Soil Moisture

Soil moisture refers to the amount of water stored in the soil, which is essential for plant growth and agricultural productivity. It is influenced by factors such as rainfall, irrigation, evaporation, and soil type. Sufficient soil moisture helps plants absorb nutrients and maintain their health, while too little can lead to drought stress, affecting crop yields. Conversely, excessive moisture can cause waterlogging, hindering root development and leading to plant rot. Monitoring soil moisture is vital for effective water management in farming and gardening, ensuring that plants receive the right amount of water for optimal growth.