Clay soil possesses a significantly higher specific surface area and a greater density of negatively charged exchange sites compared to sandy or gravelly soils. This structural property allows clay particles to attract, hold, and exchange positively charged ions (cations) effectively, resulting in a high Cation Exchange Capacity (CEC).
552
Why does the presence of sodium ions lead to the dispersion of clay particles in soil?
Clay particles are typically held together by flocculating cations like calcium. Sodium ions have a large hydrated radius and a low charge density, which prevents them from effectively bridging clay particles. Instead, they increase the thickness of the diffuse double layer, causing the particles to repel each other and disperse, which severely degrades soil structure and permeability.
553
In which Indian location can a prominent alluvial fan be observed?
An alluvial fan is a cone-shaped deposit of sediment formed where a high-velocity stream emerges from a narrow mountain canyon onto a flatter plain, causing a sudden decrease in flow velocity. In India, the region near Haridwar is a classic example of an alluvial fan, as it marks the point where the Ganges River exits the Himalayan foothills and enters the Indo-Gangetic plain, depositing significant amounts of sediment.
554
What is the estimated average annual water availability in India, measured in Billion Cubic Meters (BCM)?
The average annual water availability in India is estimated at approximately 1850 Billion Cubic Meters (BCM), representing the aggregate water resources across the country's 20 major river basins. Despite this volume, India faces significant water stress, receiving only about 4% of global rainfall. Consequently, the country ranks 133rd globally in terms of per capita water availability, highlighting the critical need for efficient water management and conservation strategies.
555
What are the primary nutrient components found in Single Super Phosphate (SSP) fertilizer?
Single Super Phosphate (SSP) is a traditional phosphatic fertilizer that provides multiple essential nutrients. It typically contains 16% water-soluble phosphorus (as P2O5), 12% sulfur, and 21% calcium. This combination makes it a valuable fertilizer, especially in sulfur-deficient soils, as it provides both primary and secondary nutrients necessary for plant growth and development.
556
Approximately what percentage of the total global water supply is saline and contained within the oceans?
The vast majority of Earth's water is stored in the oceans as saline water. Scientific estimates generally place this figure at approximately 97.5%. Only a very small fraction of the total global water volume exists as fresh water, which is available for human consumption, agriculture, and industrial use.
557
In which year and location was the first dairy cooperative established?
The first dairy cooperative society in India was established in 1913 at Katra, Allahabad. This initiative marked an early attempt to organize milk producers to improve marketing and processing, laying the groundwork for the later cooperative movements that transformed the Indian dairy sector.
558
What is identified as a primary driver of global biodiversity loss?
Climate change is recognized as a major driver of biodiversity loss, as it alters habitats and forces species to migrate or face extinction. The destruction of ecosystems further exacerbates this issue by reducing nature's capacity to sequester carbon and regulate greenhouse gases. This creates a feedback loop where biodiversity loss accelerates climate change, which in turn leads to further degradation of natural resources and agricultural productivity.
Diatoms are a major group of algae, specifically unicellular photosynthetic organisms characterized by unique cell walls made of silica. They are found in various environments, including soil, where they contribute to primary production and soil structure.
560
What is the typical range for the Cation Exchange Capacity (CEC) of organic soils?
Cation Exchange Capacity (CEC) is a measure of a soil's ability to hold and exchange positively charged ions (cations) such as calcium, magnesium, and potassium. Organic matter possesses a high density of negative charges, which significantly contributes to the soil's CEC. Organic soils typically exhibit high CEC values, generally ranging between 50 and 100 meq/100 g, reflecting their high nutrient retention capacity.