Effectiveness of Reducing P Fertilizer and Adding Fish Pond Mud Waste on Growth and Yield of Soybean in Peatland
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Flooding Projections from Elevation and Subsidence Models for Oil Palm Plantations in the Rajang Delta Peatlands, Sarawak, Malaysia
Flooding projections from elevation and subsidence models for oil palm plantations in the Rajang Delta peatlands, Sarawak, Malaysia Flooding projections from elevation and subsidence models for oil palm plantations in the Rajang Delta peatlands, Sarawak, Malaysia Report 1207384 Commissioned by Wetlands International under the project: Sustainable Peatlands for People and Climate funded by Norad May 2015 Flooding projections for the Rajang Delta peatlands, Sarawak Table of Contents 1 Introduction .................................................................................................................... 8 1.1 Land subsidence in peatlands ................................................................................. 8 1.2 Assessing land subsidence and flood risk in tropical peatlands ............................... 8 1.3 This report............................................................................................................. 10 2 The Rajang Delta - peat soils, plantations and subsidence .......................................... 11 2.1 Past assessments of agricultural suitability of peatland in Sarawak ...................... 12 2.2 Current flooding along the Sarawak coast ............................................................. 16 2.3 Land cover developments and status .................................................................... 17 2.4 Subsidence rates in tropical peatlands .................................................................. 23 3 Digitial Terrain Model of the Rajang Delta and coastal -
Acid Discharge from the Tropical Peat Swamp Forest and Its Impact on Local People – a Review
TROPICAL PEATLANDS Acid discharge from the tropical peat swamp forest and its impact on local people – a review Akira Haraguchi 1, Liwat Yulintine 2, Linda Wulandari 2, Tris Liana 2, Sepmiarna Welsiana 3 1 The University of Kitakyushu, Hibikino 1-1, Wakamatsu, Kitakyushu 808-0135, Japan Phone: +81 93 695 3291, Fax: +81 93 695 3383, E-mail: [email protected] 2 The University of Palangkaraya, Palangkaraya, Central Kalimantan, Indonesia 3 Marine and Fishery Department, Katingan Regency, Central Kalimantan, Indonesia Summary After destruction of the peat layer over pyrite-containing sediment, pyrite is oxidized and sulphuric acid is produced. Sulphuric acid contaminates soil and river water and then acidifies the environment. Soil chemical and limnological studies in peat swamp forest in Central Kalimantan showed that sulphuric acid loading from acid sulphate soil occurred widely in the coastal region ranging from the river mouth up to 150 km from the coast. The amount of sulphuric acid discharged to freshwater systems was much higher in the rainy season than in the dry season. By holding interviews with local inhabitants on the source of drinking water for inhabitants in polluted areas this was significantly different between dry and rainy seasons. During the rainy season, river and canal water in polluted areas is not available for drinking, and at this time people avoid using river water for drinking. This paper reviews our limnological and biogeochemical studies on acidification of peat by sulphuric acid, discharging process of sulphuric acid to freshwater system, and impact of sulphuric acid pollution on local inhabitants. Key index words : acid sulphate soil, freshwater ecosystem, peat swamp forest, tropical peat, water resource Distribution of pyrite and its impact on Sulphuric acid discharge from acid peat acidification sulphate soil to freshwater ecosystems Pyrite (FeS 2) is formed in a reducing environment, e.g. -
Questioning Ten Common Assumptions About Peatlands
Questioning ten common assumptions about peatlands University of Leeds Peat Club: K.L. Bacon1, A.J. Baird1, A. Blundell1, M-A. Bourgault1,2, P.J. Chapman1, G. Dargie1, G.P. Dooling1,3, C. Gee1, J. Holden1, T. Kelly1, K.A. McKendrick-Smith1, P.J. Morris1, A. Noble1, S.M. Palmer1, A. Quillet1,3, G.T. Swindles1, E.J. Watson1 and D.M. Young1 1water@leeds, School of Geography, University of Leeds, UK 2current address: Centre GEOTOP, CP 8888, Succ. Centre-Ville, Montréal, Québec, Canada 3current address: Geography, College of Life and Environmental Sciences, University of Exeter, UK _______________________________________________________________________________________ SUMMARY Peatlands have been widely studied in terms of their ecohydrology, carbon dynamics, ecosystem services and palaeoenvironmental archives. However, several assumptions are frequently made about peatlands in the academic literature, practitioner reports and the popular media which are either ambiguous or in some cases incorrect. Here we discuss the following ten common assumptions about peatlands: 1. the northern peatland carbon store will shrink under a warming climate; 2. peatlands are fragile ecosystems; 3. wet peatlands have greater rates of net carbon accumulation; 4. different rules apply to tropical peatlands; 5. peat is a single soil type; 6. peatlands behave like sponges; 7. Sphagnum is the main ‘ecosystem engineer’ in peatlands; 8. a single core provides a representative palaeo-archive from a peatland; 9. water-table reconstructions from peatlands provide direct records of past climate change; and 10. restoration of peatlands results in the re-establishment of their carbon sink function. In each case we consider the evidence supporting the assumption and, where appropriate, identify its shortcomings or ways in which it may be misleading. -
Beje Aquaculture and Inland Fishery in Tropical Peatland of Indonesia
Beje aquaculture and inland fishery in tropical peatland of Indonesia Source Mitigation of Climate Change in Agriculture (MICCA) Programme of FAO Keywords Fisheries, aquaculture, fish production, ponds Country of first practice Indonesia ID and publishing year 8619 and 2016 Sustainable Development Goals No proverty and life below water Summary For many tribes in the tropics (e.g. the between two rivers, and thanks to the soil Kutai and Banjar tribes in East Kalimantan, properties, it forms a kind of water tower Indonesia), fishing in peatland catchments or peat dome (Figure 3), with fully diverse is their main livelihood. Peatlands are their vegetation on the top of it. That is why in the main resources area. They traditionally catch Figure 2, the peatland is higher than the level fishes and reptiles, and collect fuel wood and of the river. In the rainy season it collects grass in peatlands. In January and February, water and in the dry season water is slowly fishes migrate into the waters in the peat released (compare Figure 3). forest for mating and breeding. During this Figure 1. Fishing in a peat swamp forest season fishermen have relatively little catch since most fishes are in the shallow inland waters far inside the peat forest. Fishers using these artificial ponds, called beje, take advantage of fluctuations in the movement of water or overflow of river water during the rainy season from November to March to trap the fish in artificial ponds or special containers. Fish come into the beje by © FAO/TECA themselves since they follow the water flow from the river to the peatland. -
Does Soil Fertility Influence the Vegetation Diversity of a Tropical Peat Swamp
Does soil fertility influence the vegetation diversity of a tropical peat swamp forest in Central Kalimantan, Indonesia? By Leanne Elizabeth Milner Dissertation presented for the Honours degree of BSc Geography Department of Geography University of Leicester 24 th February 2009 Approx number of words (12,000) 1 Contents Page LIST OF FIGURES I LIST OF TABLES II ABSTRACT III ACKNOWLEGEMENTS IV Chapter 1: Introduction 1 1.1 Aim 2 1.2 Objectives 2 1.3 Hypotheses 2 1.4 Scientific Background and Justification 3 1.5 Literature Review 7 1.5.1 Soil Fertility and Vegetation Species Diversity 7 1.5.2 Tropical Peatlands 7 1.5.3 Vegetation and Soil in tropical peatlands 8 1.5.4 Hydrology 14 1.5.5 Phenology and Rainfall 15 Chapter 2 : Methodology 17 2.1 Study Site and Transects 18 2.2 Soil Analysis 21 2.3 Chemical Analysis 22 2.4 Tree Data 25 2.5 Phenology Data 25 2.6 Rainfall Data 26 2.7 Data Analysis 26 2.7.1 Soil Data Analysis 26 2.7.2 Tree Data Analysis 26 2.7.3 Phenology Data Analysis 28 2 2.7.4 Rainfall Data Analysis 28 Chapter 3: Analysis 29 3.1 Tree and Liana Analysis 30 3.1.1 Basal Area and Density 31 3.1.2 Relative Importance Values 33 3.2 Peat Chemistry Analysis 35 3.3 Tree Phenology Analysis 43 3.4 Rainfall Analysis 46 Chapter 4: Discussion 47 4.1 Overall Findings 48 4.2 Peat Chemistry 48 4.3 Vegetation and Phenology 51 4.4 Peat Depth and Gradient 53 4.5 Significance of the Water Table 54 4.6 Limitations and Areas for further Research 56 Chapter 5: Conclusion 59 5.0 Conclusion 60 REFERENCES 62 APPENDICES 67 Appendix A: Soil Nutrient Analysis 68 Appendix B: Regression Outputs 70 Appendix C: Tree Data ON CD Appendix D: Phenology Data ON CD 3 List of Figures Figure 1 – Distribution of tropical peatlands in South East Asia and location of the study area. -
A-414 History of Tropical Peatland in Southeast Asia
15TH INTERNATIONAL PEAT CONGRESS 2016 Abstract No: A-414 HISTORY OF TROPICAL PEATLAND IN SOUTHEAST ASIA Furukawa Hisao Kyoto University, Japan * Corresponding author: [email protected] SUMMARY Geohistory of tropical peatlands in Southeast Asia and a historical retrospect of the exploitation are presented. Keywords: Age, stratigraphy, early and modern ways of exploitation. INTRODUCTION Coastal plains of the Malay Peninsula, Sumatra and Borneo bordering the Sunda Sea were, and still are partly, the realm of swamp forests which included mangrove at seaward outskirts, freshwater swamp forests in the tidal zone, and peat swamp forests inland. Under natural conditions, the ground surface is covered by tropical woody peat layers of varying thickness. These peatlands emerged through the Holocene submersion of the vast and flat terrains at the periphery of the former Sunda Land, and the productive tropical rain forests which expanded over the region. The tropical peatlands inhabited only by mammals, apes, birds and reptiles, remained miasmic for long periods against human interferences because of dense forests, high humidity, numberless mosquitoes, often submerged and bumpy ground surface. Now amidst the worldwide industrialism, they are swiftly changing into one of the important agro-industrial bases, and no one cannot deny that industrialism is a powerful engine to make a people richer and more free. On the other hand, we have seen negative effects of industrialism so often. London was famous for its smog by the mid 20th century. Japan in the 1960s to 1970s was an emporium with so many kinds of environmental pollution and induced diseases. These issues were met, and even now are met through dialogs, scientific studies and legislative measures supported by our own accord. -
Landcover Pattern Analysis of Tropical Peat Swamp Lands in Southeast Asia
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Science, Volume XXXVIII, Part 8, Kyoto Japan 2010 LANDCOVER PATTERN ANALYSIS OF TROPICAL PEAT SWAMP LANDS IN SOUTHEAST ASIA K. YOSHINOa,d, T. ISHIDAb,d, T. NAGANOb,d㧘Y. SETIAWANc a Graduate School of Systems and Information Engineering, University of Tsukuba, Japan, - [email protected] b Faculty of Agriculture, Utsunomiya University, Japan [email protected] b Faculty of Agriculture, Utsunomiya University, Japan [email protected] c Graduate School of Life and Environmental Sciences, University of Tsukuba, Japan, - [email protected] dJST,CREST Commission VIII, WG VIII/8-Land KEY WORDS: Remote Sensing, Land cover, Tropical peat swamp ABSTRACT: Tropical peat swamp lands in the Southeast Asia which store tremendous large amount of carbon in their peat layer and abundant biodiversity are now endangered by human activities such as deforestation, forest fires, land development and urbanization. To earlier start a better environmental policy for conservation of nature of the tropical peat swamp area is one of the preferential global issues. This study aimed at 1) clarifying the state of the tropical peat swamp area in terms of the areas of each land cover categories, and 2) locating the regions where environment have been severely damaged or lands have been extensively developed. Some digital environmental data such as GeoCover, GeoCover LC, SRTM, digital soil maps and so on were analyzed to estimate land cover maps of fine scale around 2000 region by region. As a result of this analysis, following characteristic on the land cover pattern in the Southeast Asia are clarified. -
The Use of Subsidence to Estimate Carbon Loss from Deforested and Drained Tropical Peatlands in Indonesia
Review The Use of Subsidence to Estimate Carbon Loss from Deforested and Drained Tropical Peatlands in Indonesia Gusti Z. Anshari 1,2 , Evi Gusmayanti 1,3 and Nisa Novita 4,* 1 Magister of Environmental Science, Universitas Tanjungpura, Pontianak 78124, Indonesia; [email protected] (G.Z.A.); [email protected] (E.G.) 2 Soil Science Department, Universitas Tanjungpura, Pontianak 78124, Indonesia 3 Agrotechnology Department, Universitas Tanjungpura, Pontianak 78124, Indonesia 4 Yayasan Konservasi Alam Nusantara, DKI Jakarta 12160, Indonesia * Correspondence: [email protected] Abstract: Drainage is a major means of the conversion of tropical peat forests into agriculture. Accordingly, drained peat becomes a large source of carbon. However, the amount of carbon (C) loss from drained peats is not simply measured. The current C loss estimate is usually based on a single proxy of the groundwater table, spatially and temporarily dynamic. The relation between groundwater table and C emission is commonly not linear because of the complex natures of heterotrophic carbon emission. Peatland drainage or lowering groundwater table provides plenty of oxygen into the upper layer of peat above the water table, where microbial activity becomes active. Consequently, lowering the water table escalates subsidence that causes physical changes of organic matter (OM) and carbon emission due to microbial oxidation. This paper reviews peat bulk density (BD), total organic carbon (TOC) content, and subsidence rate of tropical peat forest and drained peat. Data of BD, TOC, and subsidence were derived from published and unpublished sources. We Citation: Anshari, G.Z.; Gusmayanti, found that BD is generally higher in the top surface layer in drained peat than in the undrained peat. -
Beje, Aquaculture and Inland Fishery in Tropical Peatland
Beje, aquaculture and inland fishery in tropical peatland Indonesia Bambang Setiadi1 and Suwido Limin2 1BPPT and (UNPAR); 2BPPT Summary ©FAO/Bambang Setiadi ©FAO/Bambang Schematic representation of Beje cultivation Beje is a traditional fishing method in tropical peat and peat forests, to provide a source of food from traditional fisheries, relying on fluctuations in the movement of water or overflow of river water during the rainy season (November to March) by using a trap in the form of an artificial pond or special tools, allowing fish to breed in the pond and later harvested during the dry season when the water recedes (April to October). The beje system also indirectly play a role in reducing carbon emissions by functioning as a buffer and inhibit the spread of fires in peatlands, keeping peat wet, thus preventing fires in peat. Furthermore, beje also accelerate the development of vegetation. Overall, beje has a role to reduce carbon emissions in peat An overview of the composition of fish species caught in beje, ranging between 5–12 types and dominated by marsh fish (black fish) from the fanily Anabantidae and Nandidae. Other types of fish caught in beje are: Sepat siam (Trichogaster pectoralis), Sepat rawa (Trichogaster trichopterus), Gabus (Channa striata), Betok (Anabas testudineus), Tambakan (Helostoma temminckii), Baung (Mystus nemurus), Singgaringan (Mystus nigriceps), Lundu (Mystus Gulio), Lais lampok (Cryptopterus limpok), Lele (Clarias spp.), Singgaringan (Mystus nigriceps), Lundu (Mystus Gulio) Kakapar (Peristolepis fasciatus). -
Tropical Peatlands of Southeast Asia
Tropical peatlands of Southeast Asia: Functions, threats and the role of fire in climate change mitigation Matthew Warren [email protected] USDA Forest Service, Northern Research Station Tropical peat swamp forests are ecologically diverse Tropical wetland forests Structurally similar to other upland tropical wet forests. Hydric conditions drive ecosystem processes and functions, supporting unique biological communities physically and physiologically adapted to the anaerobic soil environment. Southeast Asia: The global center of tropical peatlands About 44.1 Mha of tropical peatlands ~11% of the total peatland area; volume is ~18 -25% (Page et al. 2011). About 25 Mha (56%) of tropical peatlands occur in SE Asia. Indonesia contains around 47% (Page et al. 2011). TRUE EXTENT? Miettinen et al. 2011 Posa et al. (2011) Extensive peatlands occur in Sumatra, Borneo, and W. Papua (not shown) Posa et al. 2011 Ecosystem Services Environmental functions that support human well-being - Supporting: Primary production, nutrient cycling, soil maintenance - Provisioning: Food, water, fiber, timber, fuel, medicine, NTFP’s - Regulating: Climate, floods, sedimentation, drought, disease - Cultural: Aesthetic, spiritual, recreational, educational, ecotourism - Biological: Unique biodiversity, genetic and biochemical resources Hydrological Regulation Faiz Rahman $ustenance Timber • Local construction • Commercial extraction • Fuel wood • Charcoal Biological Diversity Many flagship species for conservation find refuge in wetland forests. Countless plants, fungi, fish and insects remain poorly known or undescribed. B. Kauffman ZSL- Berbak Orangutan Tropical Peatland Project: www.outrop.com Carbon Storage • Tropical wetlands store more C per ha than any other tropical forest type • Tropical peatlands store about 88.6 Gt C, 15-19% of global peat C pool • Estimates range from about 2000-3000 Mg C/ha, average 2009 MgC/ha globally (Page et al. -
Contributions of Organic and Inorganic Matter to Sediment 10.1002/2015EF000334 Volume and Accretion in Tidal Wetlands at Steady State
Earth’s Future RESEARCH ARTICLE Contributions of organic and inorganic matter to sediment 10.1002/2015EF000334 volume and accretion in tidal wetlands at steady state Special Section: James T. Morris1, Donald C. Barber2, John C. Callaway3, Randy Chambers4, Scott C. Hagen5, Integrated field analysis & Charles S. Hopkinson6, Beverly J. Johnson7, Patrick Megonigal8, Scott C. Neubauer9, modeling of the coastal Tiffany Troxler10, and Cathleen Wigand11 dynamics of sea level rise in 1Department of Biological Sciences, Belle W. Baruch Institute for Marine & Coastal Sciences, University of South the northern Gulf of Mexico Carolina, Columbia, South Carolina, USA, 2Department of Geology, Bryn Mawr College, Bryn Mawr, Pennsylvania, USA, 3Department of Environmental Science, University of San Francisco, San Francisco, California, USA, 4Keck Environmental Key Points: Field Laboratory, College of William and Mary, Williamsburg, Virginia, USA, 5Department of Civil & Environmental • Sediment bulk density can be largely Engineering and Center for Computation & Technology, Louisiana State University, Baton Rouge, Louisiana, USA, explained by its organic matter 6Department of Marine Sciences, University of Georgia, Athens, Georgia, USA, 7Department of Geology, Bates College, concentration 8 9 • Bulk volume approximates the Lewiston, Maine, USA, Smithsonian Environmental Research Center, Edgewater, Maryland, USA, Department of summed volumes of the mineral and Biology, Virginia Commonwealth University, Richmond, Virginia, USA, 10Department of Biological Sciences, -
Hydrological Self-Regulation of Domed Peatlands in South-East Asia and Consequences for Conservation and Restoration
Hydrological self-regulation of domed peatlands in south-east Asia and consequences for conservation and restoration R. Dommain, J. Couwenberg and H. Joosten Institute of Botany and Landscape Ecology, Ernst-Moritz-Arndt University, Greifswald, Germany _______________________________________________________________________________________ SUMMARY This article explores the hydrological constraints on the existence of forested peat domes (peat swamp forests) in the humid tropics, the self-regulation mechanisms that enable them to persist and the implications for restoration of damaged domes. The most important requirement for the preservation of peat is permanent saturation by water. The variable input of precipitation must be translated into a constant water supply to the peat mound. In intact tropical peat swamp domes, water is stored above the peat surface in depressions between hummocks that surround tree trunks and between spreading buttress roots. This above-ground water store is analogous to the water stored in the loose upper layer of peat and vegetation in Sphagnum bogs. The horizontal differentiation of the peat swamp forest floor into hummocks with limited hydraulic conductivity and depressions with high storage capacity resembles the hummock-hollow patterning of these Sphagnum bogs. Hummocks and other surface elements functionally resemble V-notch weirs that regulate water availability. Buttressed trees play a key role in providing the structural elements for hydrological self-regulation. An additional level of regulation is found in the concentric zonation of forest types with increased presence of buttressed trees on steeper margins. Conservation and restoration efforts should take into account the inter- relationships between trees, water and peat and the hydrological feedbacks that operate as a consequence.