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Biodrainage may be defined as “pumping of excess soil water using bio-energy through deep-rooted vegetation with high rate of transpiration.”The biodrainage system consists of fast growing tree species, which absorb water from the capillary fringe located above the ground water table. The absorbed water is translocated to different parts of plants and finally more than 98% of the absorbed water is transpired into the atmosphere mainly through the stomata. This combined process of absorption, translocation and transpiration of excess ground water into the atmosphere by the deep rooted vegetation conceptualizes bio-drainage. Fast growing Eucalyptus species like known for luxurious water consumption under excess soil moisture condition are suitable for biodrainage. These species can be planted in blocks in the form of farm forestry or along the field boundary in the form of agroforestry. Other suitable species for block plantations are Casuarina glauca, Terminalia arjuna, Pongamia pinnata and Syzygium cuminii etc. Experiments were conducted in Haryana state. Plantations were raised in water logged areas of Haryana state. To measure the ground water table observation wells were installed in between the tree plantations. Corbon content of oven dried timber, fuel wood, twings/leaves and roots samples were determined by dichromate oxidation method. The transpiration rate was measured using dissipation probes. The basic dissipation probe has two thermocouple needles inserted in the sapwood, the upper one containing an electric heater. The probe needles measure the temperature difference (dT) between the heated needle and the sapwood ambient temperature below. The dT variable and the maximum dTm at zero flow provide a direct conversion to sap velocity. Girth of all trees was measured at the breast height with the help of a measuring tape. Four parallel strip plantations worked as bio-pumps and lowered the water table by 0.85 m in 3 years in canal-irrigated, agricultural, waterlogged fields located in a semi-arid region with alluvial sandy-loam soil. The annual rate of transpiration by these plantations was 268 mm against the mean annual rainfall of 212 mm. Lowering of water table and associated improvement by Eucalyptus plantations increased by 3.4 times than the adjacent fields. There was no net increase in ground water table salinity underneath the plantation. The fluctuations in g.w.t. caused fluctuations in g.w.t. salinity underneath the plantation as well as in the adjacent fields. Tree species vary in their “biodrainage potential” as evidenced by the extent of lowering of water table immediately beneath the plantations. Eucalyptus species has a higher biodrainage potential as compared to relatively slow biodariners like T. Aphylla and P.pinnata.
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