Tag: climate and season cycle

Soil that has very little capacity to hold water is sandy soil. Sandy soils have low moisture storage. High evaporation and low capacity limit the availability of rainwater for plant use.

Ganganagar (SGNR) is a planned city and the northernmost city of Rajasthan, situated near borders of Rajasthan and Punjab states. The place consists of Alluvium. It consists of alluvial and Aeolian soil as it is flooded by Ghaggar River.

Ganganagar (SGNR) is a planned city and the northern-most city of the Indian state of Rajasthan, situated near borders of Rajasthan and Punjab states. The place consists of Alluvium. It is loose, unconsolidated (not cemented together into a solid rock) soil or sediments, which has been eroded, reshaped by water in some form. It is fertile and supports agriculture. 

Brown soils are found in desert areas of Rajasthan. The colour of soils ranges from greyish brown too yellowish brown. Major areas of these soils are in catchment of Banas River. Brown soils are rich in calcium but it has poor organic matter. As the ground water are saline, soils irrigated with these water have accumulated salts.

Red loam soils of Rajasthan are rich in Iron Oxide. It is a type of soil that develops in a warm, temperate, moist climate. They are usually poor growing soils, low in nutrients and humus and difficult to cultivate because of its low water holding capacity. Red soils are generally derived from crystalline rock. 

As Rajasthan is mostly covered by desert, it has sandy soil to the most extent. Soil that has very less capacity to hold water is sandy soil. Sandy soils have low moisture storage. High evaporation & low capacity limit the availability of rain water for plant use. 

The largest area in Rajasthan is occupied by desert soil, which covers the area west of the Aravallis up to the Pakistan border. The entire area is ill watered and unproductive and characterized with sand dunes, hillocks and rock outcrops. The soils contain about 90 to 95 per cent sand and about 5 to 7 per cent clay.

In arid and semi-arid areas, evaporation is always greater than precipitation. Under such circumstances, two main factors determine the nature and properties of soils. Firstly, there is very little vegetation and the soils lack humus content. Hence the soils are invariably of light colour. Secondly, the excess of evaporation makes soils lime accumulating. Thus they are bound to be pedocal in nature. This is the main reason behind the formation of Pedocal soil in Rajasthan.

Though there is very less fertility in desert soils to support agriculture, the presence of Phosphates and Nitrate components make the desert sands fertile for agricultural crops where water supply is regular.

In Rajasthan, both granite and sandstone give birth to sandy soil. Sandy soils have low moisture storage. High evaporation and low capacity limit the availability of rainwater for plant use. As Rajasthan is mostly covered by desert, it has sandy soil to the most extent.