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Study on respiration of soils in the Jiulongjiang river basin and its effect factors

机译:九龙江流域土壤呼吸作用及其影响因素研究。

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Soil respiration has become the largest source that terrestrial ecosystems release CO2 to atmosphere, and it plays an important role in global carbon cycle. In this paper, dynamic variation of soil respiration and effect of temperature, water content and organic matter in three different habitats (vegetable plot, bamboo grove, banana forest) were evaluated using a laboratory soil incubation experiment. The findings indicated: (1) Under the different water content condition, the soil respiration speed has certain difference along with the temperature. Among 15∼35°C, soil respiratory rate in the vegetable plot, the bamboo grove, the banana forest, respectively, is 11.15∼32.45, 9.42∼30.34, 20.99∼30.34 mgCO2kg−1·h−1. Soil respiration''s change scope in the vegetable plot and the bamboo grove is higher than that in the banana forest soil. Soil respiration speed and water content in the vegetable plot soil and the banana forest assume the obvious inverse correlation, but soil respiration speed and water content in the bamboo grove has not obvious correlation. The temperature coefficient Q10 varied from 0.94∼1.7 in vegetable farmland, 0.95∼1.62 in bamboo grove earth, 0.95∼1.03 in banana forest earth, according to water content variation. In three types of soil, the vegetable plot soil is most sensitive to the temperature, next is the bamboo grove soil. But the banana forest soil is lowest to the temperature sensitivity. (2) The content order of high-activity organic matter in the soil is: the vegetable plot soil > the bamboo grove soil > the banana forest soil; therefore the soil carbon storehouse, particularly the activated carbon storehouse''s storage quantity is affecting the effect of temperature on soil respiration to a great extent. But the content order of total active organic matter is: the bamboo grove soil > t--he banana forest soil > the vegetable plot soil. Hence, changes of these factors have indicated complexity on the soil respiration research.
机译:土壤呼吸已成为陆地生态系统向大气释放CO 2 的最大来源,并且在全球碳循环中发挥着重要作用。本文通过实验室土壤培养实验评估了三种不同生境(菜地,竹林,香蕉林)土壤呼吸的动态变化以及温度,水分和有机质的影响。研究结果表明:(1)在不同含水量条件下,土壤呼吸速度随温度的变化有一定差异。在15〜35°C下,菜地,竹林和香蕉林的土壤呼吸速率分别为11.15〜32.45、9.42〜30.34、20.99〜30.34 mgCO 2 kg -1 ·h -1 。菜地土壤呼吸变化范围较大,竹林高于香蕉林土壤。菜地和香蕉林的土壤呼吸速度与含水量呈明显的反相关关系,而竹林土壤呼吸速度与含水量则无明显的相关关系。根据水分含量的变化,蔬菜农田的温度系数Q10从0.94〜1.7,竹林地的温度系数在0.95〜1.62,香蕉林地的温度系数在0.95〜1.03。在三种类型的土壤中,菜地土壤对温度最敏感,其次是竹林土壤。但是香蕉林土壤对温度的敏感性最低。 (2)土壤中高活性有机质的含量顺序为:菜地土壤>竹林土壤>香蕉林土壤;因此,土壤碳库,特别是活性碳库的储藏量在很大程度上影响温度对土壤呼吸的影响。但是总活性有机物的含量顺序为:竹林土壤> t- -- 他的香蕉林土壤>蔬菜田土壤。因此,这些因素的变化表明了土壤呼吸研究的复杂性。

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