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Salt export will greatly exceed salt import, so that with the same drainage fraction a rapid desalinization occurs. After one or two years, the soil salinity is decreased so much, that the salinity of the drainage water has come down to a normal value and a new, favorable, equilibrium is reached.
The southern shoreline of the Persian Gulf is a shallow, low-angle carbonate ramp characterised by an evaporitic supratidal system passing offshore, via a broad carbonate–evaporite intertidal environment, into a carbonate-dominated subtidal system. This is a low-energy setting with a small tidal range (1–2 m) and low wave energy as a result ...
In any doab, khadar land (green) lies next to a river, while bangur land (olive) has greater elevation and lies further from the river. Khādir or Khadar and Bangar, Bāngur or Bhangar (Hindi language: खादर और बांगर, Urdu languageکهادر اور بانگر) are terms used in Hindi, Urdu, Punjabi and Sindhi in the Indo-Gangetic plains of North India and Pakistan to ...
The Thal desert is a subtropical sandy region with severe climatic conditions that are prone to temperature extremes. [17] Approximately 50% of the region sees hyper-arid climatic conditions (annual rainfall less than 200mm) and the remaining half sees semi-arid climatic conditions (annual rainfall between 200mm and 500mm). [18]
This will reduce the average American’s sodium intake to about 2,750 mg per day—still higher than the recommended amount, but a big improvement that could result in large public health benefits.
The Salt Range (Punjabi: سلسلہ کوہ نمک) is a mountain range in the north of Punjab [1] province of Pakistan, deriving its name from its extensive deposits of rock salt. [ 1 ] [ 2 ] The range extends along the south of the Potohar Plateau and the north of the Jhelum River .
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Consequences include corrosion damage, reduced plant growth, erosion due to loss of plant cover and soil structure, and water quality problems due to sedimentation. Salination occurs due to a combination of natural and human-caused processes. Arid conditions favour salt accumulation. This is especially apparent when soil parent material is saline.