...
首页> 外文期刊>Ecological indicators >Does change in precipitation magnitude affect the soil respiration response? A study on constructed invaded and uninvaded tropical grassland ecosystem
【24h】

Does change in precipitation magnitude affect the soil respiration response? A study on constructed invaded and uninvaded tropical grassland ecosystem

机译:降水量的变化会影响土壤呼吸反应吗?人工入侵和非入侵热带草原生态系统的构建研究

获取原文
获取原文并翻译 | 示例
           

摘要

Change in precipitation in tropics would have a severe consequence on soil CO2 flux and on its major determinants like soil temperature and soil moisture. Variation in climatic condition also supports the establishment of invasive species in the area. In this communication an attempt is made to assess the impact of change in precipitation regime on soil CO2 flux in a constructed tropical grassland with and without an invasive plant, Hyptis suaveolens. Three rainout shelters with manipulated precipitation doses (i) of 800 mm (20% the below average), (ii) 1100 mm (average) and (iii) 1600 mm (60% above the average) were established, along with one unsheltered plot (open C) receiving ambient precipitation. Each rain-out shelter containing three sub-treatments viz. (i) bare plots with no vegetation, (ii) uninvaded indigenous grassland plots (NIG), and (iii) grassland plots invaded with H. suaveolens (IG). Significant high soil CO2 flux was found in plots receiving maximum precipitation (1600 mm) and low in plots receiving minimum precipitation (800 mm). Furthermore, vegetated plots (NIG and IG) exhibited higher soil CO2 flux than the non-vegetated plots. Among the vegetated plots, IG plots receiving maximum precipitation (1600 mm) had highest soil CO2 flux, followed by IG plots receiving 1100 mm, and 800 mm precipitation. Seasonal and monthly observations showed that maximum soil CO2 flux occurred in rainy season, (in July), and minimum in winter season (in January). The important controlling factors for soil CO2 flux were soil moisture, root biomass and soil temperature. In this study soil moisture explained 61% variability in the soil CO2 flux. A linear combination of moisture and root biomass explained 74% variability in soil CO2 flux, and when temperature was added in the multiple regression a total of 79% variability in soil CO2 flux was accounted for. These findings would help us to understand the biological thresholds of tropical ecosystem related to precipitation regime. It will encourage researchers around the globe to develop ecosystem models, which would enable to forecast the impact of climate change on nutrient cycling.
机译:热带地区降水的变化将对土壤二氧化碳通量及其主要决定因素(如土壤温度和土壤湿度)产生严重影响。气候条件的变化也支持该地区入侵物种的建立。在这种交流中,尝试评估降水状态的变化对人工热带草原(带或不带入侵植物Hyptis suaveolens)的土壤CO2通量的影响。建立了三个雨棚,其中雨量控制剂量(i)为800毫米(低于平均值20%),(ii)1100毫米(平均值)和(iii)1600 mm(高于平均值60%),以及一个未设防的地块(C开口)接收环境降水。每个防雨棚都包含三个子处理。 (i)没有植被的裸露土地;(ii)未入侵的本土草原地块(NIG),以及(iii)入侵了suaveolens(IG)的草地。在最大降水量(1600毫米)的样地中发现了较高的土壤CO2通量,在最小降水量(800毫米)的样地中发现了较低的土壤CO2通量。此外,植被地块(NIG和IG)的土壤CO2通量要高于非植被地块。在有植被的样地中,接受最大降水量(1600毫米)的IG地块具有最高的土壤CO2通量,其次是接受1100毫米和800毫米降水量的IG地块。季节性和月度观测表明,土壤二氧化碳通量最大发生在雨季(7月),最小发生在冬季(1月)。土壤CO2通量的重要控制因素是土壤水分,根系生物量和土壤温度。在这项研究中,土壤水分解释了土壤CO2通量的61%变异性。水分和根生物量的线性组合解释了土壤CO2通量的74%变化,当在多元回归中添加温度时,土壤CO2通量的总变化为79%。这些发现将有助于我们了解与降水状况有关的热带生态系统的生物学阈值。它将鼓励全球研究人员开发生态系统模型,这将有助于预测气候变化对养分循环的影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号