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Experimental manipulation of water levels in two French riverine grassland soils

机译:在法国的两种河流草地土壤中水位的实验处理

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In this experimental study, we simulated the effects of different river flooding regimes on soil nutrient availability, decomposition and plant production in floodplain grasslands. This was done to investigate the influences of soil water contents on nutrient cycling. Water levels were manipulated in mesocosms with intact soil turfs from two French floodplain grasslands. Three water levels were established: a 'wet' (water level at the soil surface), an 'intermediate' (water level at -20 cm) and a 'dry' treatment (water level at -120 cm). With increasing soil moisture, soil pH became more neutral, while redox-potential and oxygen concentration decreased. The 'dry' treatment showed much lower values for process rates in soil and vegetation than the 'intermediate' and 'wet' treatments. Regressions showed that soil C-evolution and N-mineralization were positively related to soil moisture content. Not all mineralized N was available for plant uptake in the wet treatment, as a considerable part was denitrified here. Denitrification was especially high as soil water contents increased to levels above field capacity, where redox-potentials sharply dropped. Further, soil P availability was higher under wet conditions. In the 'dry' treatment, soil water content was close to the wilting point and plant production was low. In the 'intermediate' treatment, plant production was most likely limited by nitrogen. The 'wet' treatment did not result in a further increase in plant production. Dam construction and river bed degradation can result in lower river levels and summer drought on floodplains. This experimental study suggests that summer drought on floodplain soils reduces decomposition of soil organic matter, nutrient availability, denitrification, plant production and nutrient uptake. This can affect the capacity of floodplains to remove or retain nutrients from river water in a negative way. (C) 2000 Editions scientifiques et medicales Elsevier SAS. [References: 70]
机译:在这项实验研究中,我们模拟了不同的洪水淹没制度对洪泛草原上土壤养分的有效性,分解和植物生产的影响。这样做是为了调查土壤水分对养分循环的影响。用来自两个法国洪泛区草地的完整土壤草皮在中层环境中控制了水位。确定了三个水位:“湿”(土壤表面的水位),“中级”(-20厘米的水位)和“干”处理(-120厘米的水位)。随着土壤湿度的增加,土壤的pH值变得更中性,而氧化还原电位和氧气浓度降低。与“中间”和“湿”处理相比,“干”处理在土壤和植被中的处理速率值要低得多。回归分析表明,土壤碳演化和氮矿化与土壤含水量呈正相关。在湿法处理中,并非所有矿化氮都可用于植物吸收,因为此处相当一部分被反硝化了。当土壤含水量增加到高于田间持水量水平(氧化还原电势急剧下降)时,反硝化作用特别高。此外,在潮湿条件下土壤磷的有效性更高。在“干式”处理中,土壤含水量接近于枯萎点,而植物产量较低。在“中间”处理中,植物生产极有可能受到氮的限制。 “湿式”处理并未导致植物产量的进一步增加。大坝的建设和河床的退化可能导致河床水位降低和洪泛区夏季干旱。该实验研究表明,洪泛区土壤上的夏季干旱减少了土壤有机质的分解,养分的可利用性,反硝化作用,植物生产和养分吸收。这会负面影响洪泛区从河水中去除或保留养分的能力。 (C)2000版的《科学与医学》 Elsevier SAS。 [参考:70]

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