首页> 外文期刊>International journal of ecohydrology and hydrobiology >Unraveling the ecological functioning of the monsoonal Songkhram river floodplain in Thailand by integrating data on soil, water, and vegetation
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Unraveling the ecological functioning of the monsoonal Songkhram river floodplain in Thailand by integrating data on soil, water, and vegetation

机译:通过整合土壤,水和植被的数据来解除泰国季风嵩高河洪泛区的生态运作

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Although the functioning of river floodplains as sink or source of nutrients has been studied extensively for temperate regions, similar studies in tropical regions are less abundant and studies integrating data about floodplain soil, vegetation, and water are scarce. We examined and compared nutrient contents in soil, water, and vegetation tissue in two different vegetation zones on the monsoon Songkhram river floodplain (Thailand). Significant differences were found between bamboo and grass zones. The soil in the bamboo zone is more fertile than the soil in the grass zone, as indicated by the lower C/N ratio, and has significantly higher organic matter and higher total N and K. Bamboo leaf tissue had significantly higher concentrations of nutrients than grass biomass. The growth of the bamboo is P-limited or P and N co-limited, but grass is N-limited. In both zones, the soil-available P and organic carbons after flooding were significantly lower than before flooding. Floodwater in both zones had low dissolved solid concentrations. After the flood peak, most concentrations tended to increase, especially organic carbon and dissolved nitrogen but phosphorus decreased. The results suggest a significant loss of organic carbon from the soil after flooding, indicating that the floodplain acts as a source of carbon that is exported downstream. Nonetheless it is also evident that the floodwater brings in sediment and nutrients. Based on rough estimations of nutrient budgets we conclude that the highly productive bamboo zone adjacent to the river filters out the nutrients before they reach the grass zone. (C) 2017 European Regional Centre for Ecohydrology of the Polish Academy of Sciences. Published by Elsevier Sp. z o.o. All rights reserved.
机译:虽然河流泄漏作为水槽或营养素来源的运作已经过度研究了温带地区,但热带地区的类似研究不太丰富,研究整合有关洪泛区土壤,植被和水的数据是稀缺的。我们在季风宋卡姆河洪泛区(泰国)的两种不同植被区中的土壤,水和植被组织中检测和比较了土壤,水和植被组织的营养物质。竹子和草区之间发现了显着差异。竹子区的土壤比草区的土壤更为肥沃,如下面的C / N比率所示,有机质和更高的总N和K.竹叶组织具有显着高于营养素的营养物质草生物量。竹子的生长是p限制或p和n合同,但草是n-limited。在两个区域中,洪水后的土壤可用的P和有机碳是显着低于洪水之前。两个地区的洪水具有低溶解的固体浓度。洪峰后,大多数浓度往往增加,尤其是有机碳和溶解的氮,但磷减少。结果表明洪水后土壤中有机碳的显着损失,表明洪泛平原作为出口下游的碳源。尽管如此,洪水也会带来沉积物和营养素。根据对营养预算的粗略估计,我们得出结论,河流附近的高效竹区在进入草区之前过滤出营养物质。 (c)2017欧洲区域科学院生态学学中心。由elsevier sp发布。动物园。版权所有。

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