الظروف الجيولوجية والهيدروجيولوجية لمنطقة برج إسلام
Abstract
تقع منطقة البحث شمال مدينة اللاذقية، يحدها من الشمال نهر وادي قنديل، ومن الجنوب والشرق نهر العرب، ومن الغرب البحر المتوسط.
يهدف البحث إلى دراسة ظروف توضع المياه الجوفية في المنطقة، وتقويم موارد المياه الجوفية فيها.
اعتمدت الدراسة على القياسات في شبكة رصد موزعة بشكل شبه منتظم في المنطقة. تتألف الشبكة
من 24 بئراً مراقبة محفورة في توضعات النيوجين والباليوجين.
تتأرجح تغيرات مناسيب المياه الجوفية في توضعات النيوجين بين 0 و 0.62 م، بسبب التغذية الراشحة من مياه الأمطار شتاءً، وتسرب مياه شبكات الري صيفاً. بينما تصل تغيرات مناسيب المياه الجوفية في توضعات الباليوجين إلى 20 متراً.
تتأرجح الناقلية الكهربائية للمياه الجوفية بين 450 و 1255 ميكروموس/سم، حيث تُسهم مياه البحر في زيادة ملوحة المياه الجوفية في منطقة شاليهات رأس شمرا.
The research area located at the north of Latakia; it is bounded by Wadi Qandil River from the north, Al-Arab River from the south and the east, and the Mediterranean Sea from the west.
The research aimed to study and evaluate the groundwater resources in the area. The study depends on measuring on observation network, which is regularly distributed in the region. The network consists of 24 wells drilled in the Neogene and Paleogene deposits.
The changes of groundwater levels in the Neogene deposits fluctuate between 0 and 0.62m, due to the infiltration of the rainfall in winter, and of irrigation water in summer, while the changes in the Paleogene reaches to 20m.
The electrical conductivity of the groundwater amount to 450 - 1255µs/cm, that the sea water contributes to increase the saltiness of groundwater at the area of Rass Shamra beach cabins.
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