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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >The Amazon. Bio-geochemistry applied to river basin management Part I. Hydro-climatology, hydrograph separation, mass transfer balances, stable isotopes, and modelling
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The Amazon. Bio-geochemistry applied to river basin management Part I. Hydro-climatology, hydrograph separation, mass transfer balances, stable isotopes, and modelling

机译:亚马逊。生物地球化学在流域管理中的应用第一部分。水文气候学,水文图分离,传质平衡,稳定同位素和建模

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A hydrochemical model, using hydrograph separation, developed for the Niger basin, has been proposed as a strategic tool for studying the watershed dynamics at any time and space scales. The model is applied to the Amazon basin, including the main channel and its major tributaries. The database corresponds to a sampling and analytical program developed over 8 cruises at 9 stations (about 70 samples), collected in the framework of the CAMREX Project (1982-1984). The model, based on a hydrograph separation of 3 reservoirs, is successful in extrapolating and predicting the geochemical and environmental behaviour of such large basins, naturally submitted to large secular or annual, regular or even catastrophic climatic oscillations. Several topics have been considered. (1) Coherence among the physico-chemical analyses: dissolved species (pH, NH4+, Na+, K+, Ca2+, Mg2+, NO3-, HCO3-, Cl-, DOC-, SO42-, HPO42-, SiO2, O-2 and CO2), and inorganic or organic suspended load (fine and coarse fractions FSS, CSS, POCF, POCC). (2) Hydrograph separation in 3 reservoir contributions: R-S, the superficial or rapid runoff, R-1, the hypodermic or intermediate runoff, including the flood plain contributions, and R-B the ground water or base flow. (3) Estimation of the isotopic and physico-chemical features of each of the 3 flow components: R-S, R-I, and R-B. (4) Determination of the 3 hydrological parameters (size of the reservoir, drying up coefficient, and residence time of water), characterizing each of the 3 flow components (R-S, R-I, and R-B), in each of the 9 basins considered. (5) Hydrological and geochemical balances for all the parameters analysed either (a) cruise by cruise for all tributaries and the Amazon River at Obidos, or (b) among each of the 3 river flow components. (6) Isotopic data set of delta(18)O in waters, tests of coherence of the hydrograph separation model. (7) Relationships between isotopic signatures and morphological or hydroclimatical parameters characterizing the river-soil-vegetation systems. The developed procedure presents a new tool in environmental predictions, emphasizing the potentiality of geochemical interpretation of complex hydrochemical data sets. (c) 2005 Elsevier Ltd. All rights reserved.
机译:已经提出了为尼日尔盆地开发的利用水位线分离的水化学模型,作为研究任何时间和空间尺度的流域动力学的战略工具。该模型应用于亚马逊流域,包括主要河道及其主要支流。该数据库对应于在CAMREX项目(1982-1984年)的框架内在9个站进行的8次航行中开发的采样和分析程序(约70个样本)。该模型基于3个水库的水文分离,成功地推断和预测了这种大盆地的地球化学和环境行为,这些大盆地自然会遭受长期或长期,定期甚至灾难性的气候振荡。已经考虑了几个主题。 (1)理化分析之间的连贯性:溶解物(pH,NH4 +,Na +,K +,Ca2 +,Mg2 +,NO3-,HCO3-,Cl-,DOC-,SO42-,HPO42-,SiO2,O-2和CO2)和无机或有机悬浮负荷(细颗粒和粗颗粒FSS,CSS,POCF,POCC)。 (2)在3个水库储层中进行水文法分离:R-S,表层或快速径流,R-1,皮下或中层径流,包括洪泛区贡献,R-B地下水或基流。 (3)估算3种流动组分:R-S,R-I和R-B各自的同位素和理化特征。 (4)确定3个水文参数(水库的大小,干燥系数和水的滞留时间),表征所考虑的9个盆地中每个3个流量分量(R-S,R-I和R-B)的特征。 (5)分析的所有参数的水文和地球化学平衡(a)对所有支流和奥比都斯的亚马逊河进行逐流航行,或(b)在3条河流流量分量中的每一个之间。 (6)水中δ(18)O同位素数据集,水位图分离模型的相干性测试。 (7)同位素特征与表征河流-土壤-植被系统的形态学或水文气候参数之间的关系。开发的程序提供了一种环境预测的新工具,强调了复杂水化学数据集的地球化学解释潜力。 (c)2005 Elsevier Ltd.保留所有权利。

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