Water system for underground water basins between Free Rivers Ghamqa and Abrash - Southern Tartous

Natural changes in the level of ground water through time is gaining great importance in evaluating the water system and to provide a lot of information about groundwater movement , which allows the assessment of the water situation public water layer in the study area . We adopted our measurements in groundwater levels frequencies on a private network monitoring hydrogeological She is the author of 26 wells distributed over the entire area of the region studied were carried out in some measurements for a period of six years. The study found that groundwater system of climate type (water division line) is directly linked to seep from rainfall and seepage from canals and irrigation water plays a significant role in the pose, which is characterized by Baltkareh and periodic quarterly in the annual changes of the levels, and the stability and balance in the conditions of these elevations, and the general direction of movement of groundwater will be from the east and north-east towards the west and southwest and Askew Hydraulic 0.005 a faddish topographic situation and the general trend of the cracks and fissures in the area.