KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO

This study focuses on the study of hydrogeomorphology in mapping vulnerability of flooding in Gorontalo City. flooded based on aspect of hydrology and the aspect geomorphology in order to (1) examine the characteristics of potential flood hazards by hydrogeomorphological mapping unit of Gorontalo Ci...

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Main Authors: , Arqam Laya, , Prof. Dr. H. Sudarmadji, M.Eng.Sc.
Format: Thesis
Published: [Yogyakarta] : Universitas Gadjah Mada 2013
Subjects:
ETD
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author , Arqam Laya
, Prof. Dr. H. Sudarmadji, M.Eng.Sc.
author_facet , Arqam Laya
, Prof. Dr. H. Sudarmadji, M.Eng.Sc.
author_sort , Arqam Laya
collection UGM
description This study focuses on the study of hydrogeomorphology in mapping vulnerability of flooding in Gorontalo City. flooded based on aspect of hydrology and the aspect geomorphology in order to (1) examine the characteristics of potential flood hazards by hydrogeomorphological mapping unit of Gorontalo City. (2) assess the vulnerability of flood hydrogeomorphological mapping units and the relationship with the level of vulnerability of hydrogeomorphological. (3) determine the hydrogeomorphological zonation Gorontalo city flooded by the characteristics of the causes of flooding, (4) formulate solutions and Gorontalo City flood control directives. The method used is grid approach, it was to divide the land in Gorontalo City to be 46 grids. Sampling data taking in every grid based on systimatic sampling method, the results can be shown in tabulation/matrix. Data analysis using was to use cross tabulation method, and then it was described. The results of this study shows that: (1) analysis of variance showed that overall the potential flood hazard and hydrogeomorphology variables have a significant influenced. This is demonstrated by the significant value of 0% is less than 1%. Expectation value of the infiltration rate 66.7%, the rainfall rate 66,7%, the drainage 33.3%, the landform 75% and the slope of 66.7%. Soil type not effective, (2) the analysis of the level of vulnerability to hydrogeomorphological variables are very significant. Flood affected area covering 965.828 ha (14.47%), evaluated the rate of infiltration I4 and I5 covering 1744.33 ha. Rainfall causes flooding there are 4 types. Poor drainage conditions (2097.64 Ha). F landforms is 3549.37Ha and D landform area of 3121 Ha. The slope < 7% is 3507.84 Ha (52.6%). Aluvial soil type an area of 3492.31 Ha, (3) mapping of zone of flood hydrogeomorphology in Gorontalo city got five classes of vulnerabilities are: Highly vulnerable (SR = 273.28 Ha), vulnerability (R = 1023.339 Ha), vulnerable enough (CR = 2302,13 Ha), less vulnerable (KR = 168.77 Ha), not vulnerable (TR = 2781.95 Ha). (4) Based on the guidance development polder drainage channels are divided into 3 (three) zoning, namely western zone (1069.826 Ha)
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spelling oai:generic.eprints.org:1241192016-03-04T08:27:07Z https://repository.ugm.ac.id/124119/ KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO , Arqam Laya , Prof. Dr. H. Sudarmadji, M.Eng.Sc. ETD This study focuses on the study of hydrogeomorphology in mapping vulnerability of flooding in Gorontalo City. flooded based on aspect of hydrology and the aspect geomorphology in order to (1) examine the characteristics of potential flood hazards by hydrogeomorphological mapping unit of Gorontalo City. (2) assess the vulnerability of flood hydrogeomorphological mapping units and the relationship with the level of vulnerability of hydrogeomorphological. (3) determine the hydrogeomorphological zonation Gorontalo city flooded by the characteristics of the causes of flooding, (4) formulate solutions and Gorontalo City flood control directives. The method used is grid approach, it was to divide the land in Gorontalo City to be 46 grids. Sampling data taking in every grid based on systimatic sampling method, the results can be shown in tabulation/matrix. Data analysis using was to use cross tabulation method, and then it was described. The results of this study shows that: (1) analysis of variance showed that overall the potential flood hazard and hydrogeomorphology variables have a significant influenced. This is demonstrated by the significant value of 0% is less than 1%. Expectation value of the infiltration rate 66.7%, the rainfall rate 66,7%, the drainage 33.3%, the landform 75% and the slope of 66.7%. Soil type not effective, (2) the analysis of the level of vulnerability to hydrogeomorphological variables are very significant. Flood affected area covering 965.828 ha (14.47%), evaluated the rate of infiltration I4 and I5 covering 1744.33 ha. Rainfall causes flooding there are 4 types. Poor drainage conditions (2097.64 Ha). F landforms is 3549.37Ha and D landform area of 3121 Ha. The slope < 7% is 3507.84 Ha (52.6%). Aluvial soil type an area of 3492.31 Ha, (3) mapping of zone of flood hydrogeomorphology in Gorontalo city got five classes of vulnerabilities are: Highly vulnerable (SR = 273.28 Ha), vulnerability (R = 1023.339 Ha), vulnerable enough (CR = 2302,13 Ha), less vulnerable (KR = 168.77 Ha), not vulnerable (TR = 2781.95 Ha). (4) Based on the guidance development polder drainage channels are divided into 3 (three) zoning, namely western zone (1069.826 Ha) [Yogyakarta] : Universitas Gadjah Mada 2013 Thesis NonPeerReviewed , Arqam Laya and , Prof. Dr. H. Sudarmadji, M.Eng.Sc. (2013) KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=64238
spellingShingle ETD
, Arqam Laya
, Prof. Dr. H. Sudarmadji, M.Eng.Sc.
KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title_full KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title_fullStr KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title_full_unstemmed KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title_short KAJIAN HIDROGEOMORFOLOGI BANJIR DI KOTA GORONTALO
title_sort kajian hidrogeomorfologi banjir di kota gorontalo
topic ETD
work_keys_str_mv AT arqamlaya kajianhidrogeomorfologibanjirdikotagorontalo
AT profdrhsudarmadjimengsc kajianhidrogeomorfologibanjirdikotagorontalo