Titlebook: Agriculture, Recreation, Water Quality and Nature Protection in the Hula Valley, Israel; 70 years of a Mega-e Moshe Gophen Book 2023 The Ed

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Subterranean Migration of Nutrients in the Hula Valley,nsequently, the dominant direction of underground water flows and nutrient migration is from north to south. Nutrients and water migrate through the underground preferential pathways. Concentrations of Nitrogen and Phosphorus substances are higher in the northern part of the Hula Valley. The Ground

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Nutrients Dynamics in Lake Agmon-Hula,t sources and their dynamics are presented in this chapter. The input sources are Canal Z (syn. 101), Hula East, and reconstructed river Jordan. Lake effluents were sampled as well. Geochemical features of lake Agmon-Hula are nitrogen sink by de-nitrification and sedimentation whilst phosphorus fluc

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HALL

Hula Valley and Lake Kinneret Interrelationships: Future Management Proposition of Lake Agmon-Hula e protection, tourism, and public relations issues. An attempt of a tentative prognosis design is suggested for the management of Lake Agmon-Hula. The reduction of phosphorus and enhancement of nitrogen through Lake Agmon-Hula is beneficial to the Kinneret ecosystem. A proposal of diversion of peat

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Climatological Dryness and Water Loss in the Hula Valley,hrough preferential pathways in the northern and southern parts of the valley are therefore dissimilar, and nutrient concentrations are higher in the south, where GWT is lower. Nevertheless, the existence of an enigmatic water and nutrients “l(fā)oss” through migration to deeper layers is not impossible