Open AccessCharacteristics of Flood Water Level Based on Hydrologic Soil Group Analysis in Temef Watershed
Author(s) -
Davianto Frangky B. Welkis,
Ferry Moun,
Iki Lobo,
Denik Sri Krisnayanti
Publication year - 2020
Publication title -
iop conference series. earth and environmental science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.179
H-Index - 26
eISSN - 1755-1307
pISSN - 1755-1315
DOI - 10.1088/1755-1315/437/1/012005
Subject(s) - watershed , hydrogeology , surface runoff , hydrology (agriculture) , geology , flood myth , alluvium , permeability (electromagnetism) , time of concentration , drainage basin , environmental science , geomorphology , geotechnical engineering , geography , ecology , genetics , cartography , archaeology , machine learning , membrane , computer science , biology
Temef Watershed is located in the Benanain River Basin with a catchment area of 551.50 km 2 . River characteristics in the Temef Watershed are influenced by three main river streams from upstream to downstream. Conventional collection of data on watershed characteristics requires a relatively long process and time. However, when based on Geographic Information Systems (GIS), the cost and time will be more efficient. The floodwater level is affected by the amount of rainwater runoff that occurs in the Temef Watershed. The amount of runoff depends on the level of soil permeability and land cover. To determine the level of soil permeability, hydrogeological maps are used. Based on this, a study of the characteristics of flood waters from GIS-based hydrogeology is needed. The analysis method used ArcGIS overlay on hydrogeological maps, while data on watershed characteristics used the Archydro and HEC-GeoHMS features. The results of the analysis showed a level 3 permeability type with limestone lithology, solid volcanic breccia, sandy marlene, conglomerate, and alluvium consisting of sand and gravel having moderate to high permeability. The metamorphic and basalt rocks have low to moderate permeability and the scaly clay has low to very low permeability. This condition causes runoff that turn into flood streams.