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首页> 外文期刊>Lakes & Reservoirs >Temporal and spatial patterns based on sediment and sediment-water interface characteristics along a cascade of reservoirs (Paranapanema River, south-east Brazil)
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Temporal and spatial patterns based on sediment and sediment-water interface characteristics along a cascade of reservoirs (Paranapanema River, south-east Brazil)

机译:基于一系列水库(巴西东南部的帕拉纳帕内玛河)上的沉积物和沉积物-水界面特征的时空格局

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摘要

Physical and chemical characteristics of the sediments in a cascade of eight reservoirs located in the Paranapanema River (south-east Brazil) were analysed during two consecutive years during summer (January), autumn (April), winter (July) and spring (October) of 2000 and 2001, respectively. The granulometric texture, organic matter content and nutrient concentration (total nitrogen and phosphorus) were determined in the superficial sediment of 19 sampling stations, as well as the temperature, dissolved oxygen, pH, conductivity and redox potential in the bottom layer of the water column. Seasonal and spatial changes were observed for both years, especially for organic matter and nutrient concentrations. Three different areas could be identified along the river, which corresponded to the upper, middle and lower Paranapanema basin. The first area was characterized by an increase of nutrients and organic matter in the sediments and a decrease of temperature and dissolved oxygen in the downstream direction. The second one represented a region where fluctuations in nutrient and organic matter concentrations and a reduction in dissolved oxygen were observed. In the third area, there was an increase in nutrient and organic matter in the sediments and also an increase in temperature and dissolved oxygen towards the river mouth. The results of the principal components analysis, using water and sediments variables, showed the ordination of sampling stations by periods: wet (January-April) and dry (July-October) during 2000. This pattern was also verified during 2001, but with slight changes, probably due to the increase in the rains which would have produced certain homogenization effects along the river.
机译:在夏季(一月),秋季(四月),冬季(七月)和春季(十月)连续两年分析了位于巴拉那帕内玛河(巴西东南部)的八个水库的级联中沉积物的物理和化学特征。分别为2000年和2001年。测定了19个采样站表层沉积物的粒度结构,有机物含量和养分浓度(总氮和磷),以及水柱底层的温度,溶解氧,pH,电导率和氧化还原电势。两年都观察到季节和空间变化,尤其是有机质和营养物浓度。沿河可识别出三个不同的区域,分别对应上,下和下巴拉那帕内玛盆地。第一个区域的特征是沉积物中养分和有机质增加,下游方向的温度和溶解氧降低。第二个区域代表一个区域,在该区域中观察到营养物和有机物浓度的波动以及溶解氧的减少。在第三区域,沉积物中的营养物和有机物增加,并且向河口的温度和溶解氧增加。使用水和泥沙变量进行的主成分分析结果表明,按时间段划分了采样站的排序:2000年期间为湿(1月至4月)和干燥(7月至10月)。这种模式在2001年也得到验证,但略有减少变化可能是由于降雨增加,沿河会产生一定的均质化作用。

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