MONITORING CHANGING POSITION OF THE SHORELINE ALONG BURULLUSBALTIM, NILE DELTA, EGYPT, AND THE RULE OF COASTAL DUNES AS A NATURAL DEFENSE AGAINST EROSION IN A GEO-HERITAGE SITE: REMOTE SENSING APPLICATION

Taha
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引用次数: 2

Abstract

Monitoring the coastal area along the Burullus-Baltim coast shows that it is a fragile coastal area composed of loose sand eroded from the old Sebennitic Promontory since historical time of more than 1000 years, then enhanced after the construction of Aswan High Dam (AHD). The interplay of waves, wind and sands along this coast led to construction of a unique geomorphosite with the characteristic barchan and linear sand dunes. Due to the high threshold velocity that reached at Baltim (Vt) 19.38 cm sec, such velocity is able to blow sands with diameter D50 of 250 m. The velocity need for suspending the D50 to an elevation Z (Vz=5m) is equal to 630 cm sec-1. Contrary is the case to the east at Gamasa where the Vt equal to 16.3 cm sec-1 and the Vz for suspending the D50 (180 m at Gamasa) is equal to 560 cm sec . This may explain why the dunes at Baltim are coarser in grain diameter and together withthe tight back desert strip explain the presence of Baltim dunes at elevations more than 20m, while at Gamasa not exceeds 5m. These dunes represent natural defence measures for the barrier beach separating the Burullus Lake from the Mediterranean Sea. Due to human intervention including urban extension and agricultural activities much of these dunes were deteriorated and diminished from 174.8km to 6.4km. The project of extraction and concentration of heavy minerals from sand dunes seem uneconomic. Although the heavy mineral concentration is more than 5%, more than half of the detected minerals is Ilmenite, which is neitherstrategic nor economic mineral. Such project may add new form of hazards. Although the defence measures seem effective in protecting the coast, several rates of erosion and accretion were detected along the studied sectors, and the shoreline does not retain its present position in many areas of the coast since 1984.
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监测沿布鲁鲁斯巴尔提姆,尼罗河三角洲,埃及海岸线的位置变化,和海岸沙丘的规则,作为一个自然防御侵蚀的地质遗迹:遥感应用
对Burullus-Baltim沿海地区的监测表明,该地区是一个脆弱的沿海地区,由1000多年的历史时期从旧塞本尼特海岬侵蚀而来的松散沙组成,在阿斯旺高坝(AHD)建设后得到加强。沿着海岸的海浪、风和沙子的相互作用形成了一个独特的地貌,具有典型的barchan和线状沙丘。由于在Baltim (Vt)达到19.38 cm秒的高阈值速度,该速度能够吹出直径D50为250 m的砂。将D50悬浮到高度Z (Vz=5m)所需的速度等于630厘米秒-1。相反,在Gamasa东部的情况下,Vt等于16.3 cm秒-1,而悬浮D50(在Gamasa 180米)的Vz等于560 cm秒。这也许可以解释为什么巴尔提姆的沙丘颗粒直径更粗,再加上后面紧实的沙漠带,为什么巴尔提姆的沙丘出现在海拔超过20米的地方,而Gamasa的沙丘不超过5米。这些沙丘代表了将布鲁勒斯湖与地中海分开的屏障海滩的自然防御措施。由于城市扩张和农业活动等人类活动的影响,大部分沙丘从174.8km减少到6.4km。从沙丘中提取和浓缩重矿物的项目似乎不经济。重矿浓度虽在5%以上,但检出矿物中半数以上为钛铁矿,既非战略矿物,也非经济矿物。这样的项目可能会增加新的危害形式。虽然防御措施在保护海岸方面似乎是有效的,但沿着所研究的部分发现了一些侵蚀和增生的速度,自1984年以来,海岸的许多地区的海岸线没有保持其目前的位置。
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