Abstract

Stream flow, nutrient loading, and sediment yield closely reflect land use and management practices in relation to growing seasons in mid-hill watersheds of the central Himalaya. A preliminary study was conducted to determine approximate total water discharge and sediment yields from the Galaundi and Pokhare catchments. Mean discharge and sediment loads during the 2002 rainy season were 2.1 m3?s-1 and 0.9 kg?s-1 for Galaundi Khola and 0.45 m3 s-1 and 0.28 kg?s-1 for Pokhare Khola. Estimates of total annual discharge of water and sediment were, respectively, 27.8 million m3 and 11,400 t (Galaundi) and 6.4 million m3 and 3,500 t (Pokhare). These corresponded to about 71.6% and 60.4% of total rain volumes and soil loss rates of 5.18 t?ha-1 and 5.83 t?ha-1 for Galaundi and Pokhare sub-watersheds, respectively. Good correlations were observed for stream discharge vs. sediment concentration (R2 = 0.83 and 0.94 respectively) and rainfall amount vs. discharge (R2 = 0.94 and 0.96 respectively) for both streams. 
 
 Key words: stream flow, sediment concentration, land use, pre-monsoon, sub-watershed 
 
 Himalayan Journal of Sciences 2(3): 51-54, 2004

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.