Abstract

In arid countries such as Saudi Arabia, aeolian sand often covers a large area of the country. Understanding the variations of sand properties in dunes, including grain size, sorting, mineral composition and water content, can be important for groundwater recharge, environmental, and construction applications. Earlier studies examined properties of sand dunes by collecting samples from the surface. This study aims to investigate variations of sand properties within a Barchan sand dune in the coastal area of Saudi Arabia, by collecting samples and measurements from two vertically drilled boreholes up to the ground water level; one drilled in the dune crest and another one in the limb. Representative samples were collected and analyzed for their texture parameters, water content, and mineralogy. Electrical resistivity survey data was also acquired to map water content variation in the dune limb, and for comparison with well bore data. The reported results show no vertical variations in grain size or sorting in the dune crest. In contrast, the upper 0.5 m of the dune limb shows a relatively poorer sorting than found in deeper parts of the dune. Laterally, no variations in minerology were observed between crest and limb sands while grain size tended to be slightly coarser in the dune limb compared to the crest. Regarding the water content, it was found to vary vertically, probably due to previous cycles of rainfall infiltration through the sand body. Such observed variation in water content is consistent with the measured resistivity profile which could clearly identify the water table and areas with higher water content. This study concludes that beyond the upper 0.5 m, the Barchan sand dune body can be treated as a homogeneous medium in terms of mineralogy and sorting while grain size increases slightly toward the limb side.

Highlights

  • More than one-third of Saudi Arabia is covered by aeolian sand dunes in four large dune fields, namely, Ar Rub’ al Khali, An Nafud, Ad Dahna, and Al Jafurah [1]

  • This study investigated variations of sand properties within a Barchan sand dune in the coastal area in the Eastern Province, Saudi Arabia, by collecting samples and measurements from two vertically drilled boreholes up to the ground water level

  • Our results showed no variation in mineralogy between the two vertical profiles drilled in the crest and limb

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Summary

Introduction

More than one-third of Saudi Arabia is covered by aeolian sand dunes in four large dune fields, namely, Ar Rub’ al Khali, An Nafud, Ad Dahna, and Al Jafurah [1]. The sand dunes that occurred in the coastal area belong to the Al Jafurah dune field, which lies south of the Gulf of Bahrain [1]. The aeolian sand in the Eastern Province was accumulated during the Quaternary Period and originated from the Bitlis–Zagros thrust belt [2]. Its source was the Tigris–Euphrates paleo-river system. Sands were transported by northerly winds (Shamal) during the Pleistocene Period and formed barchanoid dunes due to the consistent high speed of the winds [3,4].

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