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首页> 外文期刊>Revista Brasileira de Biologia >Microbial respiration and chemical composition of different sediment fractions in waterbodies of the upper Paraná River floodplain, Brazil
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Microbial respiration and chemical composition of different sediment fractions in waterbodies of the upper Paraná River floodplain, Brazil

机译:巴西巴拉那河上游漫滩水体中不同沉积物组分的微生物呼吸和化学成分

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Four size fractions of the sediment of six environments of the upper Paraná River floodplain were analyzed for carbon, nitrogen, and phosphorus contents and microbial respiration (oxygen consumption). Particle size did not affect nitrogen and phosphorus content or microbial activity, but did affect carbon content (F = 4.274, df = 3; 20, p = 0.020). The carbon concentration of ultra-fine particles was significantly lower than that of other sizes of sediment particles. Microbial respiration values were well predicted by sediment chemical composition, as shown by multiple regression (microbial respiration = -0.39 - 0.210C + 0.108N + 0.796P; F = 7.0495, p = 0.0022). However, phosphorus was the element which best explained the microbial respiration (partial coefficient = 0.796, p = 0.0039, n = 23). Considering that i) phosphorus was the best predictor of microbial respiration; ii) phosphorus is trapped in the series of reservoirs located upstream from the section of the floodplain studied; and iii) microbial respiration is a measure of decomposition rates and nutrient cycling, we hypothesize that the long-term accumulation of litter detritus and reduction of nutrient cycling in environments of the upper Paraná River floodplain are probable impacts of this decrease in phosphorus caused by the upstream reservoirs.
机译:分析了巴拉那河上游漫滩的六个环境中沉积物的四个大小部分的碳,氮和磷含量以及微生物呼吸(耗氧量)。粒度不影响氮,磷含量或微生物活性,但影响碳含量(F = 4.274,df = 3; 20,p = 0.020)。超细颗粒的碳浓度显着低于其他尺寸的沉积物颗粒。微生物呼吸值可以通过沉积物的化学成分很好地预测,如多元回归所示(微生物呼吸= -0.39-0.210C + 0.108N + 0.796P; F = 7.0495,p = 0.0022)。但是,磷是最能解释微生物呼吸的元素(偏系数= 0.796,p = 0.0039,n = 23)。考虑到i)磷是微生物呼吸的最佳预测指标; ii)磷被困在所研究的洪泛区的上游一系列储层中; iii)微生物呼吸是衡量分解速率和养分循环的指标,我们假设巴拉那河上游平原环境中垃圾碎屑的长期积累和养分循环的减少可能是由磷引起的磷减少的影响。上游水库。

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