Plant Growth Regulators Improve Magnesium Uptake and Berry Quality in Shine-Muscat Grapes
In 2025, a groundbreaking study published in the Journal of Plant Growth Regulation revealed a powerful solution to a common…
Soil Science
Soil science is an interdisciplinary field that combines biology, chemistry, physics, and environmental science to study soil properties and processes. It examines how soil interacts with plants, water, and the atmosphere, and how these interactions influence crop growth, water filtration, and carbon storage.
Global Demand For Subtropical Crops Worsens Mediterranean Soil Erosion As Farms Expand Into Fragile Lands
The Mediterranean region, known for its rich agricultural heritage, now faces an unprecedented environmental challenge. As global demand for high-value…
New Machine Learning Models And Biochar Can Prevent Water Phosphorus Pollution
Phosphorus is a vital nutrient for crops, but its excessive use in farming has created a serious environmental problem. When…
Integrating Multidisciplinary Approach to Enhancing Heavy Metal Tolerance in Plants
Heavy metal (HM) contamination in agricultural soils has emerged as a pressing global challenge, threatening crop productivity, ecosystem balance, and…
Cover Crops Influence Phosphorus and Metal Leaching in Broiler Litter Soils
Agricultural practices have long been a subject of scrutiny due to their environmental impacts, particularly concerning nutrient and metal leaching…
Transcriptome Analysis Reveals Cotton’s Genetic Response to Sodium Sulfate Stress
Soil salinity is a major environmental challenge that affects crop production worldwide. High salt levels in the soil can harm…
Exogenous Melatonin Can Be Game-Changer for Salt Tolerance in Cotton Plants
In the face of escalating environmental challenges, soil salinization has emerged as a significant threat to agricultural productivity. As the…
Clayey Soil
Clayey soil is a type of soil that is commonly found in various parts of the world, particularly in areas with a humid climate.
Colluvial Soil
Colluvial soil forms through the process of gravity-driven soil movement down a slope and accumulates at the base of hills or mountains.
Soil pH
Soil pH is a measure of acidity or basicity of a soil. It is defined as negative logarithm of hydrogen ion concentration in a soil solution.