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The phreatic groundwater from the Ialomita – Buzau river basin are quartered in the sedimentary formations of Quaternary age, starting with the ones of the lower Pleistocene and finishing with the Holocene and recent ones. The most important phreatic aquifer layers, from the point of view of the water resources quartered in permeable and raw formations (gravels, blocks, raw and average sands), are spread in the Buzau dry delta area, in the divagation plain between Buzău and Călmăţui and in the alluvial plain...

Groundwater is an important source of drinking water for many human communities, both urban and rural, their quality directly determining the health state of the population. At European level a great importance is given to water, the Water Framework Directive 60/200/EC establishing clear objectives through which all European waters (including groundwaters) should achieve a “good status” until 2015 and through which water should be used in a sustainable way throughout Europe. In this context, sanitary protectio...