The Impact of Climatic Characteristics on Increasing Soil Salinity in Manathira District Center
Samer H. Kadhim Al-JashaamiFaculty of Physical Planning, Urban Planning Department, University of Kufa, Najaf, Iraq. samer.khidhr@uokufa.edu.iq0009-0002-2090-7614
Safaa M. AlmudhafarDepartment of Geography, Faculty of Arts, University of Kufa, Najaf, Iraq. safaa.almudhafar@uokufa.edu.iq0000-0002-0425-2868
Basim A. AlmayahiDepartment of Physics, Faculty of Science, University of Kufa, Najaf, Iraq. basim.almayahi@uokufa.edu.iq0000-0001-7052-8060
Keywords: Properties, high temperatures, the soil of the area, environmental impacts, salt concentrations
Abstract
The climate plays a crucial role in shaping soil characteristics. High temperatures during summer can lead to increased evaporation of soil moisture, resulting in drier and more fragmented soils. This process often leads to higher salt concentrations, altering the soil's properties. In the study area, the soil is categorized into four types: river shoulder soil, river basin soil, riverine island soil, and desert gypsum soil. These soil types are significantly influenced by environmental factors, both natural and anthropogenic. Soil, being a fundamental component of the environment that supports life, is essential for the survival of humans, plants, and animals. In the Najaf Governorate, the soil is vital for agriculture, supporting the growth of various important crops, including vegetables and fruits. However, the soil's natural and human-induced changes have led to a noticeable deterioration in its quality, rendering much of the land unsuitable for agriculture due to high concentrations of saline elements. The natural factors impacting the soil in the study area include climate, soil properties, and water resources, while human activities have further exacerbated these effects. As a result, the soil, particularly in cultivated and uncultivated basins, has seen a rise in the levels of total dissolved salts, sodium, magnesium, calcium, potassium, sulfate, and chloride, often exceeding global standards. In contrast, the soils of river shoulders have remained within acceptable limits.