Characteristics of Khadar Soil
- It belongs to the new category of alluvial soils or new soils.
- It contains fine soil particles.
- It has a pale color.
- This soil is fertile.
- It is found along riverbanks, floodplains, and plains.
- Found at the bottom of a valley that floods every year.
What is Khadar? – Overview, Characteristics, Importance
The lower regions, also known as Nali or Naili, are known as Khadir or Khadar. Khadar soil is mainly found in eastern Uttar Pradesh, Bihar, and West Bengal. When wet, it becomes sticky and retains moisture. The Khadar regions are prone to flooding. Parts of the old riverbed are often accessible to agriculture when the river’s flow changes.
Khadir or Khadar is the lower region, also known as Nali or Naili. The Khadar areas are prone to flooding and often have some parts of the old riverbed made available for farming as the river’s flow changes. It is sticky and retains moisture when wet. The Khadir Formation consists of fresh alluvial soil with a relatively higher content of new river alluvium, which is replenished with each flood cycle and is fertile. To the north of Haryana, which is a vast expanse of lush grassland between the Ghaggar River and the southern limit of the Saraswati Canal Depression, Khadir is also known as Nali. According to the Khadar map, these areas are flooded during rains.
Table of Content
- Khadar
- Characteristics of Khadar Soil
- Significance of Khadar
- Khadar and Bhangar
- Difference Between Khadar and Bangur