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首页> 外文期刊>Environmental Science and Pollution Research >Factors that control the spatial and temporal distributions of phosphorus, nitrogen, and carbon in the sediments of a tropical reservoir
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Factors that control the spatial and temporal distributions of phosphorus, nitrogen, and carbon in the sediments of a tropical reservoir

机译:控制热带水库沉积物中磷,氮和碳的空间和时间分布的因素

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摘要

The impacts of anthropic activities have had profound effects on the nitrogen (N) and phosphorus (P) cycles in many aquatic ecosystems. We investigated the spatial and temporal distributions of carbon (C), N, and P in the sediments of a tropical Paiva Castro Reservoir (S?o Paulo, Brazil), as well as their release and retention in the system. In 2010, surface sediments were collected at nine sites in the reservoir, and a core was obtained in the limnetic zone, in 2010. The core was dated using the_(210)Pb technique. The organic C content was estimated from organic matter concentration, which was measured by the loss-on-ignition method, and the concentrations of P and N were determined by spectrophotometry. Marked spatial heterogeneity in the Paiva Castro sediments associated with both natural variations in the water body and variations induced by human impacts was observed. Heterogeneity was evidenced by a decrease in the allochthonous contribution of organic matter (C/N) in the upstream-downstream direction and increases of N and P, mainly associated with water flows in the different compartments of the reservoir. In the core, C and N concentrations display significant positive correlations with increases in population and agricultural activities in the drainage basin through time. The C/P molar ratios in surface sediments are indicative of human impacts in the region, as C:P ratios in the sediment are low (7.8:1) compared to the Redfield ratio (C:P?=?108:1). Predominance of oxic conditions at the sediment surface and particles sizes
机译:人类活动的影响对许多水生生态系统中的氮(N)和磷(P)循环产生了深远的影响。我们研究了热带Paiva Castro水库沉积物中的碳(c),n和p的空间和时间分布(S?O Paulo,Brazil)以及系统释放和保留。在2010年,在储存器中的九个地点收集表面沉积物,2010年在紫尼区获得核心。使用_(210)Pb技术进行核心。从有机物质浓度估计有机C含量,通过损失点火方法测量,并通过分光光度法测量P和N的浓度。观察到与水体的自然变化相关的Paiva Castro沉积物中标记的空间异质性和人类撞击诱导的变化。通过在上游下游方向上下游方向的有机物质(C / N)的表发育的减少和N和P的增加来证明异质性,主要与水库不同隔室中的水流相关。在核心,C和N浓度随着时间推移,C和N浓度与排水盆中的人口和农业活动的增加表现出显着的正相关。表面沉积物中的C / P摩尔比指示该区域的人体撞击,因为与REDFIEL比率相比,沉积物中的C:P比率低(7.8:1)(C:P?= 108:1)。沉积物表面和颗粒尺寸的氧化条件的优势<α63≤μm为沉积物中的P保留提供了有利条件,这有助于防止富营养化。本研究中使用的方法应扩展到其他地点,特别是在菊雌营养和寡糖储层中,以提供有关这种水生生态系统中的历史影响的信息。

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