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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Coupled UV-exposure and microbial decomposition improves measures of organic matter degradation and light models in humic lake
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Coupled UV-exposure and microbial decomposition improves measures of organic matter degradation and light models in humic lake

机译:耦合紫外线暴露和微生物分解改善了腐殖湖中有机物质降解和光学模型的措施

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Increasing terrestrial input of colored dissolved organic matter (CDOM) to temperate softwater lakes has reduced transparency, distribution of pristine rosette plants and overall biodiversity in recent decades. We examined microbial and UV-induced reduction of absorption by CDOM and dissolved organic carbon pools (DOC) in humic water from a groundwater-fed softwater lake as well as groundwater received from surrounding heathland and coniferous forest. An experimental setup that mimics naturally coupled continuous UV-exposure and microbial degradation was introduced and compared with experiments applying a single initial or no UV-exposure. We found that decreases of CDOM and DOC concentrations were negligible in groundwater and very small in lake water over 30 days in the absence of UV-exposure. Initial UV-exposure increased degradation rates, but further degradation ceased after 20 days preventing determination of the natural time course of degradation. Coupled continuous UV-exposure and microbial degradation showed high and constant degradation of CDOM (340 nm) over 30 days removing 87% of the initial absorption in heathland groundwater, and 20% in forest groundwater and lake water. Declines in DOC concentrations over 30 days were 34%, 28% and 13% of the initial levels in heathland groundwater, forest groundwater and lake water, respectively. Model estimates showed that a shift in land use from a forest dominated to a heathland dominated catchment could increase lake transparency from 0.6 to 2.5 m. and expand plant-covered area from 3 to 35%. The main time delay to a new steady state of better light climate would be degradation of soil organic pools and exchange of groundwater magazines, while the delay in the lake water after a complete shift to inflow of CDOM-poorer groundwater would last only 1-2 years. Consequently, changes in CDOM levels in groundwater input should have relatively rapid and marked influence on light conditions and plant distribution in shallow softwater lakes.
机译:增加了彩色溶解有机物质(CDOM)的陆地投入,以温带软水湖泊,近几十年来降低了透明度,原始玫瑰花植物和整体生物多样性的分布。我们检查了来自地下水供给软水湖的CDOM和溶解的有机碳库(DOC)的微生物和紫外线诱导的吸收减少,以及从周围的Heathland和针叶林接收的地下水。引入了模拟天然耦合的连续紫外线暴露和微生物降解的实验设置,并与应用单一初始或无紫外线暴露的实验进行比较。我们发现,在没有紫外线暴露的情况下,在地下水和湖水中的湖水中较小的CDOM和DOC浓度的降低是忽略不计。初始紫外线暴露增加降解速率,但在20天后再消除降解进一步降解,防止测定了降解的自然时间进程。耦合连续紫外线暴露和微生物降解显示CDOM(340nm)的高且恒定的降解30天,除去Heathland地下水的初始吸收的87%,20%在森林地下水和湖水中。 30天内的DOC浓度下降分别为Heathland地下水,森林地下水和湖水初始水平的34%,28%和13%。模型估计表明,从主导地位的森林的土地利用转移可以将湖泊透明度从0.6升增加到2.5米。并将植物覆盖面积从3升至35%。新的稳定状态更好的轻微气氛的主要时间延迟将降低土壤有机池和地下水杂志的交换,而湖水延迟到湖水之后的CDOM - 较贫穷的地下水的流入将持续1-2年。因此,地下水投入中的CDOM水平的变化应该对浅软水湖泊的光线和植物分布产生相对迅速和显着的影响。

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