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Effects of atmospheric CO2 concentration on soil-water retention and induced suction in vegetated soil

机译:大气二氧化碳浓度对植被土壤水保留和诱导吸力的影响

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摘要

Current atmospheric CO2 (400 ppm) is increasing 2 ppm annually and might reach up-to 1000 ppm by year 2100 due to global climate change. Different plant growth was observed under elevated CO2 in the previous studies. However, plant induced soil suction besides plants growth due to increasing atmospheric CO2 concentration in heavily compacted soil remain elusive. The objective of this study is to quantify transpiration and evapo-transpiration induced soil suction by Schefflera heptaphylla in heavily compacted soil under different atmospheric CO(2 )concentration. Three replicates of the plant were grown, and their characteristics were measured under 400 ppm and 1000 ppm CO2 concentration for three months. Leaf area index of plants decreased by 35% under 1000 ppm CO2 concentration due to soil nitrogen scarcity which impedes the plants ability to metabolize increased atmospheric CO2 concentration. Despite having LAI of 0.5-0.7, plant induced suction decreased by 10-25 kPa during transpiration and evapo-transpiration test under 1000 ppm CO(2 )concentration. Although a strong positive linear correlation (R-2 = 0.8-0.9; P-value 0.1) of LAI and root-shoot biomass ratio with induced peak soil suction under 400 ppm CO2 concentration, a weak linear correlation (R-2 = 0.6-0.8; P-value 0.1) of the same plant traits under 1000 ppm CO2 concentration was observed. This is because leaves cannot open stomata wide enough to transpire more water when they absorb more CO2 from the atmosphere resulting in soil suction reduction. This implies that the effects of atmospheric CO2 concentration on plant induced soil suction must be considered in vegetated soils.
机译:目前的大气二氧化碳(400ppm)每年增加2 ppm,由于全球气候变化,2100年可能达到高达1000 ppm。在先前的研究中,在CO 2升高的CO 2下观察到不同的植物生长。然而,植物诱导的土壤抽吸除植物生长外,由于增加了大气压的土壤中的大气二氧化碳浓度,仍然难以捉摸。本研究的目的是在不同大气CO(2)浓度下,量化什菲莱切拉氏菌在大型压实土壤中的蒸发和蒸发蒸腾诱导的土壤吸入。生长植物的三种重复,其特征在400ppm和1000ppm的CO 2浓度下测量三个月。由于土壤氮稀缺,植物的叶片区域植物指数下降了35%以下,由于土壤氮气稀缺,阻碍了植物代谢增加的大气二氧化碳浓度的能力。尽管含量为0.5-0.7,但在1000ppm co(2)浓度下,植物诱导的吸力在蒸腾蒸腾和蒸发蒸腾试验期间减少了10-25kPa。虽然具有在400ppm CO 2浓度下的诱导峰土壤吸力的赖和根芽生物质比的强烈的正线性相关(R-2 = 0.8-0.9; p值<0.1)。弱线性相关性(R-2 =观察到在1000ppm CO 2浓度下的相同植物性状的0.6-0.8; p值> 0.1)。这是因为叶不能打开足够宽的气孔,以便在从大气中吸收更多的二氧化碳时透射更多的水,导致土壤吸入减少。这意味着在植被的土壤中必须考虑大气二氧化碳浓度对植物诱导的土壤吸力的影响。

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