首页> 外文期刊>Soil Biology & Biochemistry >Impact of land degradation on soil respiration in a steppe (Stipa tenacissima L.) semi-arid ecosystem in the SE of Spain
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Impact of land degradation on soil respiration in a steppe (Stipa tenacissima L.) semi-arid ecosystem in the SE of Spain

机译:西班牙东南部草原(Stipa tenacissima L.)半干旱生态系统中土地退化对土壤呼吸的影响

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摘要

Climate change scenarios predict increases in temperature, changes in precipitation patterns, and longer drought periods in most semi-arid regions of the world. Ecosystems in these regions are prone to land degradation, which may be aggravated by climate change. Soil respiration is one of the main processes responsible for organic carbon losses from arid and semi-arid ecosystems. We measured soil respiration over one year in two steppe ecosystems having different degrees of land degradation under three ground-covers: with vegetation, bare soil, and an intermediate situation between plants and bare soil.The largest differences in soil respiration rates between the sites were observed in spring, coinciding with the highest level of plant activity. The degraded site had drier and hotter soils with less soil water availability and a longer drought period. As a result, vegetation on the degraded site did not respond to spring rainfall events. Soil respiration showed a strong seasonal variability, with average annual rates of 1.1 and 0.8 mu mol CO2 m(-2) s(-1) in the natural and degraded sites, respectively. We did not observe significant differences in soil respiration rates associated with ground-cover i.e., the temporal variation was much larger than the spatial variation. At both sites, soil moisture was the controlling driver of soil respiration for most of the year, when temperatures were above 20 degrees C and constrained the response to temperature for the few months when the temperature was below 20 degrees C. An empirical model based on soil temperature and soil moisture explained 90% and 72% of the seasonal variability of soil respiration on the natural and degraded sites, respectively. For the first time, this study suggests that land degradation may alter the carbon balance of these ecosystems through changes in the temporal dynamics of soil respiration and plant productivity, which have important negative consequences for ecosystem functioning and sustainability
机译:气候变化情景预测,世界上大多数半干旱地区的气温将会升高,降水模式将发生变化,干旱时期将更长。这些地区的生态系统容易发生土地退化,气候变化可能会加剧土地退化。土壤呼吸是造成干旱和半干旱生态系统有机碳损失的主要过程之一。我们在三个植被覆盖,裸露的土壤和植物与裸露的土壤之间的中间情况下,在两个具有不同土地退化程度的草原生态系统中,测量了一年内的土壤呼吸作用。两个站点之间土壤呼吸速率的最大差异是在春季观察到,与植物活动的最高水平相吻合。退化地点的土壤较干燥,较热,土壤水分较少,干旱期较长。结果,退化地点的植被对春季降雨事件没有响应。土壤呼吸显示出强烈的季节性变化,在自然和退化地点的年平均速率分别为1.1和0.8μmol CO2 m(-2)s(-1)。我们没有观察到与地面覆盖相关的土壤呼吸速率的显着差异,即时间变化远大于空间变化。在这两个地点,当温度高于20摄氏度时,一年中的大部分时间里,土壤水分都是土壤呼吸的控制因素,而当温度低于20摄氏度时,土壤水分在几个月中都限制了对温度的响应。土壤温度和土壤湿度分别解释了自然地点和退化地点土壤呼吸季节变化的90%和72%。这项研究首次表明,土地退化可能通过土壤呼吸和植物生产力的时间动态变化而改变这些生态系统的碳平衡,这对生态系统的功能和可持续性具有重要的负面影响。

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