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Renuka Lake ecosystem and wetland protection, Lesser Himalaya ...

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other l<strong>and</strong> uses. It even absorbs sediment,chemical nutrients <strong>and</strong> other substances innon-point source run off. Riparian zones areinstrumental in water quality improvementfor both surface <strong>and</strong> water flowing intowater bodies through sub-surface or groundwater flow. The wetl<strong>and</strong> riparian zonesshows a particularly high rate of removal ofnitrate entering a stream <strong>and</strong> thus has aplace in eutrophication management.Because of there prominent role insupporting a diversity of species, riparianzones wetl<strong>and</strong> are often the subject ofnational <strong>protection</strong> in a Biodiversity ActionPlan.<strong>Renuka</strong> <strong>Lake</strong> having a riparian course<strong>and</strong> a wetl<strong>and</strong> shows water quality control,soil conservation, their biodiversity <strong>and</strong>influence on aquatic <strong>ecosystem</strong>. Toestablish these characters a comprehensivestudy of water quality, lake <strong>and</strong> wetl<strong>and</strong>sediment geochemistry, isotope chemistryto determine rate of sedimentation, <strong>and</strong>survey of flora <strong>and</strong> fauna distribution havebeen carried out. The lake is unique inlesser <strong>Himalaya</strong> <strong>and</strong> is under RamsarConvention Environment Act.2. MethodologyThe water samples were collected in prewashed1L polythelene bottles filling it tothe capacity. Within 5-6 hours of collectionpH, E.C, D.O, TDS etc. were measuredusing portable field kit. The samples werefiltered using 0.45 µm Millipore filtermembranes. A part of this was used formeasurement of carbonate <strong>and</strong> bi-carbonateby acid titration, choride by AgNO 3titration, sulphate by Ba(ClO 4 ) 2 titrationafter passing the samples through cationexchange resin, phosphate by an ascorbicacid spectrophotometry, silicate bymolybdenum blue spectrometry. Na, K byflame photometer <strong>and</strong> Ca <strong>and</strong> Mg by AAS2100(Perkin Elmer Atomic AbsorptionSpectrophotometer).The sediment samples carefully selectedwere collected from lake <strong>and</strong> wetl<strong>and</strong>, dried<strong>and</strong> processed. The samples were ground to-200 mesh size in agate mortar <strong>and</strong> wereused for making pellets. These pellets weresubjected to X-ray fluorescencespectrophotometer (energy dispersive,Phillips EXAM-6 system) <strong>and</strong> major <strong>and</strong>trace elements were estimated. Theaccuracy was checked by running USGSsediment st<strong>and</strong>ards SDO1, SCO1, GSD9<strong>and</strong> SO1. The major element accuracy is~2.5%. The REE’s were measured on ICP-MS using G2 <strong>and</strong> SDO1 st<strong>and</strong>ards in theUniversity of Kiel, Germany. As the REE.sare present in minor quantities in the matrixelements, therefore, elements have to beseparated as a group so that the spectralinterference from the matrix elements canbe avoided. The precision of data is betterthan 5% except for Ce <strong>and</strong> Nd, which haveprecision of about 10% <strong>and</strong> for REE(

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