SOIL ATLAS OF ASIA
2ND EDITORIAL BOARD MEETING
RURAL DEVELOPMENT ADMINISTRATION, NATIONAL INSTITUTE OF AGRICULTURAL SCIENCES,
JEONJU, REPUBLIC OF KOREA | 29 APRIL – 3 MAY 2019
Markus Anda (Indonesia)
Land Use Changes on Soil Carbon Dynamics, Stocks in Eastern Himalayas, IndiaExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Parmar Brajendra, from Indian Institute of Rice Research - India, in FAO Hq, Rome
Effects of land use/cover on soil aggregate-associated organic carbon in a mo...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Tshering Dorji, from Ministry of Agriculture and Forest - Bhutan, in FAO Hq, Rome
Calculating changes in soil carbon in Japanese agricultural land by IPCC-tier...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 1, Monitoring, mapping, measuring, reporting and verification (MRV) of SOC, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Yasushito Shirato, from Institute for Agro-Environmental Sciences - Japan, in FAO Hq, Rome
Status of Soil Organic Carbon Stocks in the Small Island Developing States (S...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 1, Monitoring, mapping, measuring, reporting and verification (MRV) of SOC, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Siosiua Halavatu, from Secretariat of Pacific States - Fiji, in FAO Hq, Rome
Soil management strategies to enhance carbon sequestration potential of degra...koushalya T.N
Reclamation of degraded lands has huge potential for carbon (C) sequestration to counteract the climate change. It was estimated that about 1,964 Mha of land is degraded worldwide and in India 146.8 Mha of land is degraded ( Bai et al., 2008). The major land-degradation processes in the World and in Asia are water erosion, wind erosion, salinity, alkalinity, nutrient depletion and metal pollution. Enrichment of soil organic carbon (SOC) stocks through sequestration of atmospheric CO2 in agricultural soils and degraded lands is important because of its impacts on improving soil quality and agronomic production, and also for adaptation to mitigation of climate change. Various management strategies like conservation agriculture, integrated nutrient management, afforestation, alternate land use, plantations and amendments and use of biochar hold promise for long-term C sequestration. It can be concluded that land degradation is a serious problem in India which need to be tackled because shrinking of land resource base will lead to a substantial decline in food grain production which in turn would hamper the economic growth rate and there would also be unprecedented increase in mortality rate owing to hunger and malnutrition.
Soil survey is the study and mapping of soils in their natural environment.
It is to enables, more numerous, more accurate, more useful prediction of soil for specific purpose
It is starting point of all soil research. .
Land Use Changes on Soil Carbon Dynamics, Stocks in Eastern Himalayas, IndiaExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Parmar Brajendra, from Indian Institute of Rice Research - India, in FAO Hq, Rome
Effects of land use/cover on soil aggregate-associated organic carbon in a mo...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Tshering Dorji, from Ministry of Agriculture and Forest - Bhutan, in FAO Hq, Rome
Calculating changes in soil carbon in Japanese agricultural land by IPCC-tier...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 1, Monitoring, mapping, measuring, reporting and verification (MRV) of SOC, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Yasushito Shirato, from Institute for Agro-Environmental Sciences - Japan, in FAO Hq, Rome
Status of Soil Organic Carbon Stocks in the Small Island Developing States (S...ExternalEvents
This presentation was presented during the 2 Parallel session on Theme 1, Monitoring, mapping, measuring, reporting and verification (MRV) of SOC, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Siosiua Halavatu, from Secretariat of Pacific States - Fiji, in FAO Hq, Rome
Soil management strategies to enhance carbon sequestration potential of degra...koushalya T.N
Reclamation of degraded lands has huge potential for carbon (C) sequestration to counteract the climate change. It was estimated that about 1,964 Mha of land is degraded worldwide and in India 146.8 Mha of land is degraded ( Bai et al., 2008). The major land-degradation processes in the World and in Asia are water erosion, wind erosion, salinity, alkalinity, nutrient depletion and metal pollution. Enrichment of soil organic carbon (SOC) stocks through sequestration of atmospheric CO2 in agricultural soils and degraded lands is important because of its impacts on improving soil quality and agronomic production, and also for adaptation to mitigation of climate change. Various management strategies like conservation agriculture, integrated nutrient management, afforestation, alternate land use, plantations and amendments and use of biochar hold promise for long-term C sequestration. It can be concluded that land degradation is a serious problem in India which need to be tackled because shrinking of land resource base will lead to a substantial decline in food grain production which in turn would hamper the economic growth rate and there would also be unprecedented increase in mortality rate owing to hunger and malnutrition.
Soil survey is the study and mapping of soils in their natural environment.
It is to enables, more numerous, more accurate, more useful prediction of soil for specific purpose
It is starting point of all soil research. .
Dr. Jim Camberato - Nitrogen Management: We Aren't There YetJohn Blue
Nitrogen Management: We Aren't There Yet - Dr. Jim Camberato, Purdue University, from the 2020 Conservation Tillage and Technology Conference, held March 3-4, 2020, Ada, OH, USA.
Assessing the potential of soil organic carbon sequestration in African soilsExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Ms. Tantely Razafimbelo, from University of Antananarivo and CASA - Madagascar, in FAO Hq, Rome
Assessment of Spatial and Temporal Variations of Soil Salinity using Remote S...Hamdi Zurqani
“The aim of this paper is to identify the change in saline soils (Sebkha) using Remote Sensing (RS) and geographic information system (GIS) techniques”.
Soil Organic Carbon stabilization in compost amended soilsExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Riccardo Spaccini, from Universitá di Napoli Federico II - Italy, in FAO Hq, Rome
Development and rainfed paddy soils potency derived from lacustrine material ...NurdinUng
Rainfed paddy soils that are derived from lacustrine and include of E4 agroclimatic zone have many unique properties and potentially for paddy and corn plantations. This sreseach was aimed to: (1) study the soil development of
rainfed paddy soils derived from lacustrine and (2) evaluate rainfed paddy soils potency for paddy and corn in Paguyaman. Soil samples were taken from three profiles according to toposequent, and they were analyzed in laboratory. Data were analyzed with descriptive-quantitative analysis. Furthermore, assessment on rainfed paddy soils potency was conducted with land suitability analysis using parametric approach. Results indicate that all pedon had evolved with B horizons structurization. However, pedon located on the summit slope was more developed and intensely weathered than those of the shoulder and foot slopes.The main pedogenesis in all pedons were through
elluviation, illuviation, lessivage, pedoturbation, and gleization processes. The main factors of pedogenesis were climate, age (time) and topography factors. Therefore, P1 pedons are classified as Ustic Endoaquerts, fine, smectitic,
isohypertermic; P2 as Vertic Endoaquepts, fine, smectitic, isohypertermic; and P3 as Vertic Epiaquepts, fine, smectitic,
isohypertermic. Based on the potentials of the land, the highest of land suitability class (LSC) of land utilization type (LUT) local paddy was highly suitable (S1), while the lowest one was not suitable with nutrient availability as the limiting factor (Nna). The highest LCS of paddy-corn LUT was marginally suitable with water availability as the limiting factor (S3wa), while the lower LSC was not suitable with nutrient availabily as the limiting factor (Nna).
Dr. Jim Camberato - Nitrogen Management: We Aren't There YetJohn Blue
Nitrogen Management: We Aren't There Yet - Dr. Jim Camberato, Purdue University, from the 2020 Conservation Tillage and Technology Conference, held March 3-4, 2020, Ada, OH, USA.
Assessing the potential of soil organic carbon sequestration in African soilsExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Ms. Tantely Razafimbelo, from University of Antananarivo and CASA - Madagascar, in FAO Hq, Rome
Assessment of Spatial and Temporal Variations of Soil Salinity using Remote S...Hamdi Zurqani
“The aim of this paper is to identify the change in saline soils (Sebkha) using Remote Sensing (RS) and geographic information system (GIS) techniques”.
Soil Organic Carbon stabilization in compost amended soilsExternalEvents
This presentation was presented during the 2 Parallel session on Theme 2, Maintaining and/or increasing SOC stocks for climate change mitigation and adaptation and Land Degradation Neutrality, of the Global Symposium on Soil Organic Carbon that took place in Rome 21-23 March 2017. The presentation was made by Mr. Riccardo Spaccini, from Universitá di Napoli Federico II - Italy, in FAO Hq, Rome
Development and rainfed paddy soils potency derived from lacustrine material ...NurdinUng
Rainfed paddy soils that are derived from lacustrine and include of E4 agroclimatic zone have many unique properties and potentially for paddy and corn plantations. This sreseach was aimed to: (1) study the soil development of
rainfed paddy soils derived from lacustrine and (2) evaluate rainfed paddy soils potency for paddy and corn in Paguyaman. Soil samples were taken from three profiles according to toposequent, and they were analyzed in laboratory. Data were analyzed with descriptive-quantitative analysis. Furthermore, assessment on rainfed paddy soils potency was conducted with land suitability analysis using parametric approach. Results indicate that all pedon had evolved with B horizons structurization. However, pedon located on the summit slope was more developed and intensely weathered than those of the shoulder and foot slopes.The main pedogenesis in all pedons were through
elluviation, illuviation, lessivage, pedoturbation, and gleization processes. The main factors of pedogenesis were climate, age (time) and topography factors. Therefore, P1 pedons are classified as Ustic Endoaquerts, fine, smectitic,
isohypertermic; P2 as Vertic Endoaquepts, fine, smectitic, isohypertermic; and P3 as Vertic Epiaquepts, fine, smectitic,
isohypertermic. Based on the potentials of the land, the highest of land suitability class (LSC) of land utilization type (LUT) local paddy was highly suitable (S1), while the lowest one was not suitable with nutrient availability as the limiting factor (Nna). The highest LCS of paddy-corn LUT was marginally suitable with water availability as the limiting factor (S3wa), while the lower LSC was not suitable with nutrient availabily as the limiting factor (Nna).
Chemical and spectroscopy of peat from West and Central Kalimantan, Indonesia...Agriculture Journal IJOEAR
Abstract— Improving peat soil is difficult but not impossible. Managed correctly, peat can be a highly productive medium for agriculture, but drainage and cultivation can lead to irreversible peat shrinkage. Vegetational changes during the restoration of cutover peatlands leave a legacy in terms of the organic matter quality of the newly formed peat. Current efforts to restore peatlands at a large scale therefore require low cost and high throughput techniques to monitor the evolution of organic matter. In this study, we assessed the merits of using Fourier transform infrared (FTIR) spectra to predict the organic matter composition in peat samples in relation with soil peat properties, tends to to be hydrophobic, flammable.
Spatial Analysis of Soil and Water Quality in Tsunami AffectedAreas of Nagapa...IJERA Editor
In India, the natural disasters, especially the Tsunami in 2004 having exposed our unpreparedness, variability, diverse scientific, engineering, financial and also social processes. Vedaranyamtalukof Nagapattinam coastal region of Tamilnadu, India,was severely affected by Tsunami-2004. Due to its unique geological nature and climate conditions, the quality of soil and water resources was subjected to natural and synthetic changes. The recent efforts of prawn culture and saltpan in these areas also affect the natural resources. This study has revealed the present scenario of soil and water resources by analyzing their chemical parameters in the Tsunami affected areas after ten years of Tsunami-2004. For this study, soil samples (less than 30cm depth from land surface) and groundwater samples (from existing hand/bore pumps) were collected in the study area. It was observed from the analysis that the pH of soil was improved well and EC was lowered significantly except few places. Regarding the available N, P, K of soil, N was low, P and Kwere low to medium range. Further thepH,DO, Turbidity, Hardness,Cl and Mgof groundwater were within the permissible limit;EC and TDS were slight to moderate range for irrigation and drinking.The SAR is within the maximum allowable limit which inferred that groundwater can be used for irrigation without any risk.Thisspatial-temporal variability of soil and water parameters were mapped in GIS environment (Surfer ver. 9) and compared with pretsunami-2004 as well as ground truth scenario. Keeping these results, the soil is suitable for agriculture production. The natural flash flood has helped to reduce contamination of soil and water due to Tsunami-2004. However,due to alkaline in nature the quality of groundwater is not fit for drinking in some places but suitable for irrigation. Among the affected villages, Vedaranyam village has worst quality. This study also recommends suitable management strategies for sustainable development.
Soil fertility analysis for rice production in the lowland areas of Diplahan,...Open Access Research Paper
The most important practice that contributes to rice production is nutrient management. However, if the nutrient plant required is insufficient, low production is unavoidable. Thus, this study was carried out to determine the soil fertility status of lowland areas in the municipality of Diplahan. Soil samples from each sampling site were collected in rice farms using a composite random soil sampling moving in a zigzag pattern. A depth of 0- 15cm soil samples were collected from 15 – 30 different places in 1-5 hectares. An air-drying procedure was done before it was carried to the laboratory for final testing. Soil samples were analyzed for pH, organic carbon, organic matter, nitrogen, phosphorous, and potassium following the BSWM (Bureau of Soils and Water Management) procedures. Furthermore, a soil fertility map was outlined through ArcGIS software by plotting local coordinates in Google Map. Results showed that the areas in 10 selected barangays in the municipality have moderate soil acidity, with a pH level that falls below the desirable range of 5.5 – 7.0 but no lower than 4.5. According to the results of the soil organic carbon analysis, all barangays have insufficient SOC. Only four barangays have the optimal soil organic matter content for lowland rice production. The study also revealed that only two (2) barangays receive an adequate amount of nitrogen, while the rest are considered deficient. Phosphorous-rich soils were found in two (2) barangays; the five (5) barangays have a medium content; and the remaining three (3) barangays have a low content. Lastly, no barangay in the municipality obtains an adequate amount of exchangeable potassium ranging from 82-246 ppm. Problem of insufficient nutrient requirements for rice crop production is widespread in the municipality.
Item 8: WRB, World Reference Base for Soil ResoucesExternalEvents
SOIL ATLAS OF ASIA
2ND EDITORIAL BOARD MEETING
RURAL DEVELOPMENT ADMINISTRATION, NATIONAL INSTITUTE OF AGRICULTURAL SCIENCES,
JEONJU, REPUBLIC OF KOREA | 29 APRIL – 3 MAY 2019
Satira Udomsri (Thailand)
SOIL ATLAS OF ASIA
2ND EDITORIAL BOARD MEETING
RURAL DEVELOPMENT ADMINISTRATION, NATIONAL INSTITUTE OF AGRICULTURAL SCIENCES,
JEONJU, REPUBLIC OF KOREA | 29 APRIL – 3 MAY 2019
Shree Prasad Vista (Nepal)
Item 6: International Center for Biosaline AgricultureExternalEvents
SOIL ATLAS OF ASIA
2ND EDITORIAL BOARD MEETING
RURAL DEVELOPMENT ADMINISTRATION, NATIONAL INSTITUTE OF AGRICULTURAL SCIENCES,
JEONJU, REPUBLIC OF KOREA | 29 APRIL – 3 MAY 2019
Item 5: Japanese Soil Map based on World Reference Base for Soil Resources (2...ExternalEvents
SOIL ATLAS OF ASIA
2ND EDITORIAL BOARD MEETING
RURAL DEVELOPMENT ADMINISTRATION, NATIONAL INSTITUTE OF AGRICULTURAL SCIENCES,
JEONJU, REPUBLIC OF KOREA | 29 APRIL – 3 MAY 2019
How to Create Map Views in the Odoo 17 ERPCeline George
The map views are useful for providing a geographical representation of data. They allow users to visualize and analyze the data in a more intuitive manner.
The Art Pastor's Guide to Sabbath | Steve ThomasonSteve Thomason
What is the purpose of the Sabbath Law in the Torah. It is interesting to compare how the context of the law shifts from Exodus to Deuteronomy. Who gets to rest, and why?
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
This is a presentation by Dada Robert in a Your Skill Boost masterclass organised by the Excellence Foundation for South Sudan (EFSS) on Saturday, the 25th and Sunday, the 26th of May 2024.
He discussed the concept of quality improvement, emphasizing its applicability to various aspects of life, including personal, project, and program improvements. He defined quality as doing the right thing at the right time in the right way to achieve the best possible results and discussed the concept of the "gap" between what we know and what we do, and how this gap represents the areas we need to improve. He explained the scientific approach to quality improvement, which involves systematic performance analysis, testing and learning, and implementing change ideas. He also highlighted the importance of client focus and a team approach to quality improvement.
Item 9: Soil mapping to support sustainable agriculture
1. Markus AndaMarkus Anda
INDONESIAN CENTER FOR AGRICULTURAL LAND RESOURCE
RESEARCH AND DEVELOPMENT
INDONESIAN AGENCY FOR AGRICULTURAL RESEARCH AND
DEVELOPMENT
MINISTRY OF AGRICULTURE
2019
Soil mappingSoil mapping to support sustainable agricultureto support sustainable agriculture
ICALRD :
Jl. Tentara Pelajar No. 12, Bogor 16114
Telp. +62 251 8323012
Fax. +62 251 8311256
Email: csar@indosat.net.id
http://bbsdlp.litbang.deptan.go.id
2. Increasing food production and sustainable food self
sufficiency (for 265 million people)
Food security and nutrition
Increasing competitiveness, added value and export
Increase farmer’s income
Optimation of soil productivity, climate change
adaptation and mitigation, and soil conservation
GOALS OF AGRICULTURAL
DEVELOPMENT IN INDONESIA
3. Swampy land
Non-swampy
wetland 9.5 Mha
Upland wet
climate (acid)
104.6 M ha
Upland dry
climate 10.8 M ha
Tidal swampy land 7.6 M ha
Inland swampy land 11.6 M
ha
Peatland 14.9 M ha (1.4 M ha
tide and 13.6 Mha inland)
Tidal swampy land 7.6 M ha
Inland swampy land 11.6 M
ha
Peatland 14.9 M ha (1.4 M ha
tide and 13.6 Mha inland)
Land grouping based on
Agro-ecosystem
(source: soil map 1:250.000
scale)
Upland wet climate
(Non-acid): 20.9 M ha
4. Flowchart of soil map production and its derivative map generation in Indonesia
Base/supporting mapsBase/supporting maps
Topographic mapsTopographic maps
SRTM (DEM)SRTM (DEM)
Geological mapsGeological maps
IMAGEIMAGE
INTERPRETATIONINTERPRETATION
(Landsat, Radar)(Landsat, Radar)
Delineation based on relief,Delineation based on relief,
contour, pattern, texture,contour, pattern, texture,
wetness, color featurewetness, color feature
LAND SUITABILITYLAND SUITABILITY
MAPSMAPS
Image geometricImage geometric
correctionscorrections
LANDFORMLANDFORM
UNITSUNITS
Field observations:
profiles, minipit,
augering , landuse
LAND EVALUATIONLAND EVALUATION
Land useLand use
requirementsrequirements
e.g. SPECIFIC CROPe.g. SPECIFIC CROP
SUITABILITY MAPSUITABILITY MAP
RECOMMENDATIONRECOMMENDATION
MAPSMAPS
Present LandPresent Land
useuse
SPATIALSPATIAL
PLANNINGPLANNING
Land qualities: soil,Land qualities: soil,
climate,climate,
environmentsenvironments
SOIL MAPSSOIL MAPS
9. Soil map sheet of Cigudeg district, Bogor Regency, west Java (scale 1:50.000)
Mapping units legend:
2. Gleisol Distrik (Typic Endoaquept), alluvial plain, clay sediment)
43. Andosol Distrik (Typic Hapludand), deep, well drainage, fine texture, slightly acid,
low CEC, medum BS; old volcanic hill landform, Andesite and basalt
44. Kambisol Oksik (Oxic Dystrudept) old volcanic hill landform, Andesite
48. Kambisol litik (Lithic Dystrudept) and Andosol Distrik (Typic Hapludand), old
volcanic mountain landform, Andesite and basalt
10. Key success: drainage management, raised bed cultivation, ameliorant,Key success: drainage management, raised bed cultivation, ameliorant,
fertilizersfertilizers
Syahbudin and Alwi, 2012
11. Horticultural crop (shallot, Bauji variety) performance on a peat soilHorticultural crop (shallot, Bauji variety) performance on a peat soil
Rice husk biochar + chicken manure (15
t/ha) was able to increase shallot yield 2.5
order of magnitude compared to control
(cow manure) and suppress CO2
emission. Yield of shallot is 6,5 t/ha
(Kalampangan, Central Kalimantan)
Application of NPK 500kg/ha, KCl
200kg/ha fertilizer: shallot yield 9 t/ha
in Landasan ulin, South Kalimantan
Photo: Dr. Eni Mufta
14. Rubber crops in 8 mRubber crops in 8 m
deep peat soils withdeep peat soils with
minimum drainageminimum drainage
(6 years old,(6 years old,
starting tapping)starting tapping)
15. Peat soils used for rubber, rambutan and forest in Tangkit district, Jambi
Rambutan Forest for conservationRubber
16. Oil palm at famer’s farm, shallow waterOil palm at famer’s farm, shallow water
table 60 cm in peat soil, Tanjungtable 60 cm in peat soil, Tanjung
Jabung, JambiJabung, Jambi
17. Sukarman et al,2012
LOKASI
JAMBI :
Desa Arang-arang, Kecamatan Kumpeh Ulu, Kabupaten
Muaro Jambi, Provinsi Jambi.
RIAU
Desa Lubuk Ogong, Kecamatan Bandar Sei Kijang,
Kabupaten Pelalawan, Provinsi Riau.
Kedua lokasi merupakan lokasi Percobaan ICCTF
18. Correlation between CO2 flux and water table
under oil palm plantation
Water table
depth
Y = 0,593e 0,015x
R2
= 0,3764
CO2 flux increases with
increasing water table
depth
Sukarman et al. (2012)
Water table (cm)
19. Relationship between CO2 flux and soil water
content
Soil moisture
content
Y = 41,582e -0,007x
R2
= 0,6002
CO2 flux decreases with
increasing water content
Sukarman et al. (2012)
Soil water content (%)
20. Pengukuran CO2 pada lahan gambut diukur pada bagian serasah dan tanpa serasah
26. UNSUR WMS:
1. Zoning Based on Hydrotopografi
2. Infrastructure Drainage construction Based on Hydrotopografi
3. Water Level Based on Roots of Oil Palm
a. Water Level Monitoring Piezometer
b. Water Level Control Bangunan Air /Overflow
c. Akar Sawit : 1. 0 - 20 cm = 50%
2. 20 - 40 cm = 25%
3. 40 - 60 cm = 25%
4. Monitoring Subsidence
5. Fire Prevention System
C. WATER MANAGEMENT SYSTEM
GAPKI, 2014
27. Thank you for your
kind attention
ICALRD :
Jl. Tentara Pelajar No.12, Bogor 16114
Telp. +62 251 8323012
Fax. +62 251 8311256
Email: csar@indosat.net.id
http://bbsdlp.litbang.deptan.go.id
Sharing the management
of fragile soils promotes
soil use sustainability