DOCSLIB.ORG

Acrotelm Survey of Clara Bog I I Part One

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Acrotelm Survey of Clara Bog I I Part One I IRISII - DlITCH RAISED BOG STUDY ~4u~D I GEOHYDROLOGY ECOLOGY :-Jer'C"-~:r.en~ Er:y~ru~i::-em~1 ~:c:~,:,~io=: cn~ 8' Ne'io:loJ Fo:-k, C:~~ \tv"iicli'iie SC':--.·i:~ o of r':oru:e (o:uervo1icn.. I 01 the ·:>Hice o! PLl~;it Works, ;-l..biin 'v,lildliie M!:""u2e.,~e,r,. TIM; Hogue ~ N oli,;,n~J ~ores: SeTvj~e, Drie!:l(!T'<!cn I I A.CROTELlvI SIJRVEY OF CLARo\. BOG I .1 J.R.G. van der Cruiisen _A. r'urent. .. I R. van VVolfswin.4.el I I Agricaltural University, Dept, of Water Resources Nieu...ve Kanaalll, NL-6709PA Wageningen, I The Netherlands I I .... I • Q ( il .---------~---------- I I I I Acrotelm survey of Clara Bog I I Part one: I J.H.G. van der Cruijsen A. Grent I R. van Wolfswinkel I Part two: I R. van Wolfswinkel I Appendices: I J.H.G. van der Cruijsen A. Grent I R. van Wolfswinkel I August, 1993 I I I~ I Wageningen Agricultural University Department of Water Resources "I" Nieuwe Kanaal 11, 6709 PA Wageningen, The Netherlands I l ' ~,----".----"-'----- ~ -------------------- 'I I I I I Erratum I The map scaleson appendices V.1, V.2, VI.1 and VI.2 show 2.5em to 1 km. I This should be 2.5 cm to 200 m I' I I I I I I .-I I I I I I ------------------•••• 2 ;? ? 'I_ ', _. ~-r- ,- -,,"=¥,",:, ,.'" -' ,- -- - .. I I­ I I· I I I PART ONE I I I- I I I I I I I I II lJ___.. ------'(N),.J -~-~-~-------------- I I PREFACE I This report is the result of a close cooperation between the authors. But we never could have done this without some very good help and assistance. Therefore we would like to thank everyone who has given us a helping hand. Especially we would I like to thank Sake van der Schaaf, our supervisor, for giving us directions and keeping us in touch with the Netherlands, Mr. F. Dolezal for the supply of the evaporation I figures and last but not least our Irish colleagues: Ray, lara and Mary. For this research we spent five months in Ireland. Although we were staying in Clara I during one of the wettest winters in years, we enjoyed almost every minute of it. The sport- and publife was a welcome diversion after working on a cold and wet bog all day. We thank the people of Clara for their hospitality and friendship which we I enjoyed during our stay. I Wageningen, April 1993. I I I I I I I I I I I I ..-..-_----------------~(~ -------------------- I I INDEX I PREFACE I INDEX INDEX OF TABLES AND FIGURES I SUMMARY I page 1 INTRODUCTION 1 1.1 The project 1 I 1.2 The report 2 2 RECONSTRUCTION AND GENERAL DESCRIPTION 3 I 2.1 Reconstruction of the development of raised bogs 3 2.2 Clara Bog 5 I 2.3 The main discharge systems on Clara-West 8 3 ACROTELM 11 3.1 The diplotelmic bog 11 I 3.2 Acrotelm mapping 13 3.2.1 The acrotelm map 13 3.2.1.1 Introduction 13 I 3.2.1.2 Methods ' 13 3.2.1.3 Results 14 3.2.2 The augerholes and hummock/hollow map 15 I 3.2.2.1 Introduction 15 3.2.2.2 Methods 15 I 3.2.2.3 Results 16 . 3.3 Relation acrotelm thickness and vegetation 17 3.3.1 Introduction ················ 17 I 3.3.2 Methods 1:- 3.3.3 Results ············ 18 3.3.4 Conclusions 22 I 3.4 Relation acrotelm thickness and slope 23 3.4.1 Introduction ············ 23 3.4.2 Methods 23 I 3.4.3 Results ········ 24 3.4.3.1 Clara-West 24 3.4.3.2 Clara-East 24 I 3.4.4 Conclusions 25 3.5 Relation acrotelm thickness and the fluctuation of the phreatic level 26 I 3.5.1 Introduction ············· 26 3.5.2 Methods 26 I I ( vi) I 3.5.2.1 Clara-West 26 I 3.5.2.1 Clara-East 27 3.5.3 Results ········ 27 3.5.3.1 Clara-West 27 'I 3.5.3.2 Clara-East 28 3.5.4 Conclusions 28 3.6 The methods for measuring the transmissivity .: 29 I 3.6.1 Introduction ········· 29 3.6.2 The two methods 29 3.6.2.1 The Guinness method 29 I 3.6.2.2 The Pitbailing method 30 3.6.3 The conditions for the two methods and the accuracy of the measurements 31 I 3.6.4 The accuracy of the measured transmissivities in general 36 3.7 Transmissivity 36 I 3.7.1 Introduction ·· .. ·.·· 36 3.7.2 Humification degree 37 3.7.3 Depth of the phreatic level 38 I 3.7.4 Transmissivity related to acrotelm thickness 39 3.7.5 Transmissivity related to vegetation cover 41 3.8 A and m as indicators of the condition of the bog 47 I 4 EVAPOTRANSPIRATION 49 ,I 4.1 Introduction 49 4.2 The different methods 49 4.2.1 The Penman and the Thorn & Oliver equations 49 I 4.2.2 lysimeters 50 4.3 Results 52 4.3.1 The Penman and the Thorn & Oliver equations 52 I 4.3.2 lysimeters 53 5 SYNTHESIS 57 I 5.1 Introduction 57 5.2 Synthesis 57 I 6 CONCLUSIONS AND RECOMMENDATIONS 59 6.1 Introduction 59 6.2 Conclusions 59 I 6.3 Recommendations 61 I REFERENCES I I I I ~-\~ . I I INDEX OF TABLES AND FIGURES I Tables page 2.1 Time table for the blo-geological periods after the Weichsel-Pleniglacial 5 I 2.2 Preference of Sphagna for range of pH and the bog water level 8 2.3 The discharge of the Rossum, Thomson and Tunnel drains and their mutual I ratio's, measured with a bucket and a stop-watch .- 9 3.1 . Characteristic differences between the properties of acrotelm and catotelm . 12 3.2 Augerhole classification 16 I 3.3 Relation complex type and acrotelm thickness 19 3.4 Vegetation and presence of acrotelm 23 3.5 The chosen cross sections 24 I 3.6 The acrotelm thickness at the different tubes 26 3.7 Transmissivities calculated by using different methods .. " 33 3.8 Transmissivity calculated according the Guinness method, using different. I imaginary J1 and t values 34 3.9 Transmissivity depending on drawdown, pumping time and discharge, measured at location 03 at a water level of 2.8 em. below surface, using the I Guinness method 36 3.10 Average values for the A and m factors and the standard deviations per acrotelm thickness 40 I 3.11 The m- and A-values for areas with different acrotelm thicknesses within the Sphagnum magellanicum zone : ..•.... 41 I 3.12 Acrotelm holes, vegetation zone, acrotelm thickness, m- and A-values .... 45 4.1 Evapotranspiration in mmlday according to the Penman and Thorn & Oliver equation ..........................................•~ ..... 52 I 4.2 Daily average evapotranspiration in mmlday measured with Iysimeters ..•. 53 I 4.3 Monthly evapotranspiration 54 I I I I I I I • (riit) I Figures page I 1.1 location of Clara and Raheenmore bogs 1 I 2.1 Stages in the development of a raised bog 4 2.2 Raised bog confined in a deep basin 6 I 3.1 Relation storage coefficient and humification degree 34 3.2 The effect upon the transmissivity when u, t and Sw differ 35 3.3 Humification-permeability correlation in top layer 37 I 3.4 Relation kD and depth for a degree of humification of: 38 a 4 b 5 I c 6 d 7 3.5 The relation transmissivity-depth of the water table for different acrotelm I thicknesses within the Sphagnum magellanicum zone 42 3.6 Variation with depth z of the mean estimate of hydraulic conductivity, LIII: Sphagnum capil/ifolium, lIV Sphagnum magellanicum 43 I 4.1 Evapotranspiration Thorn & Oliver versus Iysimeters 54 I 4.2 Monthly evapotranspiration calculated with the two equations and measured with the lysimeters 55 I I I I I I I I I. I I ~i)._ I I SUMMARY I In the north-western part of Europe raised bogs have become rare, The Irish government tries to preserve the raised bog remnants now as good as possible. Sound hydrological management is therefore needed. The Irish-Dutch bog project is set up to I find solutions concerning this management. The project is a cooperation between the Irish Wildlife Service and the Dutch National Forest Service. I This report consists mainly of an inventory of the health of Clara Bog, especially of the toplayer, the acrotelm. To understand the importance of the acrotelm first a I reconstruction and a general description of Clara Bog is given. The acrotelm is the toplayer of the bog. It is defined here as the top layer that consists of fresh to almost unhumified plant remains with a humification degree of 1 or 2. It is I important for the bog because of its hydrological characteristics, like its relatively high permeability and its periodically fluctuating phreatic level.. The main discharge of excess rainwater is through this layer. A thick acrotelm normally means that the bog I is healthy. To gain information about the spatial variabi lity of the acrotelm layer, an acrotelm I thickness map was made for both Clara-East and Clara-West. This was done with the "foot-spade" method. Also some augerings were made to give some information about the state of health the bog is in.
Load more

Recommended publications
  • Global Peatland Restoration Manual
    Global Peatland Restoration Manual Martin Schumann & Hans Joosten Version April 18, 2008 Comments, additions, and ideas are very welcome to: [email protected] [email protected] Institute of Botany and Landscape Ecology, Greifswald University, Germany Introduction The following document presents a science based and practical guide to peatland restoration for policy makers and site managers. The work has relevance to all peatlands of the world but focuses on the four core regions of the UNEP-GEF project “Integrated Management of Peatlands for Biodiversity and Climate Change”: Indonesia, China, Western Siberia, and Europe. Chapter 1 “Characteristics, distribution, and types of peatlands” provides basic information on the characteristics, the distribution, and the most important types of mires and peatlands. Chapter 2 “Functions & impacts of damage” explains peatland functions and values. The impact of different forms of damage on these functions is explained and the possibilities of their restoration are reviewed. Chapter 3 “Planning for restoration” guides users through the process of objective setting. It gives assistance in questions of strategic and site management planning. Chapter 4 “Standard management approaches” describes techniques for practical peatland restoration that suit individual needs. Unless otherwise indicated, all statements are referenced in the IPS/IMCG book on Wise Use of Mires and Peatlands (Joosten & Clarke 2002), that is available under http://www.imcg.net/docum/wise.htm Contents 1 Characteristics,
    [Show full text]
  • Peat Bog Ecosystems: Structure, Form, State and Condition
    IUCN UK Committee Peatland Programme Briefing Note No. 2 IUCN UK Committee Peatland Programme Briefing Note No 2 Peat Bog Ecosystems: Structure, Form, State and Condition Structure : Actively-growing bogs are wetlands which consist of two layers – a thin living two layers surface layer of peat-forming vegetation (the acrotelm), generally between 10 cm and 40 cm deep, and the relatively inert, permanently-waterlogged peat store (the catotelm) Critical which may be several metres deep. A peat bog can thus be thought of as a tree, much- importance of compressed in the vertical dimension. The acrotelm represents the thin canopy the living consisting of leaves on a tree, the catotelm represents the branches and trunk of surface layer the tree. The analogy is not perfect because in a tree the water travels upwards through (acrotelm) the trunk to the leaves, whereas water in a bog travels from the living canopy downwards into the trunk of the catotelm. The acrotelm supplies plant material which then forms peat in the catotelm, much as leaves provide the products of photosynthesis to create the trunk and branches of a tree. Without an acrotelm a bog cannot accumulate peat or control water loss from the catotelm, just as a tree cannot grow without its canopy of leaves. In a fully functioning natural bog only the acrotelm is visible because the catotelm peat beneath is normally shielded from view by the living acrotelm, much as only the forest canopy is visible when forests are viewed from above. 1. Acrotelm 2. Catotelm Peat-forming Peat-forming species are wetland species, generally consisting of the Sphagnum bog species are mosses and cotton grasses, although other material such as non-Sphagnum mosses, wetland purple moor grass, or heather stems and roots can sometimes make significant species contributions to the peat matrix particularly in shallower or degraded peats.
    [Show full text]
  • Raised Bog Restoration to Peat Producing Sphagnum Species: an Overview of European Approaches
    Raised Bog Restoration to Peat Producing Sphagnum Species: An Overview of European Approaches Steve Roos INTRODUCTION The use of peatlands in Europe for human purposes has a history that dates back over a millennia. Before the advent of commercial exploitation, peat was used as a domestic fuel and the drained fields put into agricultural production. Urban and commercial expansion, beginning in the Middle Ages, created great demands for fuel. This demand, combined with shrinking woodlands, provided the incentive to develop methods of commercial bog exploitation (Borger 1990). The use of peat as a fuel continues up to the present, especially in peat rich, coal poor countries. Peat is also used extensively in horticulture as a soil conditioner, mulch and in growing media (Bather and Miller 1991). In addition, after the cessation of peat harvesting, bogs were almost always reclaimed for human use, most often for agriculture. Currently, commercial peat harvesting in Europe is concentrated on a specialized form of peatland, the raised bog. This extensive history of human influence has impacted the ecological processes to some degree in essentially every raised bog throughout Europe (Wheeler and Shaw 1995). In recent times, there has been an increasing awareness of the value of natural systems. This awareness has extended to raised bogs not only for their value as a biological resource but also for their value as a renewable (albeit slowly) consumable resource. The importance of raised bogs in wildlife management, in the control of hydrological regimes and as global carbon sinks has also been identified (Bather and Miller 1991). For these reasons much recent research has been devoted to identifying suitable restoration techniques for raised bogs affected by peat extraction.
    [Show full text]
  • Operational Guide Forest Road Wetland Crossings Learning from Field Trials in the Boreal Plains Ecozone of Manitoba and Saskatchewan, Canada
    OPERATIONAL GUIDE FOREST ROAD WETLAND CROSSINGS LEARNING FROM FIELD TRIALS IN THE BOREAL PLAINS ECOZONE OF MANITOBA AND SASKATCHEWAN, CANADA SFI-01536 VERSION 1.0 MAY 2014 PURPOSE OF THIS GUIDE The purpose of this guide is to provide forestry professionals and contractors with a general understanding of boreal wetlands, what to expect in terms of water movement between different types of wetlands and general considerations when planning, constructing, monitoring and decommissioning wetland crossings. ACKNOWLEDGMENTS The project team would like to extend our sincere gratitude and appreciation to the Sustainable Forestry Initiative Inc. (SFI) PURPOSE OF THIS GUIDE AND ACKNOWLEDGMENTS PURPOSE OF for their commitment to helping the forest industry and other organizations achieve sustainable forest management. SFI has recognized the importance of wetlands as an integral component of healthy forest landscapes through their financial support of this project. We applaud SFI for their continued support of projects like ours through the Conservation and Community Partnerships Grant Program that contribute to enhancement of current and future SFI forest certification standards. The project team would like to thank all partners who were instrumental in assisting with the design, development and implementation of all aspects of this project: Ducks Unlimited Canada, FPInnovations, Louisiana-Pacific Canada Ltd., Weyerhaeuser Canada, and Spruce Products Ltd. In addition, we would also like to thank all of the staff and forestry contractors who participated in the workshops and implementation of the field trials in Manitoba and Saskatchewan. DISCLAIMER The information included in this handbook constitutes advice/guidance based on work undertaken by the project partners. It does not exclude other methods that may be suitable, should not be relied upon as legal advice, and does not supersede any regulatory requirements.
    [Show full text]
  • Wetlands-Different Types, Their Properties and Functions
    Technical Report TR-04-08 Wetlands – different types, their properties and functions Erik Kellner Dept of Earth Sciences/Hydrology Uppsala University August 2003 Wetlands – different types, their properties and functions Erik Kellner Dept of Earth Sciences/Hydrology Uppsala University August 2003 Keywords: Bog, Wetlands, Mire, Biosphere, Ecosystem, Hydrology, Climate, Process. This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author and do not necessarily coincide with those of the client. A pdf version of this document can be downloaded from www.skb.se Summary In this report, different Swedish wetland types are presented with emphasis on their occurrence, vegetation cover, soil physical and chemical properties and functions. Three different main groups of wetlands are identified: bogs, fens and marshes. The former two are peat forming environments while the term ‘marshes’ covers all non-peat forming wetlands. Poor fens are the most common type in Sweden but (tree-covered) marshes would probably be dominating large areas in Southern Sweden if not affected by human activity such as drainage for farming. Fens and bogs are often coexisting next to each other and bogs are often seen to be the next step after fens in the natural succession. However, the development of wetlands and processes of succession between different wetland types are resulting from complicated interactions between climate, vegetation, geology and topography. For description of the development at individual sites, the hydrological settings which determine the water flow paths seem to be most crucial, emphasizing the importance of geology and topography.
    [Show full text]
  • Conceptual Frameworks in Peatland Ecohydrology: Looking Beyond the Two-Layered (Acrotelm–Catotelm) Model†
    ECOHYDROLOGY Ecohydrol. 4, 1–11 (2011) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/eco.191 Ecohydrology Bearings—Invited Commentary Conceptual frameworks in peatland ecohydrology: looking beyond the two-layered (acrotelm–catotelm) model† Paul J. Morris,1* J. Michael Waddington,1 Brian W. Benscoter2 and Merritt R. Turetsky3 1 McMaster Centre for Climate Change and School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario, Canada 2 Department of Biological Sciences, Florida Atlantic University, Davie, Florida, USA 3 Department of Integrative Biology, University of Guelph, Guelph, Ontario, Canada ABSTRACT Northern peatlands are important shallow freshwater aquifers and globally significant terrestrial carbon stores. Peatlands are complex, ecohydrological systems, commonly conceptualized as consisting of two layers, the acrotelm (upper layer) and the catotelm (lower layer). This diplotelmic model, originally posited as a hypothesis, is yet to be tested in a comprehensive manner. Despite this, the diplotelmic model is highly prevalent in the peatland literature, suggesting a general acceptance of the concept. We examine the diplotelmic model with respect to what we believe are three important research criteria: complexity, generality and flexibility. The diplotelmic model assumes that all ecological, hydrological and biogeochemical processes and structures can be explained by a single discrete boundary—depth in relation to a drought water table. This assumption makes the diplotelmic scheme inherently inflexible, in turn hindering its representation of a range of ecohydrological phenomena. We explore various alternative conceptual approaches that might offer greater flexibility, including the representation of horizontal spatial heterogeneity and transfers. We propose that the concept of hot spots, prevalent in terrestrial biogeochemistry literature, might be extended to peatland ecohydrology, providing a more flexible conceptual framework.
    [Show full text]
  • Working Today for Nature Tomorrow Proceedings of the Risley Moss Bog Restoration Workshop, 26-27 February 2003 23
    Proceedings of the Risley Moss Bog Restoration Workshop 26-27 February 2003 working today for nature tomorrow Proceedings of the Risley Moss Bog Restoration Workshop, 26-27 February 2003 23 PEAT FORMING PROCESS AND RESTORATION MANAGEMENT Richard A Lindsay Head of Conservation, School of Health & Bioscience, University of East London HE restoration of bogs has received If the EC definition is taken as the the story should be quite the reverse. considerable attention in recent years. yardstick of restoration success (and it is Cajander (1913) addressed these two T Given that no truly natural bogs difficult to find specific or better alternative anomalous observation by proposing that remain in the lowlands of Britain (Lindsay & forms of yardstick within the literature), the sometimes peat is able to form directly on Immirzi 1996), those who take on the key is clearly the establishment of appropriate ground that was formerly dry. He observed management of an ombrotrophic bog system, peat-forming vegetation. Given this that such a phenomenon is possible if the particularly in the lowlands, are generally objective, it is very important to understand climate is sufficiently wet, or if the ground faced with a site requiring significant, if not the mechanisms by which such vegetation becomes wet because of adjacent substantial, ‘restoration’ management. types arise spontaneously when devising, waterlogging. He termed this process A considerable body of experience about evaluating or choosing restoration techniques paludification . restoration
    [Show full text]
  • An Acrotelm Transplant Experiment on a Cutover Peatland-Effects On
    AN ACROTELM TRANSPLANT EXPERIMENT ON A CUTOVER PEATLAND­ EFFECTS ON MOSITURE DYNAMICS AND C02 EXCHANGE By JASON P. CAGAMPAN, BES A Thesis Submitted to the School of Graduate Studies In Partial Fulfillment of the Requirements For the Degree Master of Science McMaster University ©Copyright by Jason P. Cagampan, September 2006 MASTER OF SCIENCE (2006) McMaster University (Geography) Hamilton, Ontario TITLE: An Acrotelm Transplant Experiment on a Cutover Peatland - Effects on Moisture Dynamics and C02 Exchange AUTHOR: Jason P. Cagampan SUPERVISOR: Professor J. Michael Waddington NUMBER OF PAGES: xi, 96 ii ABSTRACT Natural peatlands are an important component of the global carbon cycle representing a net long-term sink of atmospheric carbon dioxide (COz). The natural carbon storage function of these ecosystems can be severely impacted due to peatland drainage and peat extraction leading to large and persistent sources of atmospheric COz following peat extraction abandonment. Moreover, the cutover peatland has a low and variable water table position and high soil-water tension at the surface which creates harsh ecological and microclimatic conditions for vegetation reestablishment, particularly peat-forming Sphagnum moss. Standard restoration techniques aim to restore the peatland to a carbon accumulating system through various water management techniques to improve hydrological conditions and by reintroducing Sphagnum at the surface. However, restoring the hydrology of peatlands can be expensive due to the cost of implementing the various restoration techniques. The goal of this study is to examine a new extraction-restoration technique where the acrotelm is preserved and replaced on the cutover surface. More specifically, this thesis examines the effects of an acrotelm transplant experiment on the hydrology (i.e.
    [Show full text]
  • Peatlands on National Forests of the Northern Rocky Mountains: Ecology and Conservation
    United States Department Peatlands on National Forests of of Agriculture Forest Service the Northern Rocky Mountains: Rocky Mountain Ecology and Conservation Research Station General Technical Report Steve W. Chadde RMRS-GTR-11 J. Stephen Shelly July 1998 Robert J. Bursik Robert K. Moseley Angela G. Evenden Maria Mantas Fred Rabe Bonnie Heidel The Authors Acknowledgments Steve W. Chadde is an Ecological Consultant in Calu- The authors thank a number of reviewers for sharing met, MI. At the time of this research project he was their expertise and comments in the preparation of this Ecologist with the USDA Forest Service’s Northern Region report. In Montana, support for the project was provided Natural Areas Program. by the Natural Areas Program of the Northern Region/ Rocky Mountain Research Station, U.S. Department of J. Stephen Shelly is a Regional Botanist with the USDA Agriculture, Forest Service. Dan Svoboda (Beaverhead- Forest Service’s Northern Region Headquarter’s Office Deerlodge National Forest) and Dean Sirucek (Flathead in Missoula, MT. National Forest) contributed portions of the soils and Robert J. Bursik is Botanical Consultant in Amery, WI. geology chapters. Louis Kuennen and Dan Leavell At the time of this research he was a Botanist with the (Kootenai National Forest) guided the authors to sev- Idaho Department of Fish and Game’s Conservation eral interesting peatlands. Mark Shapley, hydrologist, Data Center in Boise, ID. Helena, MT, volunteered his time and provided insights Robert K. Moseley is Plant Ecologist and Director for the into the hydrology and water chemistry of several rich Idaho Department of Fish and Game’s Conservation fens.
    [Show full text]
  • The Hydrology of Bog Ecosystems I
    I-.\~· . ,. s~ ,·8~, I ~'8 rlR , Staatsbosbeheer ?I~'i~ , :: ~. ~i~t rl/!~,J ',' ~:, r•..; ,1;1' .. fl.' i\C: . '1[;;, THE HYDROLOGY OF BOG ECOSYSTEMS I ,. Guidelines for management I I I I I I I tl • J.G. Streefkerk and W.A.Casparie __________ - .. - .. - i- ---- , I I I THE HYDR a LOG Y a F BOG E COS YST EMS I GUIDELINES FOR MANAGEMENT J.G. Streefkerk 1 & W.A. Casparie 2 1 2 Staatsbosbeheer, Dutch National Forestry Service, Utrecht. I Biologisch-Archaelogisch Instituut, State University, Groningen. I Published in 1989, Staatsbosbeheer I I I t ...... i I I I .,, I " , --- -- -- -- I • I I TAB LE o F CON TEN TS PREFACE I PART I- THE HYDROLOGY OF BOG ECOSYSTEMS I 1. INTRODUCTION 4 1.1 Raised bog in the Netherlands and its general significance 4 I 1.2 The hydrological problems of the existing bog remnants 5 SPATIAL AND TEMPORAL ASPECTS AND CONDITIONS FOR THE INITIATION I OF THE FORMATION OF BOG 6 2.1 General 6 I 2.2 Origin and development; aspects of time and space 7 2.2.1 General 7 2.2.1 The earliest peat deposits 9 I 2.2.2 The formation of fen peat 10 2.2.3 The marginal zone of a fen, and the lagg-zone of a bog 11 2.2.4 Seepage peat 11 2.2.5 The start of ombrogenous peat formation 12 I 2.2.6 Highly humified Sphagnum peat 12 2.2.7 Hummock - hollow systems and dome shaped complexes 13 2.2.8 Poorly humified Sphagnum peat and bog pools 16 I 2.2.9 Contact zones and bog lakes 17 2.3 Initial conditions for the formation of ombrogenous peat 18 I 2.3.1 Initial conditions of the (mineral) subsoil, which can result in the development of Sphagnum peat 18 2.3.2 Peat producing substrates, originated in the past, in which increasing oligotrophic conditions played a role at the start I of raised bog development 19 2.3.3 Strongly changed hydrological conditions caused by recent or I subrecent human influences 21 3.
    [Show full text]
  • Ecology of a Peat Bog
    PRISTINE MIRE LANDSCAPES Ecology of a peat bog Ann Brown A&A Research, Old Moorcocks, Rushlake Green, Heathfield, E Sussex, UK, TN21 9PP Tel: +44 1435 830 243; e-mail: [email protected] Summary Previous work investigating Canadian peatlands and their ecology has shown the microbial activity responsi- ble for their formation and maintenance, as well as the ease with which this environment can be disturbed, pos- sibly with significant consequences. Research indicates that it is essential that we look very carefully how our actions may destroy these unique ecosystems. A general description of the ombrotrophic peat bog is followed by specific investigations into cellulose degradation, methane production, the hydraulic conductivity of peat and then of a possible methane inhibitor. These demonstrate the potential outcome of bog destruction, whether by physical removal or flooding, either by man or climate. Key index words: methane, peatlands, acrotelm, catotelm, methanogens Introduction reducing one. Also, since bogs do not readily drain, where The aim of this paper is to draw attention to the ecology of the climate is favourable they can easily increase in extent peatlands, in order to emphasize how this environment may and cover complete hillsides to form blanket bogs. impinge on government and industry, which may not be sufficiently aware of the readily available data, which may affect their policies. Having spent several years over a decade Studies ago working on some thirty Canadian peat bogs to better understand their ecology, and realising the potential of Cellulose degradation methane ebullition when their structure is destroyed, the Peat can be regarded as a soil matrix derived from plant author would like to ensure that the consequences are biomass, made up of three polymers, cellulose, hemicellu- understood.
    [Show full text]
  • Ecology and Conservation of a Northern Minnesota Peat Bog
    University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1990 Like nothing uphill : ecology and conservation of a northern Minnesota peat bog Peggy J. Wallgren The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Wallgren, Peggy J., "Like nothing uphill : ecology and conservation of a northern Minnesota peat bog" (1990). Graduate Student Theses, Dissertations, & Professional Papers. 7471. https://scholarworks.umt.edu/etd/7471 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. Maureen and Mike MANSFIELD LIBRARY Copying allowed as provided under provisions of the Fair Use Section of the U.S. COPYRIGHT LAW, 1976. Any copying for commercial purposes or financM gain may be undertoken only with the author’s written consent. MontanaUniversity of Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. LIKE NOTHING UPHILL: ECOLOGY AND CONSERVATION OF A NORTHERN MINNESOTA PEAT BOG by Peggy J. Wallgren B.S.. University of Minnesota, Duluth, 1987 Presented in partial fulfillment of the requirements for the degree of Master of Science University of Montana 1990 Approved by Chairman. Boardyof Eiaminers Wan Graduate School Daté/ Reproduced with permission of the copyright owner.
    [Show full text]