Chemical, Hydrological and Climatological Properties of Lake Agmon, Hula Valley (Israel), (1994-2006)

M. Gophen, M. Meron, Y. Tsipris, Valerie Orlov-Levin, Mordechay Peres
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引用次数: 9

Abstract

The first decade of monitoring program in Lake Agmon (Hula Valley, Northern Israel) is summarized. The presented part of the program include: water discharges, physico-chemical (pH, EC, Temperature) and chemical parameters (TP, TN, TDN, TDP, NO3, NH4, SO4, TDS, TSS,). It was found that Nitrogen concentrations decline from north to south and the opposite for Phosphorus. Resulting of re-suspension by wind direction of western-southern-eastern and averaged maximal velocities of 9 - 10 m/s is suggested. De-nitrification and particles sedimentation emphasize Lake Agmon as a sink for Nitrogen. Sulfate-Carbonates association and the production of precipitated Gypsum (CaSO4) highlight the sink property of Lake Agmon. Nevertheless Sulfate removal by the Lake Agmon hydrological system is significant.
以色列呼拉谷阿格蒙湖化学、水文和气候特征(1994-2006)
总结了以色列北部呼拉谷阿格蒙湖监测项目的第一个十年。该方案的介绍部分包括:水排放、理化参数(pH、EC、温度)和化学参数(TP、TN、TDN、TDP、NO3、NH4、SO4、TDS、TSS、)。结果表明,氮浓度由北向南递减,磷浓度由北向南递减。提出了西南风、东南风、平均最大风速为9 ~ 10 m/s的再悬浮效应。脱氮作用和颗粒沉降作用强调了阿格蒙湖作为氮汇的作用。亚硫酸盐-碳酸盐结合和沉淀石膏(CaSO4)的产生突出了阿格蒙湖的汇性。然而,阿格蒙湖水文系统对硫酸盐的去除作用是显著的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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