STUDY OF WATER BALANCE AND WATER QUALITY ON HIDROLOGICAL SYSTEM OF BETON SPRING FOR WATER RESOURCE CONSERVATION IN DISTRICT PONJONG, GUNUNGKIDUL REGENCY
Beton Spring is an outlet or resurgence of surface stream hydrological sytem that sinked into swallow holes in karst region. Pentung, Gayam, and Tesih river was predicted as allogenic input of Beton Spring. The Discharge of Beton Spring is relatively large, with conduit stream that tends to turbulen...
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Main Authors: | , |
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Format: | Theses and Dissertations NonPeerReviewed |
Published: |
[Yogyakarta] : Universitas Gadjah Mada
2013
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Subjects: | |
Online Access: | https://repository.ugm.ac.id/123292/ http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63403 |
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Institution: | Universitas Gadjah Mada |
Summary: | Beton Spring is an outlet or resurgence of surface stream hydrological
sytem that sinked into swallow holes in karst region. Pentung, Gayam, and Tesih
river was predicted as allogenic input of Beton Spring. The Discharge of Beton
Spring is relatively large, with conduit stream that tends to turbulence and
perennial. The main function of it�s discharge is for irrigated 1250 hectares wet
rice field within 3 district, and another functions is for fisheries and domestic use.
Residents within recharge area of Beton Spring utilizing stream discharge,
springs, and caves that predicted as the same system as Beton Spring for various
purposes. Limestone mining was commonplace in a karst region, so that
sustainability of Beton Spring discharge and it's water quality are threatened.
\"The Study of Water Balance and Water Quality of Beton spring Hydrological
Systems for Water Resource Conservation within Ponjong District, Gunungkidul
Regency\" aims to 1) determine the indicative catchment area of Beton Spring, 2)
calculate water balance, 3) water quality analyzes for fisheries, and 4) water
resources conservation strategy.
The methods that used in this study were divided into method of sampling
and data collection. Area sampling method was used for landuse checking and
purposive sampling used for the interviews. Morphological analysis using
contour maps for delineation, water balance analysis, matching the suitability of
water quality for fisheries, and the criticality identification of catchment areas to
set the strategies of land and discharge management. The boundary of indicative
catchment area of Beton Spring is entire the rainwater catchment that flowing
into Pentung, Gayam, and Tesih River which is only 1678 hectares. This
Boundary verified with water balance analysis, analysis of geological map, and
field checking.
Beton Spring average discharge is 0,72 m3/sec with effective rainfall (P-
Ep) up to 468 mm, so that the dimension of cathment area is 4841 hectares, wider
than indicative boundary of water catchment. Boundary of Beton spring
catchment area is abreast to 5 allogenic catchment area among Pentung, Gayam,
Tesih, Kedung Paran, Plalar River and autogenic catchment areas. Beton Spring
water quality is suitable for freshwater fish farming with limiting factors of to
468 mm, so that the dimension of cathment area is 4841 hectares, wider than
indicative boundary phosphate and temperatures. Land management focused on
allogenic water catchment and partially autogenic catchment that extent to 3170
hectares (65,5%). 72,4 % of Recharge area condition is in good category to
natural normal, 27,6 % is almost critical and rather critical category.
Qualitatively discharge management is already good because there are sufficient
discharge quantity and good water quality. |
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