Sediment characteristics, brine chemistry and evolution of Murayr Sabkha, Arabian (Persian)‎ Gulf, Saudi Arabia

Abstract EN

Murayr Sabkha, on the western coast of the Arabian (Persian) Gulf, Saudi Arabia, is a siliciclastic dominated sabkha, with minor bioclasts and shells derived from the shore area and the surrounding tertiary carbonates.

The sabkha is subdivided into three areas: the vegetated sabkha, the bare sabkha and artificial saline pan.

The vegetated sabkha area surrounds the bare sabkha surface, composed of wind blown sand and reworked gypsum crystals.

This area is far from the present day water table, and is covered with halophytes that increase in density towards the bare sabkha area.

The bare sabkha area is located about one meter below the surface of the vegetated sabkha area.

It is wet most of the time, as the water table is shallow (< 120 cm in depth).

The surface of this area is composed of thin buckling crusts, polygonal tepee ridges, and efflorescent gypsum and / or halite patches.

The saline pan is an artificial excavation near the eastern part of the sabkha and is filled with seepage groundwater.

It is floored with a crust of grass-like gypsum crystals.

Petrographic, mineralogic (by XRD), and field examinations of sediment samples collected from 32 trenches in the sabkha revealed that gypsum is the dominant sulfate mineral recorded in the sabkha.

The gypsum is formed of random lenticular mud-sized and sand-sized crystals at the top 70 cm, and aggregates of lenticular and rosette gravelsized crystals near the water table.

Halite is recorded at / near the sediment surface as efflorescent crust and cement, respectively.

Anhydrite is recorded near the water table, whereas celestite is recorded near the gulf side.

Based on a study of 32 brine samples in Murayr Sabkha, it was found that the groundwater in the sabkha is of chloride type (MgCl2 and CaCl2) of marine origin.

It is recharged mainly from seepage of recent marine water from the gulf side and from marine and meteoric waters reacted with the surrounding carbonates.

It seems that the capillary rise of these waters from the shallow water table to the surface as a consequence of surface evaporation led to deposition of evaporite minerals in the sabkha by the "ascending-brine" mechanism.