respectively. There was a significant negative relationship between soil respiration and soil electrical conductivity, but a weak correlation between soil respiration and soil pH or soil organic carbon content. Our results showed that soil CO(2) emissions were significantly different among different agricultural and natural ecosystems, although we caution that this was an observational, not manipulative, study. Temperature at the soil surface and electric conductivity were the main driving factors of soil respiration across the five ecosystems. Care should be taken when converting native vegetation into cropland from the point of view of greenhouse gas emissions.

摘要

陆地碳平衡中不同生态系统的变化预计会很大。我们研究了一个具有广泛盐碱性土壤的典型干旱地区,并评估了不同农业和自然生态系统的土壤呼吸。我们在野外调查了五个生态系统的土壤呼吸以及土壤温度、土壤湿度、土壤 pH 值、土壤电导率和土壤有机碳含量。与自然生态系统相比,农业生态系统的平均季节性土壤呼吸速率要高 96%至 386%,而且农业生态系统对盐碱性土壤的 CO2 吸收能力较低。土壤温度和水分分别解释了五个生态系统季节性土壤呼吸变化的 48%、86%、84%、54%和 54%。土壤呼吸与土壤电导率之间存在显著的负相关关系,但与土壤 pH 值或土壤有机碳含量之间的相关性较弱。我们的研究结果表明,尽管我们警告这是一项观察性而非操纵性研究,但不同农业和自然生态系统之间的土壤 CO2 排放存在显著差异。土壤表面温度和电导率是五个生态系统土壤呼吸的主要驱动因素。从温室气体排放的角度来看,应该谨慎将原生植被转化为农田。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/88d9/3474779/d957a9b1e20c/pone.0048011.g001.jpg

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