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Sand Dunes in Qassim Region: Geomorphological Characteristics and Economic Value: An Empirical Study

المصدر: مجلة كلية الآداب
الناشر: جامعة الإسكندرية - كلية الأداب
المؤلف الرئيسي: Al-Awady, Hamdeno (Author)
مؤلفين آخرين: Al-Dughairi, Ahmed (Co-Author)
المجلد/العدد: ع88
محكمة: نعم
الدولة: مصر
التاريخ الميلادي: 2017
الصفحات: 375 - 409
رقم MD: 1121383
نوع المحتوى: بحوث ومقالات
اللغة: الإنجليزية
قواعد المعلومات: AraBase
مواضيع:
كلمات المؤلف المفتاحية:
Nafud | Sand Dunes | Grain Size | Geochemical | Wind Ripples | Internal Structure | Dune Vegetation | Qassim Region and Saudi Arabia
رابط المحتوى:
صورة الغلاف QR قانون
حفظ في:
LEADER 02878nam a22002297a 4500
001 1863768
041 |a eng 
044 |b مصر 
100 |9 602338  |a Al-Awady, Hamdeno  |e Author 
245 |a Sand Dunes in Qassim Region:  |b Geomorphological Characteristics and Economic Value: An Empirical Study 
260 |b جامعة الإسكندرية - كلية الأداب  |c 2017 
300 |a 375 - 409 
336 |a بحوث ومقالات  |b Article 
520 |b OSL dating technique has shown different periods of sand accumulation in the Qassim region. The lithified basis of dune fields at depth more than 50 m under the general level were accumulated and formed during Pleistocene age (99.5 Ka). Consequently, two different dune patterns were formed, the lower or older dunes at the early of Holocene (9.8 Ka), then the upper or recent ones were formed from 3.5 Ka until only 200 years ago. Recent pattern is active and mainly formed from barchans and transverse types, but the older one is inactive and consists essentially of dome-shaped dunes. Between them, there is a grassy surface at varying elevations above sea level. This surface separates between to two different distinct sand faces as well as two different periods of dune formation. The main geomorphological features of these dunes are discussed on the basis of dune type, origin, wind direction and velocities, wind ripples, internal structure and dune vegetation. An attempt was made to differentiate between the two patterns of sand dunes as well as the sediments of Wadi ar Rumah’s floodplain. The differentiation depends upon grain size distribution curves, statistical parameters, geochemical characteristics and OSL dating techniques. The older dune sands are finer, more sorted, positive skewed and have slightly lower kurtosis values than the recent ones and also the Wadi ar Rumah floodplain. On the other hand, the study of geochemical characteristics indicates that the older dunes and the floodplain of Wadi ar Rumah are more alkaline than the recent dunes. While the EC and TDS tend to increase in the recent dunes than the older dunes and Wadi ar Rumah floodplain. Carbonate, bicarbonate and chloride in general occur in narrow range as a result of weathering. While the concentration of micronutrient metals (Fe, Mg, Zn and Cu) decrease significantly with the decreasing in finer fractions. 
653 |a التغيرات المناخية  |a تموجات الرياح  |a الكثبان الرملية  |a السعودية 
692 |b Nafud  |b Sand Dunes  |b Grain Size  |b Geochemical  |b Wind Ripples  |b Internal Structure  |b Dune Vegetation  |b Qassim Region and Saudi Arabia 
700 |a Al-Dughairi, Ahmed  |e Co-Author  |9 602342 
773 |4 الادب  |6 Literature  |c 007  |l 088  |m ع88  |o 0310  |s مجلة كلية الآداب  |v 000 
856 |u 0310-000-088-007.pdf 
930 |d n  |p y  |q n 
995 |a AraBase 
999 |c 1121383  |d 1121383 

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