摘要：Groundwater is one of the important sources of potable water. The water table fluctuation method was usedto evaluate the annual variations in water level rise and to estimate the groundwater recharge during preinterventions and post interventions phase of Domagor-Pahuj watershed development. The area experiencesan average annual rainfall is 880 mm. The estimates of average annual water table fluctuation and change ingroundwater storage volume of randomly selected thirty wells of pre-interventions and post-interventionsphases of watershed were 3.03 to 4.34 million m3, and 1.52 to 2.18 million m3, respectively. The total annualgroundwater recharge potential estimated for the areas was 1.47 million m3 before intervention and 2.06million m3 after intervention.
