Acceleration of cavity washout process in rock salt deposits for creating underground storage facilities

1999 ◽  
Vol 35 (1) ◽  
pp. 77-83
Author(s):  
A. V. Mikhalyuk ◽  
V. V. Zakharov ◽  
P. A. Parshukov
Keyword(s):  
Rock Salt ◽  
Underground Storage ◽  
Salt Deposits ◽  
Storage Facilities

VI.—The Salt Deposits of Dax and the Pyrenees

1904 ◽  
Vol 1 (6) ◽  
pp. 265-272
Author(s):  
P. W. Stuart-Menteath
Keyword(s):  
Rock Salt ◽  
Mineral Water ◽  
Igneous Rocks ◽  
Thermal Springs ◽  
Salt Formation ◽  
The South ◽  
North West ◽  
The North ◽  
South West ◽  
Salt Deposits

On the rail to Biarritz the roots of the Pyrenees first appear at Dax, and are accompanied by those ophites and thermal springs which are special features of the entire chain. Vast deposits of salt, to whose first development I contributed, have added an important industry to the resources of this ancient capital of Aquœ Tarbelliœ, where the exact harness depicted on Roman medals is still characteristic of every cart. Beneath the existing ditch of the Roman fortifications rock-salt was accidentally discovered by a boring for mineral water, and the salt is now worked at three miles to the south-east, and is indicated by springs for a distance of seven miles. The deposit is known to be about 100 feet in thickness, but is of unknown depth beneath the existing borings.Along the entire outskirts of both sides of the Pyrenees similar salt deposits abound, and they are often similarly accompanied by igneous rocks.The salt formation of Dax is distinctly limited by the valley of the Adour, which here ceases to wander among the sands of the plain, and is suddenly and sharply diverted along a tectonic depression, running towards the Pyrenees in a south-west direction. Precisely parallel to this course, in the Cretaceous and Tertiary rocks of the Pyrenees, there runs, at a dozen miles to the north-west, the most remarkable example known of a tectonic valley sunk beneath the ocean. The Gouf de Capbreton, sinking with steep sides to over 3,000 feet beneath the even bottom of the Atlantic skirt, and affording evidence of igneous rocks in its surroundings and in the irregularities of its floor, is a perfect analogue of the neighbouring tectonic portion of the Adour.

scholarly journals Properties of Halococcus salifodinae, an Isolate from Permian Rock Salt Deposits, Compared with Halococci from Surface Waters

Life ◽  
2013 ◽  
Vol 3 (1) ◽  
pp. 244-259 ◽  
Author(s):  
Andrea Legat ◽  
Ewald Denner ◽  
Marion Dornmayr-Pfaffenhuemer ◽  
Peter Pfeiffer ◽  
Burkhard Knopf ◽  
...  
Keyword(s):  
Rock Salt ◽  
Surface Waters ◽  
Salt Deposits ◽  
Permian Rock

scholarly journals An Overview of Pakistan Rock Salt Resources and Their Chemical Characterization

2021 ◽  
Vol 64 (2) ◽  
pp. 137-148
Author(s):  
Syed Asim Hussain ◽  
Han Feng-Qing ◽  
Ma Yunqi ◽  
Hawas Khan ◽  
Yang Jian ◽  
...  
Keyword(s):  
Chemical Composition ◽  
Moisture Content ◽  
Rock Salt ◽  
Chemical Characterization ◽  
Annual Production ◽  
Human Consumption ◽  
Natural Form ◽  
Moisture Contents ◽  
Salt Range ◽  
Salt Deposits

Rock salt is of importance for both humans and industries. In this study, we discussed the main salt deposits in Pakistan by evaluating the total reserves as well as the rock salt annual production and by characterizing their chemical composition (Na+, Ca2+, Mg2+, K+, B+, K+, Li+, Cl-, SO42-, Br- and NO3-). Our objectives were to document their impurity, water-insoluble matter and moisture contents to ultimately discuss whether the halite in Pakistan, in its natural form, is safe for human consumption. Pakistan rock salt deposits are located in two distinct regions: the Salt Range area in the Potwar sub-basin with huge Precambrian salt deposits and the Eocene Bahadurkhel/Kohat salts in the Kohat sub-basin. Total reserves are estimated over tens of billion tons with an annual production of about 3,534,075 metric tons in 2017-Results show that the halite of the salt range area is purer than the Bahadurkhel/Kohat salts with purity levels (expressed as NaCl) of 99 and 95 wt. %, respectively. Gypsum represents one of the main impurities in halite for both regions, while potash salts (>9 wt. %) are observed in the Salt Range area, K contents are very low in the Kohat salts. Although the halite moisture content is similar for both regions, impurities contents are higher (>5%) for the Kohat salts, arising the need for their purification prior to eventual human consumption.    

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