Surface Irrigation
Surface irrigation is one of the oldest forms of irrigation and involves the application and distribution of water over the soil surface by gravity. This method is also commonly referred to as flood irrigation due to the way water is applied to the fields. It is considered the most prevalent form of irrigation globally, especially in regions with abundant water supplies and relatively flat topography.
Surface irrigation has been utilized for thousands of years. The Egyptians were among the first to develop this method, notably through the flooding of the Nile. Their innovation of basin irrigation laid the foundation for subsequent irrigation techniques. The Arab Agricultural Revolution further refined these systems during the Islamic Golden Age.
Basin irrigation involves dividing the field into small basins. Water is applied to each basin, and gravity aids in evenly distributing the water. This method is particularly effective for rice cultivation, which requires significant water input.
In furrow irrigation, small channels, or furrows, are created between crop rows. Water flows down these furrows, soaking into the soil. This technique is commonly used for row crops such as corn and cotton.
This method involves dividing the field into long strips separated by levees or borders. Water is directed into the strips and flows down the length of the field. It is an efficient method for many grain crops and pasturelands.
Despite its ancient origins, surface irrigation remains vital in modern agriculture. It is extensively used in countries like India and Nepal, where it supports large-scale agricultural productivity. Modern techniques often combine traditional methods with innovations to improve efficiency and sustainability.
The environmental impact of surface irrigation is significant. It can alter local hydrology, affect groundwater levels, and contribute to soil salinity. However, when managed properly, it can be part of sustainable agricultural practices that mitigate adverse effects.