التقييم الجيمورفولوجي للتعرية المائية للمنطقة المحصورة بين الطويلعة والماحوز غرب محافظة كركوك محمد عواد حسين/ جامعة تكريت/ كلية الاداب
الشريط الجانبي للمقالة
محتوى المقالة الرئيسي
الملخص
تُعد التعرية المائية من أبرز الظواهر الجيومورفولوجية التي تؤثر بعمق في تشكيل سطح الأرض وتغييره على مدى الزمن، خاصة في البيئات التي تتسم بتباين مناخي وهيدرولوجي واضح، وتضاريس غير مستقرة. وتكمن أهمية هذه الظاهرة في تأثيرها المباشر على استقرار التربة، وتراجع إنتاجية الأراضي الزراعية، وتدهور الغطاء النباتي، إلى جانب مساهمتها في فقدان الموارد الطبيعية، وتشكل أخاديد وانجرافات وانزلاقات أرضية في بعض الحالات, في ضوء هذه التحديات، تزداد الحاجة إلى إجراء دراسات جيومورفولوجية دقيقة تسلط الضوء على طبيعة وشدة التعرية المائية، لاسيما في المناطق التي تتعرض لضغوط بشرية مكثفة، مثل التوسع العمراني العشوائي، والرعي الجائر، وإزالة الغطاء النباتي، والاستغلال غير الرشيد للأراضي. ومن هنا، جاءت أهمية اختيار المنطقة الواقعة بين الطويلعة والماحوز غرب محافظة كركوك، كونها تمثل بيئة مثالية لدراسة التفاعل بين العوامل الطبيعية والبشرية، وتأثيرها المباشر في تصاعد عمليات التعرية.
المقاييس
تفاصيل المقالة
هذا العمل مرخص بموجب Creative Commons Attribution 4.0 International License.
المراجع
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