Upload
others
View
2
Download
0
Embed Size (px)
Citation preview
Organizing Committee
Secretariat
CORECT IJJSS SECRETARIAT
Room 501, 5th Floor, Main Building of FPIK
Brawijaya University, Jl. Veteran, Malang, Indonesia
(+62341) 553512
SUPPORTED BY
PUBLICATIONS PARTNER
Organizing Committees
I Wayan Gede Astawa Karang Assoc.Prof, Dept. of Marine Science and Fisheries, Udayana University, Indonesia
Bambang Semedi Assoc.Prof, Head of CORECT RG, Brawijaya University, Indonesia
Takahiro Osawa Prof, Head of CreSOS, Udayana University, Indonesia
I Wayan Arthana Prof, Dean of Faculty of Marine Science and Fisheries, Udayana University
Happy Nursyam Prof, Dean of Faculty Fisheries and Marine Science, Brawijaya University
Kuan-Tsung Chang Assoc.Prof, Dept. of Civil Engineering and Environmental Informatics, MUST,
Taiwan
Ming-An Lee Prof, Dept of Environmental Biology and Fisheries Science, NTOU, Taiwan
Gde Raka Angga Kartika Secretary, Udayana University
Rarasrum Kasitowati Executive Secretary, Brawijaya University
Pande Gde Sasmita Julyantoro, Ph.D Scienti�c and Program, Udayana University
M. Arif Asadi Scienti�c and Program, Brawijaya University
Gede Hendrawan, Ph.D Scienti�c and Program, Udayana University
Oktiyas Muzaky Luth� Scienti�c and Program, Brawijaya University
Made Ayu Pratiwi Scienti�c and Program, Udayana University
Arief Setyanto Scienti�c and Program, Brawijaya University
Dhira K. Saputra Scienti�c and Program, Brawijaya University
INTERNATIONAL CONFERENCE ON SUSTAINABILITY SCIENCE ANDMANAGEMENT: Advanced Technology in Environmental ResearchC O R E C T- I J J S S C O N F E R E N C E 2 0 1 9
HOME CONFERENCE TOPICS CORECT-IJJSS 2019 REGISTRATION AND PAYMENT ICSSM TRAINING 2 CONFERENCE VENUE PROGRAMME INFO ON BALI
.
International Conference on Sustainability Science and Management (ICSSM) Advanced Technology in Environmental Research
ICSSM 2019 Presentation Schedule | Day-2, 15 November 2019 | Page 2 of 10
DAY 2, 15 November 2019, CEReS Symposium / Environmental Science Themes, ROOM : MARGA 2
No TIME CODE AUTHORS ABSTRACT TITLE
Environment as One of Morphological Adaptation Mechanism
13 14.45 ES - 34 Kus Indriani, Hayati Sari Hasibuan, Misri Gozan
Contribution of the Industrial Sector on the in Water Quality of Ciracab River, Indonesia
14 15.00 EI - 27 Sessario Bayu Mangkara, M Arozaq, S Sunarto
Environmental Planning and Management in Traditional Market (A Study at Market Mayestik (Jakarta), Ibuh Market (Payakumbuh), Pandansari Market (Balikpapan)
15 15.15 MF - 74 M F Fadhil, E Kusratmoko, N S Oktaviani
Flood Vulnerability Mapping Areas Using Spatial Multi-Criteria Evaluatian (SMCE) Method in Minraleng Sub-watershed, Maros Regency.
16 15.30 MF - 28 O Onrizal, M Mansor Succession Pattern of Understory Plant Following Tsunami Catastrophe at Coastal Areas in Aceh, Indonesia
17 15.45 ES - 24 Aninda W Rudiastuti, Ati Rahadiati, Ratna S Dewi, Dewayany Soetrisno, Erwin Maulana
Assesing Coastal Vulnerability Index of Tourism Site: The Case of Mataram Coast
18 16.00 MF - 107 Achmad Fachruddin Syah, Sei-Ichi Saitoh, Irene D. Alabia, Toru Hirawake
Potential impact of global warming on Pacific saury (Cololabis saira) habitat in the western North Pacific
19 16.15 MF - 108.2
Muh. Herjayanto, Muta Ali Khalifa, Novita Rahmayanti, Annisa Misykah Maulidina, Novitasari Irianingrum, Etin Nurkhotimah, Nugroho Agung Prasetyo, Abdul Gani, Fitri Sil Valen, Veryl Hasan
The record of non-native Sailfin Molly Poecilia petenensis Günther, 1866 (Cyprinodontiformes, Poeciliidae) in Tunda Island, Indonesia
13 16.30 ES - 21 S W Utomo, P A Pambudi, A Pramudiatno, Sudaryatno
The Carbon Sequestration Potency of Agarwood (Aquilaria malaccensis Lam.) for Environmental Conservation
14 16.45 ES - 32 Ni Made Trigunasih, Putu Perdana Kusuma Wiguna
Analysis of Land Suitability and Land use Planning for Corn using Geographic Information System (GIS) in Ho Watershed, Tabanan Regency
Analysis of Land Suitability and Land Use Planning for Corn using Geographic Information System (GIS) in Ho Watershed, Tabanan Regency
Ni Made Trigunasih,1 and Putu Perdana Kusuma Wiguna1
1Faculty of Agriculture, Universitas Udayana, Bali, Indonesia
Abstract Corn has an important need for human life and is the second food crop commodity after rice. This study aims to evaluate
the suitability of the use of corn in the Ho River Basin, to know the limiting factors for the suitability of the use of corn land and to determine or provide directions for the use of corn land in the Ho River Basin. This activity consists of a series of activities which include the collection and evaluation of secondary data, surveys, data analysis, and field tests. 3. The actual land suitability for corn in Ho Watershed is classified as non-suitable (N) and marginally suitable (S3) with the limiting factors are slope, erosion hazard, soil drainage and nutrient availability (P-available). Potential land suitability for corn is classified as suitable 2 (S2) to marginally suitable (S3) with limiting factors are temperature slopes, erosion hazards and nutrient availability (P-available).
Ni Made Trigunasih,
Putu Perdana Kusuma Wiguna
Analysis of Land Suitability and
Land Use Planning for Corn using
Geographic Information System
(GIS) in Ho Watershed, Tabanan
Regency
Introduction
Corn is an important food crop for human and is the second food crop commodity after rice.
All parts of the plant can be used for various purposes such as raw materials / processed materials
for cooking oil, corn-starch, ethanol, dextrin, acetone, glycerol, adhesives, textiles and organic acids
for biofuel.
This study aims to evaluate the suitability of the use of corn in the Ho River Basin, to know the limiting
factors for the suitability of the use of corn land and to determine or provide directions for the use of
corn land in the Ho River Basin.
The research location was carried out in the Ho River Basin, Tabanan. Administratively the Ho water-
shed is located in two sub-districts in Tabanan Regency, Bali, Indonesia, namely Kerambitan and
Penebel sub-district. Astronomically, the DAS Ho is located at position 115o 01 '26.3 "- 115o 09' 04.9"
East and 8o 16 '30.2 "-8o 34' 03.7" South.
Methodology
Before physical data collection activities are carried out in the field, detailed
land units are overlayed from slope maps, climate maps, soil type maps and
land use maps using GIS software. Land unit map functions to direct
sampling in the field. Each land unit is sampled proportionally to its area.
Sampling is done by transect in a sloped area and with a grid system in a flat
area. Soil samples are taken in layers at a depth of 0 - 30 cm, whereas to
determine the effective depth is continued up to a depth of 150 cm for soils
classified as deep or until lytic contact in shallow soils.
All data taken from the drilling results are then evaluated in the field, to obtain
representative samples. Each soil sample then analysed in a laboratory to
determine the characteristics of the soil. The characteristics of the soil to be
analysed are Soil texture, Organic C, N- Total, P- available, K- available,
Cation Exchange Capacity (CEC), Base Saturation (KB), soil pH, Soil
permeability, and salinity.
Result and Discussions
Delineation of land units is done through overlapping 4 types of maps, namely land, climate, slope and
land use maps.
Land Unit Analysis
Land Unit
Main material
Physiography Topography Soil Type Slope Landuse
IIntermediaryVolkan Ash
Beach Ridge Flat, Grayish Brown Regosol
0-8 % Agricultural
IIAsh and IntermediaryVolkan Tuff
VolcanicWavy untilhilly
YellowishBrown Latosol
0-8 % Agricultural
IIIAsh and IntermediaryVolkan Tuff
VolcanicWavy untilhilly
YellowishBrown Latosol
8-15 % Agricultural
IVAsh and IntermediaryVolkan Tuff
VolcanicWavy untilhilly
YellowishBrown Latosol
15-25 %
Agricultural
VAsh and IntermediaryVolkan Tuff
VolcanicWavy untilhilly
YellowishBrown Latosol
25-40 %
Agricultural
VIAsh and IntermediaryVolkan Tuff
VolcanicWavy untilhilly
GrayishBrown Andosol
25-40 %
Agricultural
Result and DiscussionsLand Unit Analysis
Land units is mapped through
overlaying 4 types of maps, na
mely land, climate, slope and la
nd use maps
There are six land units and six
samples to be anaysed in the
lab
Result and Discussions
Based on the analysis of soil samples in the Laboratory, it shows that the
physical properties of the soil samples shows that soil texture dominated by a
rather fine texture, medium texture (clay). Drainage conditions range from
rather poor (ABr) to bad (Br). Coarse material, and surface rocks are found in
the the upper stream of the Yeh Ho watershed, which are located in the land
units II and III in Mangesta Village and Penatahan Village of Penebel Sub-
District. Rock outcrops are not found in all irrigated rice fields in the Yeh Ho
River Basin. The slope of the study site ranges from 2% (flat) to> 45%
(Steep). Chemical properties and soil fertility including soil pH ranges from
slightly acidic to neutral, salinity levels range from low to very high, C-organic
ranges from very low to high, soil CEC varies from moderate (21.79 me/
100g) to high (30, 59 me/ 100g), base saturation ranges from moderate
(46.15%) to very high (107.21%). N-total is classified as low (0.18%) to
moderate (0.35%), P-available is classified as very low (0.56 ppm), to high
(10.03 ppm); and K-available is high (120.58 mg / 100g) very high (334.08
mg / 100g).
Land Suitability Analysis
Result and Discussions
Based on agro-climate data which includes annual mean temperature, rainfall from the Meteorology Climatology and Geophysics Agency of the Central Tabanan Region. Average annual temperatures range from 21.5-28.9 0C, humidity ranges from 58-82%, and annual average rainfall ranges from 1000 mm - 2000 mm. Based on Bali's geological map data, the Yeh Ho watershed has soil types that are dominated by Yellowish Brown Latosol soil type, then followed by Regosol Brown Gray and Andosol Brown Gray soils.
The landform of Ho watershed is dominated by the form of a undulating to hilly sloping area, then followed by hilly to mountainous region in the upstream area of the Ho watershed, as well as the flat area form in the downstream area of the Ho River watershed.
Result and DiscussionsThe actual land suitability for corn is classified as non-suitable (N) and marginally suitable (S3) with the limiting factors are slope, erosion hazard, soil drainage and nutrient availability (P-available). Potential land suitability for corn is classified as suitable 2 (S2) to marginally suitable (S3) with limiting factor is temperature that is higher than required, especially for Berabanand Tangguntiti areas with limiting factors are slopes, erosion hazards and nutrient availability (P-available). The suitability of potential land for corn is quite suitable 2 (S2) and marginally suitable (S3) with limiting factors in temperature, slope and erosion hazard. Several efforts to improve the existing limiting factors are improvement of drainage, addition of P-fertilizer, terracing treatment for erosion prevention.
Landunit Location (Village)
Land Suitability for CornActual Limiting
FactorPotential Limiting
Factor1 Beraban S3eh2,oa,na2 Erosion hazard,
drainage, P-available
S2 tc Temperature
2 Tangguntiti S3oa,na2 Drainage,P-available
S2tc Temperature
3 Mengesta S3 eh1,2; na2 Slope, Erosion hazard, P-available
S2eh1,2 Slope, Erosion hazard
4 Penatahan S3eh1,2 Slope, Erosion hazard
S2 eh1,2 Slope, Erosion hazard
5 Wangaya Gede
Neh1 Slope S3eh1,2 Slope, Erosion hazard
6 Jatiluwih Neh1 Slope S3eh1,2 Slope, Erosion hazard
Result and Discussions
Conclussions
The actual land suitability for corn in Ho Watershed is classified as non-suitable (N) and margi-
nally suitable (S3) with the limiting factors are slope, erosion hazard, soil drainage and nutrient
availability (P-available). Potential land suitability for corn is classified as suitable 2 (S2) to mar
-ginally suitable (S3) with limiting factors are temperature slopes, erosion hazards and nutrient
availability (P-available).
Several efforts to improve the existing limiting factors are improvement of drainage, addition of
P fertilizer, terracing treatment for erosion prevention.