Contents and Disclaimer IPC 2012 Proceedings

Total Page:16

File Type:pdf, Size:1020Kb

Contents and Disclaimer IPC 2012 Proceedings 14th International Peat congress, Sweden 2012 Proceedings 1 14th International Peat congress, Sweden 2012 DISCLAIMER: The Organising Committee of the 14th International Peat Congress does not accept responsibility for the accuracy or completeness of the contents of the oral and poster presentations that are published in the Proceedings. These have not been ‘peer reviewed’ and have only been checked for English meaning and style and consistency with the ‘Guide to Authors’. Authors should be contacted di- rectly for further information. 2 14th International Peat congress, Sweden 2012 Contents Keynotes Strategy for responsible peatland management – what and what next? Jack Rieley Challenges and prospects for the peat and growing media industry Leading the way to responsible resource management of climate Norbert Siebels Peatlands in the global carbon cycle and their role as modifiers Nigel Roulet The governance of peatlands/wetlands in Sweden Lena Ek/Anders Flanking Themes/Sub-themes I.Inventory, stratigraphy and conservation of mires and peatlands Abstract Abstract no Spruce-Peatland Responses Under Climatic and Environmental Change An In Situ Warming by Carbon Dioxide Manipulation of a Characteristic High-Carbon Ecosystem................................................................109 Paul J. Hanson, Randall K. Kolka, Colleen Iversen, Steven D. Sebestyen, Richard J. Norby, Brian Palik, Jeffrey Warren, Peter Thornton, Stan D. Wullschleger General review of the Peat Landscape Geochemistry in European Russia and distribution of Ge, U and 137Cs in peat soils........................121 Vera N. Kreshtapova Sterol and N-alkaline biomarker composition of modern fen plants – potential application for palaeoecological analyses.....................................................186 Ronkainen, T The peat investigations in the Geological Survey of Finland........................................223 Samu Valpola, Asta Harju, Teuvo Herranen, Tapio Toivonen, Onerva Valo, Tuija Vähäkuopus The Accounting of peat resources in Finland...............................................................243 Asta Harju, Samu Valpola 3 14th International Peat congress, Sweden 2012 Abstract Abstract no The Accounting of peat resources in Southern Ostrobothnia, Western Finland – a digital map service pilot....................................................................244 Asta Harju, Samu Valpola Holocene carbon accumulation in the Hudson Bay Lowland, Canada (Short abstract)............................................................................................................263 Maara Packalen, Sarah Finkelstein Peat increment in the old mires of the Green Belt of Fennoscandia in Kuhmo - Kostamus watershed area...............................................281 Tapio Lindholm, Oleg Kuznetsov, Raimo Heikkilä Digital Surface Model building on base of photo flights with an ultra light aircraft...........................................................................357 Bernd Hofer, Imre Sajtos, Andre Hallscheidt Subfossil Swedish bog-pines as indicators of mid-Holocene palaeohydrology and climate.................................................................393 Johannes Edvardsson, Dan Hammarlund, Hans Linderson, Mats Rundgren Using ground penetrating radar to map peat condition at a landscape scale................452 Lauren Parry I.1 Mire ecology and biodiversity Can peatland plants take up organic nitrogen?..............................................................13 Tim Moore, Amanda Alfonso, Bev Clarkson Photosynthetic responses in Sphagnum spp. in temperate mires to temperature, pH and salinity (Short abstract)............................................................63 Akira Haraguchi Vegetation cycles in boreal peatland ponds: effects of drought and flooding.................78 Barbara Nicholson, Suzanne Bayley Utilization of generalized linear and generalized additive models to predict Sphagnum and ericaceous shrubs distributions in peatlands........................156 Rémy Pouliot, Line Rochefort Sphagnum decay rate as a functional trait (Short abstract)..........................................246 Fia Bengtsson, Håkan Rydin 4 14th International Peat congress, Sweden 2012 Abstract Abstract no Microbial communities in boreal peatlands of the Athabaska region, Canada: building a reference for fen creation............................................................................251 Roxane Andersen, J.S Price, R.R.E Artz, T. Freitag Soil microbial diversity and spatiality across peatland vegetation mosaics under restoration in the southern Pennines, UK.............................................258 Robin Sen, David Elliott, Felix Nwaishi, Graham Smith, Robin Caporn World of Sphagnum – distribution pattern as a reflection of ecology and taxonomy.............................................................................................293 Dierk Michaelis Vegetation composition and dynamics of forested mires in Finland during 1985–2006 (Short abstract)......................................346 Leila Korpela Plant cover and state of treeless fen communities in Estonia........................................359 Laimi Truus, Mati Ilomets, Raimo Pajula, Kairi Sepp Vegetation and state of mire forests in Estonia............................................................379 Raimo Pajula, Mati Ilomets, Kairi Sepp, Laimdota Truus Pollution and climate influences on vegetation of UK peatlands..................................404 Simon Caporn, Chris Field, Nancy Dise, Richard Payne, Lucy Sheppard, Ian Leith, Andrea Britton, Sally Power, Georgina Southon, Bridget Emmett, Rachel Helliwell, Laurence Jones, Steven Lees, Steve Hughes, Gareth Phoenix, Carly Stevens I.2 Mire hydrology and hydrochemistry Laggs of raised bogs in coastal British Columbia, Canada: Hydrology, hydrochemistry, and vegetation at the mire margin.....................................11 Sarah Howie, Paul Whitfield, Richard Hebda, Ilja van Meerveld Source of drainage water acidity in peat harvesting.......................................................42 Anneli Wichmann DIC and DOC in three mires representing different peatland development stages in a calcareous area of central Sweden............................................96 Anders Löfgren, Peter Saetre 5 14th International Peat congress, Sweden 2012 Abstract Abstract no Seasonal variations in heavy metal content in water from a polluted mire in southern Poland.....................................................................101 Beata Smieja-Krol, Barbara Fialkiewicz-Koziel, Arkadiusz Bauerek Influence of ditching on the hydrolgy of mire lakes.....................................................194 Pentti Åman, Johanna Partanen The impact of ditch blocking on peatland hydrology at the Gordonbush Estate, Brora, Scotland, UK....................................................................................................226 Ben Smith, Susan Waldron, Andrew Henderson, Hugh Flowers, David Gilvear Dissolved organic carbon concentrations in bogs under grassland in Northern Germany along gradients in soil organic matter and groundwater depth.............................................................232 Stefan Frank, Bärbel Tiemeyer, Annette Freibauer Estimation of mire water balance in Western Siberia...................................................265 Yulia Kharanzhevskaya Hydrological modelling of peatlands – an evaluation of meteorological input data...........................................................................................273 Enrico Frahm, Ullrich Dettmann, Roland Fuss Runoff changes after rewetting of a cutover peatland in Sweden.................................310 Torbjörn Nilsson, Lars Lundin, Sabine Jordan, Elve Lode, Monika Strömgren Field measurement of the ground water flow in the high moor peat in the Sarobetsu Mire, Hokkaido, Japan.....................................................................323 Koichi Yamamoto, Gatot Susilo, Toshio Noda, Masahiko Sekine, Tsuyoshi Imai, Yuko Yamamoto, Harukuni Tachibana, Kazuya Otani, Masayuki Oishi Effects of site characteristics on cumulative frequency distribution of water table depth in peatlands.................................................................................360 Michel Bechtold, Michel Bechtold, Bärbel Tiemeyer, Enrico Frahm, Annette Freibauer The effects of regional groundwater in bogland restoration (Short abstract)...............361 Shane Regan, Paul Johnston Nitrogen and dissolved organic carbon (DOC) losses from a degraded peatland in North-Eastern Germany.................................................367 Baerbel Tiemeyer, Petra Kahle 6 14th International Peat congress, Sweden 2012 Abstract Abstract no Effects of peatland to water quality. Comparison of peat harvesting, peatland forestry and natural peatland using continuous monitoring stations...............................................395 Pia Högmander, Päivi Saari Value-adding of fen peatlands using their purification potential with respect to surface water.........................................................................423 Dagmar Balla, Sebastian Maassen, Ralf Dannowski, Anja Coors Yulia Kharanzhevskaya I.3 Peatlands as historical archives Simple geochemical characteristics of peat in reconstructing peatland history...............30 Monika Metrak, Malgorzata Suska-Malawska Carbon accumulation shows the interplay between the natural succession of mires and climate changes......................................................49 Markku Mäkilä, Matti Saarnisto
Recommended publications
  • 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
    [Show full text]
  • Proceedings of the Eleventh Muskeg Research Conference Macfarlane, I
    NRC Publications Archive Archives des publications du CNRC Proceedings of the Eleventh Muskeg Research Conference MacFarlane, I. C.; Butler, J. For the publisher’s version, please access the DOI link below./ Pour consulter la version de l’éditeur, utilisez le lien DOI ci-dessous. Publisher’s version / Version de l'éditeur: https://doi.org/10.4224/40001140 Technical Memorandum (National Research Council of Canada. Associate Committee on Geotechnical Research), 1966-05-01 NRC Publications Archive Record / Notice des Archives des publications du CNRC : https://nrc-publications.canada.ca/eng/view/object/?id=05568728-162b-42ca-b690-d97b61f4f15c https://publications-cnrc.canada.ca/fra/voir/objet/?id=05568728-162b-42ca-b690-d97b61f4f15c Access and use of this website and the material on it are subject to the Terms and Conditions set forth at https://nrc-publications.canada.ca/eng/copyright READ THESE TERMS AND CONDITIONS CAREFULLY BEFORE USING THIS WEBSITE. L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site https://publications-cnrc.canada.ca/fra/droits LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB. Questions? Contact the NRC Publications Archive team at [email protected]. If you wish to email the authors directly, please see the first page of the publication for their contact information. Vous avez des questions? Nous pouvons vous aider. Pour communiquer directement avec un auteur, consultez la première page de la revue dans laquelle son article a été publié afin de trouver ses coordonnées. Si vous n’arrivez pas à les repérer, communiquez avec nous à [email protected].
    [Show full text]
  • 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.
    [Show full text]
  • Can Peatland Landscapes in Indonesia Be Drained Sustainably? an Assessment of the ‘Eko-Hidro’ Water Management Approach
    Peatland Brief Can Peatland Landscapes in Indonesia be Drained Sustainably? An Assessment of the ‘eko-hidro’ Water Management Approach Peatland Brief Can Peatland Landscapes in Indonesia be Drained Sustainably? An Assessment of the ‘eko-hidro’ Water Management Approach July, 2016 Under the projects Indonesia Peatland Support Project (IPSP) funded by CLUA Sustainable Peatland for People and Climate (SPPC) funded by Norad To be cited as: Wetlands International, Tropenbos International, 2016. Can Peatland Landscapes in Indonesia be Drained Sustainably? An Assessment of the ‘Eko-Hidro’ Water Management Approach. Wetlands International Report. Table of Contents Table of Contents ........................................................................................................................... iii List of Tables .................................................................................................................................... iv List of Figure ..................................................................................................................................... iv Summary ........................................................................................................................................... iii 1. Introduction ............................................................................................................................. 1 2. The ‘eko-hidro’ peatland management approach and the Kampar HCV Assessment .............................................................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Assessment on Peatlands, Biodiversity and Climate Change: Main Report
    Assessment on Peatlands, Biodiversity and Climate change Main Report Published By Global Environment Centre, Kuala Lumpur & Wetlands International, Wageningen First Published in Electronic Format in December 2007 This version first published in May 2008 Copyright © 2008 Global Environment Centre & Wetlands International Reproduction of material from the publication for educational and non-commercial purposes is authorized without prior permission from Global Environment Centre or Wetlands International, provided acknowledgement is provided. Reference Parish, F., Sirin, A., Charman, D., Joosten, H., Minayeva , T., Silvius, M. and Stringer, L. (Eds.) 2008. Assessment on Peatlands, Biodiversity and Climate Change: Main Report . Global Environment Centre, Kuala Lumpur and Wetlands International, Wageningen. Reviewer of Executive Summary Dicky Clymo Available from Global Environment Centre 2nd Floor Wisma Hing, 78 Jalan SS2/72, 47300 Petaling Jaya, Selangor, Malaysia. Tel: +603 7957 2007, Fax: +603 7957 7003. Web: www.gecnet.info ; www.peat-portal.net Email: [email protected] Wetlands International PO Box 471 AL, Wageningen 6700 The Netherlands Tel: +31 317 478861 Fax: +31 317 478850 Web: www.wetlands.org ; www.peatlands.ru ISBN 978-983-43751-0-2 Supported By United Nations Environment Programme/Global Environment Facility (UNEP/GEF) with assistance from the Asia Pacific Network for Global Change Research (APN) Design by Regina Cheah and Andrey Sirin Printed on Cyclus 100% Recycled Paper. Printing on recycled paper helps save our natural
    [Show full text]
  • Glossary Ablation Till: Till Carried on Or Near the Surface of a Glacial Ice Column and Let Down As the Glacier Melted and Retreated
    Glossary ablation till: till carried on or near the surface of a glacial ice column and let down as the glacier melted and retreated. alluvium: any mineral or detrital sediment that is transported and deposited by the flowing water of a river or stream. Riverbeds, floodplains, and deltas are all made up of alluvium. backswamp: low-lying wet areas on river floodplains, located away from the active river channel. basal till: till carried in the base of a glacial ice column and deposited under the glacier. Basal till is therefore very dense and typically forms a layer that impedes drainage. biological diversity (biodiversity): the complexity of all life at all its levels of organization, including genetic variability within species, species and species interac- tions, ecological processes, and the distribution of species and natural communities across the landscape. bog: an acidic, peat-accumulating wetland that is isolated from mineral-rich water sources by deep peat accumulation and therefore receives most of its water and nutri- ents from precipitation. Bogs are dominated by sphagnum moss and heath family shrubs. boreal forest: a circumpolar band of northern forests bordered to the north by open tundra and to the south by more transitional forests. Boreal forests are characterized by species of pine, spruce, fir, tamarack, birch, and poplar that are adapted to the extreme cold of this region. bryophyte: a division of plants including the mosses, liverworts, and hornworts. calciphile: a plant that thrives in calcium-rich soils. circumneutral: having a pH near 7.0 and therefore neither strongly acidic nor basic. cliff: an exposed, steep face of rock.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Wetlands in Agricultural Landscapes
    Wetlands at the National and International Scale General Information 1. Agricultural conservation: USDA needs to better indicators/ human activity/ forestry practices/ birds/ ensure protection of highly erodible cropland and Amphibia/ Minnesota/ disturbance/ vertebrates/ Chordata/ wetlands: Report to the ranking Democratic member, animals/ west north central states of USA/ north central Committee on Agriculture, Nutrition, and Forestry, U.S. states of USA/ United States/ North America/ developed Senate. countries/ OECD countries/ lake states of USA United States. General Accounting Office. Abstract: The present study explores the relationships U.S. General Accounting Office, 2003. between riparian wetland communities and anthropogenic Notes: Cover title./ "April 2003."/ Chiefly tables./ Includes disturbances, including urban, forestry and cultivated land. bibliographical references (p. 106). Small stream riparian wetlands in central Minnesota, USA, http://www.gao.gov/new.items/d03418.pdf provided an opportunity to detect these relationships Descriptors: agricultural conservation---United States/ soil because land use within the region is heterogeneous, conservation---United States/ wetland conservation--- resulting in disturbance gradients at the scales of stream United States reach and landscape. The research tested 2 hypotheses: organismal groups (wet meadow vegetation, shrub carr 2. Agricultural wetlands and waterbirds: A review. vegetation, aquatic macro-invertebrates, amphibians, fish Czech, H. A. and Parsons, K. C. and birds) respond
    [Show full text]