| dc.description.abstract | Soil   moisture   studies   provide   potential   information   in  the  field cf agriculture, meteorology  and  hydrology. In  the  field  of  agriculture, Information   on   soil   moisture   is   needed   for   many  diverse  applications Including   improved   yield   forecasting   and   irrigation   scheduling. In meteorology,   the  knowledge  of  soil  moisture  is  required  for  understanding   radiation   components   while   in   the   field   of   hydrology,   the   soil moisture  content   is   important   for  understanding  the  component  of  infiltration   due   to   precipitation   and   irrigation. in   such   processes   of hydrological  balance,   the  moisture  content  of  the  surface  layers  control   upward   and   downward   flow  and   storage   of  water   in  the  unsaturated zone. 
In   this   report,   investigations   on   the   soil   moisture   content   and its   redistribution   along   a   soil   profile   in  the  unsaturated  zone  using neutron  probe  are  presented.	Various  methods   for  in-situ  soil  moisture measurements   are   touched   upon.	Basic   principle,   theory   of   neutronic method,   design   features,   calibration  procedure,   merits  and  limitations of   the   probe-  are   briefly   discussed. Applications   of   neutron   probe for  the  measurement  of  soil  water  storage,   soil  water  reservoir  characteristics  and  recharge  etc.  are  given. 
Studies   carried  out  at  the  campus  of  National  Institute  of  Hydrology   clearly  show   the   capabilities   of   neutron   moisture   probe,   for accurate  measurements  of  soil  moisture  changes,  in-situ,  in undisturbed soil  in  the  natural  state. 
Some  typical   soil  moisture  profiles  were  plotted  showing depletion In   moisture   content   and   water  gained. It   is   seen  that  there  is  not much variation  in  the moisture content below 	120  cm depth.  Soil returned to   an   almost   identical   moisture   level   within   two-three   days   after a   rain   storm.	Evaporation   for   the  period	22nd  April   to	22nd  May  and 22nd   May   to	21st   June	1985  was  estimated  as	5  cm  and	1	.91	cm  respectively. | en_US |