Munch (1930) proposed the pressure flow hypothesis which best explain the transport of organic nutrients from the source (supply) to sink (utilisation site). According to this theory, source shows a high osmotic concentration than the sink. When the organic substances from mesophyll cells are (act as source) passed to the sieve tube of phloem through their companion cell by active transport, a high osmotic concentration is developed in sieve tube and acts as a source. Water is absorbed by sieve tubes from the adjacent xylem and develop a high turgor pressure. Thus, the transpiration of organic nutrient takes place from a region of higher turgor region to the area of lower turgor pressure