Jalvigyan Sameeksha: Recent submissions

  • Bhatia, K. K. S.; Chandra, Satish (National Institute of Hydrology, 1991-12)
    Water erosion is the most widely spread degradation process on the earth through which not only the fertility of soil greatly decreases but, in many cases, the soil is physically destroyed and disappears. Although the ...
  • Shangle, A. K. (National Institute of Hydrology, 1991-12)
    Sedimentation of reservoirs is a matter of vital concern to all water resources development project. In this paper various techniques like HYDAC system, Remote Sensing technique and conventional methods used for conducting ...
  • National Institute of Hydrology (National Institute of Hydrology, 1991-12)
  • National Institute of Hydrology (National Institute of Hydrology, 1991-12)
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • Raju, T. S. (National Institute of Hydrology, 1991-06)
    Soil moisture and soil physical studies are useful in evaluating the groundwater resources for estimation of actual evapotranspirational losses & specific yield of the shallow aquifer zone, to quantify the soil moisture ...
  • Sinha, Asha; Mishra, G. C. (National Institute of Hydrology, 1991-06)
    There has been some attempt to predict rainfall recharge by statistical method using only point rainfall data and water table fluctuation disregarding the fact that water table fluctuation may be result of recharge from ...
  • Ahluwalia, M. S.; Chandra, Subhash; Kapoor, P. N.; Singh, S. R. (National Institute of Hydrology, 1991-06)
    A distributed mathematical model to simulate the overland flow from fallow upland phase of the small watershed subjected to rainfall conditions has been presented. Overland flow has been simulated using St.-Venant equations ...
  • Kashyap, Deepak; Gupta, Sulekha (National Institute of Hydrology, 1991-06)
    The transport of pollutants through the unsaturated zone is governed by Richard's and mass transport equations. Thus, the distribution of pollutant in space and time for given initial and boundary conditions, can be ...
  • Dwivedi, A. K.; Jain, C. K.; Kumar, Bhishm (National Institute of Hydrology, 1991-06)
    With the increasing interest in soil water, demand of its information for planning of the watershed, forecasting of yield in an improved way, irrigation scheduling, partitioning of rainfall into its runoff and infiltration ...
  • Agrawal, D. K.; Bhargava, A. N.; Chabra, S. S. (National Institute of Hydrology, 1991-06)
    The judicious and economic use of water is a matter of national importance while meeting the water requirements for crops. In this context determination of downward movement of soil moisture in unsaturated soil ...
  • Mishra, G. C.; Kumar, C. P. (National Institute of Hydrology, 1991-06)
    A procedure for soil moisture forecast has been described. The implications of boundary conditions during storm up to ponding time and beyond ponding time and during inter storm period have been explained. The numerical ...
  • National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • National Institute of Hydrology (National Institute of Hydrology, 1991-06)
  • Contents 
    National Institute of Hydrology (National Institute of Hydrology, 1989-12)
  • National Institute of Hydrology (National Institute of Hydrology, 1989-12)
  • National Institute of Hydrology (National Institute of Hydrology, 1989-12)

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