Soil Ecology Web: Design Guidelines for Protecting

Total Page:16

File Type:pdf, Size:1020Kb

Soil Ecology Web: Design Guidelines for Protecting SOIL ECOLOGY WEB: DESIGN GUIDELINES FOR PROTECTING AND GROWING YOUR RESOURCE by ANNETTE JAEGER GRIFFIN (Under the Direction of C. Scott Nesbit) ABSTRACT The foundation of healthy landscapes lies just below the surface. The subterranean ecology of our backyards helps determine how water moves across our land, which plants we can grow, and how nutrient-rich our edibles will be, among other things. There is a direct link between caring for our soil and caring for ourselves; and yet, the most serious natural disaster that Georgia has faced is the loss of its topsoil. This study outlines patterns of amendment via a digital humanities counterpart, Soil Ecology Web (SEW), which recommends design guidelines derived from the study of soil ecology that anyone with a plot of land can follow to protect and grow their resource. INDEX WORDS: Georgia, southern outer piedmont, soil, soil ecology, soil protection, soil growth, soil health, landscape architecture, design, ecological design, topsoil, topsoil regeneration, planting, hardscape, circulation, grading, Soil Ecology Web, SEW, digital humanities, interdisciplinary design SOIL ECOLOGY WEB: DESIGN GUIDELINES FOR PROTECTING AND GROWING YOUR RESOURCE By ANNETTE JAEGER GRIFFIN B.F.A., The University of the Arts, 2010 A Thesis Submitted to the Graduate Faculty of The University of Georgia in Partial Fulfillment of the Requirements for the Degree MASTER OF LANDSCAPE ARCHITECTURE ATHENS, GEORGIA 2016 © 2016 Annette Jaeger Griffin All Rights Reserved SOIL ECOLOGY WEB: DESIGN GUIDELINES FOR PROTECTING AND GROWING YOUR RESOURCE by ANNETTE JAEGER GRIFFIN Major Professor: C. Scott Nesbit Committee: Ronald Sawhill Dorcas Franklin Stephen Brooks Electronic Version Approved: Suzanne Barbour Dean of the Graduate School The University of Georgia August 2016 DEDICATION For Bill and Florence, who taught my primer on the blessings of Georgia. "iv ACKNOWLEDGEMENTS This thesis is the result of the support and inspiration I received from teachers, friends, and family. I am continually astonished and delighted by the great luck of their company: Scott Nesbit is not only a poetic historian and witty conversationalist, but also one of the most supportive people I know. Ron Sawhill’s sincere engagement and kindness with his students is an example of how to best give one’s energy to the community. Marianne Cramer instills heart into each lecture she gives, and galvanized the beat of this research. Stephen Brooks joined my committee two weeks before I was scheduled to defend, and seems always ready with excellent advice. Dory Franklin offers sweetness and insight with every breath. Alfie Vick has a wonderful knack for showing me new places to love. Melissa Tufts makes everything seem interesting, and does so with a heck of a lot of humor and grace. Donna Gabriel saves me from my disorganized self. There are many other professors and faculty who have made hugely positive impacts upon my work, and I thank each of them sincerely, with my best wishes for their continued success and happiness. My friends and family have traced innumerable paths over the maps of experience, and I keep their atlas beside me always. Bruce is so annoying and so dear to me that I think we must be related. Genna is a spark in the night, and her sweetness is my favorite campfire. The cousins are simply my best people, and Sis is my best sis: brilliant, beautiful, and expertly fun. Mom’s talent for adaptation is a constant source of inspiration. Dad gets me, and consequently worries for me, like no one else (though I love him all the more for that). Jackie clears the way and shows me how to do it. Lynn, who was Wyoming’s best premium prickly pear and a klutz who could fly a plane, is missed every day. ! "v TABLE OF CONTENTS ACKNOWLEDGEMENTS V CHAPTER 1: OUR LAYERED EXISTENCE 1 INTRODUCTION 1 PROBLEMATIC 1 RESEARCH QUESTION 5 VI SECONDARY QUESTIONS 5 ARGUMENT 6 CONTEXT 6 SIGNIFICANCE 7 PURPOSE 7 TERMS AND DEFINITIONS 8 LITERATURE REVIEW 9 LIMITATIONS 15 DELIMITATIONS 15 RESEARCH METHODS 16 CHAPTER 2: SOIL IN GEORGIA’S SOUTHERN OUTER PIEDMONT 17 FORMATION 17 VI EVOLUTION 18 GROWING A LABYRINTH 19 LOSING PASSAGE 20 HERITAGE IS WHAT WE HAVE LEFT 21 CHAPTER 3: THE LIVING LABYRINTH 23 PRIORITIES 23 THEORY OF FLOW 23 THEORY OF HABITAT 28 THEORY OF PROTECTION 30 THEORY OF DECOMPOSITION 32 THEORY OF RESILIENCE 33 THEORY OF HERITAGE 35 CHAPTER 4: SOIL ECOLOGY WEB 41 ANYONE CAN DESIGN FOR SOIL PROTECTION AND GROWTH 41 BEFORE YOU BEGIN 43 DESIGN FOR FLOW 43 DESIGN FOR HABITAT 47 DESIGN FOR PROTECTION 49 DESIGN FOR DECOMPOSITION 51 DESIGN FOR RESILIENCE 53 VII DESIGN FOR HERITAGE 56 CHAPTER 5: SOIL ECOLOGY WEB, A RESOURCE FOR EVERYONE 59 EASY ACCESS 59 INTENDED USERS 60 DESIGN AND LAYOUT 61 FEATURES 61 OPPORTUNITIES FOR IMPROVEMENT 125 CONCLUSION 125 BIBLIOGRAPHY 127 VIII CHAPTER 1: OUR LAYERED EXISTENCE INTRODUCTION As a Piedmont native returned from over a decade of living outside of Georgia, I have become devoted to the ecologies of this region. Upon my homecoming, I saw the forests and hills with nostalgia, without realizing how much they have been compromised over the past two hundred years. I have since begun to see them differently; with just as much reverence, but also with an understanding that these are systems in need of repair. When I learned that almost all of Georgia’s topsoil has been washed from the uplands to the coast, I was astounded by the sheer volume of physical loss. Later conversations with landscape architects and horticulturalists clued me in to the full extent of the disaster; not only are ecosystem services such as water infiltration, carbon sequestration, and energy and nutrient storage impacted, but the welfare of systems above ground is as well (Wall 2004). As a practicing landscape architect, my responsibilities will lie in cultivating the expression, development, and function of ecosystems within the built environment. I believe in dealing with the accompanying issues through longterm approaches that create opportunities for experimentation, and hope that these will lead to fundamental changes that benefit the health of my home. PROBLEMATIC Throughout our planet’s history, ecological networks have developed, thrived, flickered, and disappeared. We know of, and have even witnessed, many such occurrences; however, there are probably billions more that we shall never see. Many of these invisible communities lie "1 not just on the surface of the earth, but also beneath it in a complex, living labyrinth that lays the foundation for everything above solid ground. They have wrapped our planet in a resource that is as much a living entity as it is an object and place. The soil is alive and when healthy, soil fauna eat and drink what we lay down for them, and we eat and drink what they send up to us. This is not science fiction, this is soil ecology. Although we dwell in layered spaces, these layers separate us only visually. It is easy to sigh over the strange circumstance of our life above the soil and dismiss it as too complex or inconsequential to consider when designing our world. This is a mistake. Our lives are inextricably entwined with the existence of these communities, and even our smallest movements impact them. When simply raking the leaves on a cloudy afternoon can lead to a microscopic diaspora, it is in our best interest to understand what effects this can have on our lives and how we might address them in order to ensure personal benefit. How, though, a soil’s optimum potential provides a number of ecosystem services. As the basis of biodiversity on our planet, it impacts the overall health, resilience, fertility, and quality of our land. It provides habitat and food for organisms that live in and around it. It regulates our water quality and filtration, it helps to regulate greenhouse gases and stores carbon, is the largest bank or reserve of fresh water on our planer, and decontaminates waste products. Soil also provides a surface for our picnics and walks, structural support for our homes, and a place for our ancestors to rest. It has the potential to heighten both the beauty of our surroundings and our understanding of the systems that we live in. As with any ecosystem service, it is difficult to estimate the monetary value of our inherited benefit. Although we know that soil provides numerous services, categorized by cultural, regulatory, supporting, and provisioning characteristics, much of the value of this resource is most often measured in conjunction with specific terrestrial ecosystems (Comerford "2 and Morris 2013). Currently, there is no estimation as to how much capital soil directly saves and generates worldwide. Of course, this resource’s value lies in a gradient along macro- and micro-economic lines. Soil is a form of heritage and a living record of our history. It is sweet to think that in a few hundred years bragging rights could be attached to the length of a particular tract’s preservation; that someone might say to a guest at their house, “Our family has been growing that soil for years. My great-grandmother began restoring it when she was a girl.”1 Any benefit here would lie in accordance with the concept of vertical wealth, a rich personal and familial accrual of resources developed over time through the care and maintenance of a single place (Falk 2013). Despite its value, and the fact that soil scientists and agriculturalists have been trying for centuries to improve general understanding of this material, soil is frequently taken for granted. Both the resource’s vastness and its relative invisibility have contributed to the dearth of our understanding of it, and although it is encouraging that soil science and its ecology is steadily gaining recognition as a discipline to be applied to the development of built environments, there is little information on how to go about doing this.
Recommended publications
  • Tillage and Soil Ecology: Partners for Sustainable Agriculture
    Soil & Tillage Research 111 (2010) 33–40 Contents lists available at ScienceDirect Soil & Tillage Research journal homepage: www.elsevier.com/locate/still Review Tillage and soil ecology: Partners for sustainable agriculture Jean Roger-Estrade a,b,*, Christel Anger b, Michel Bertrand b, Guy Richard c a AgroParisTech, UMR 211 INRA/AgroParisTech., Thiverval-Grignon, 78850, France b INRA, UMR 211 INRA/AgroParisTech. Thiverval-Grignon, 78850, France c INRA, UR 0272 Science du sol, Centre de recherche d’Orle´ans, Orle´ans, 45075, France ARTICLE INFO ABSTRACT Keywords: Much of the biodiversity of agroecosystems lies in the soil. The functions performed by soil biota have Tillage major direct and indirect effects on crop growth and quality, soil and residue-borne pests, diseases Soil ecology incidence, the quality of nutrient cycling and water transfer, and, thus, on the sustainability of crop Agroecosystems management systems. Farmers use tillage, consciously or inadvertently, to manage soil biodiversity. Soil biota Given the importance of soil biota, one of the key challenges in tillage research is understanding and No tillage Plowing predicting the effects of tillage on soil ecology, not only for assessments of the impact of tillage on soil organisms and functions, but also for the design of tillage systems to make the best use of soil biodiversity, particularly for crop protection. In this paper, we first address the complexity of soil ecosystems, the descriptions of which vary between studies, in terms of the size of organisms, the structure of food webs and functions. We then examine the impact of tillage on various groups of soil biota, outlining, through examples, the crucial effects of tillage on population dynamics and species diversity.
    [Show full text]
  • Soil Ecology
    LSC 322 Laboratory 10 LAB #10: SOIL ECOLOGY Soil is one of the earth’s most important resources. For a community of plants and animals to become established on land, soil must first be present. Further, soil quality is often a limiting factor for growth many systems. Soil is a complex mixture of inorganic and organic materials, microorganisms, water and air. The weathering of bedrock produces small grains of rock that accumulate as a layer on the surface of the earth. There they are altered by biology, becoming mixed with organic matter, which results from the decomposition of the waste products and dead tissue of living organisms to form humus. The soil formation process is very slow (hundreds to thousands of years), so it can be very detrimental to a community if the soil is lost through erosion or its quality degraded by pollution or misuse. Soil Sampling As a class, we will identify interesting soil ecosystems on campus that we would like to examine further. Your small group will be assigned to collect one of those samples. Using a trowel, you will scoop the top 5 cm (this is where most of the biological “action” happens) into a ziplock bag. Also, take notes to record the environmental surroundings. What is the land usage? What plants are growing here? What is the soil moisture? These environmental characteristics will influence many aspects of the soil. Questions - Describe the environment from which you took your soil sample. Include all of the information from your notes. - How do these conditions relate to the soil characteristics measured during the lab exercise (texture, nutrients, pH, and biota)? After samples are collected, we will return to the lab and measure the following characteristics: Soil Texture Soil texture refers to the proportion of sand, silt, and clay present in a soil, which differ in their particle size.
    [Show full text]
  • Soil As a Huge Laboratory for Microorganisms
    Research Article Agri Res & Tech: Open Access J Volume 22 Issue 4 - September 2019 Copyright © All rights are reserved by Mishra BB DOI: 10.19080/ARTOAJ.2019.22.556205 Soil as a Huge Laboratory for Microorganisms Sachidanand B1, Mitra NG1, Vinod Kumar1, Richa Roy2 and Mishra BB3* 1Department of Soil Science and Agricultural Chemistry, Jawaharlal Nehru Krishi Vishwa Vidyalaya, India 2Department of Biotechnology, TNB College, India 3Haramaya University, Ethiopia Submission: June 24, 2019; Published: September 17, 2019 *Corresponding author: Mishra BB, Haramaya University, Ethiopia Abstract Biodiversity consisting of living organisms both plants and animals, constitute an important component of soil. Soil organisms are important elements for preserved ecosystem biodiversity and services thus assess functional and structural biodiversity in arable soils is interest. One of the main threats to soil biodiversity occurred by soil environmental impacts and agricultural management. This review focuses on interactions relating how soil ecology (soil physical, chemical and biological properties) and soil management regime affect the microbial diversity in soil. We propose that the fact that in some situations the soil is the key factor determining soil microbial diversity is related to the complexity of the microbial interactions in soil, including interactions between microorganisms (MOs) and soil. A conceptual framework, based on the relative strengths of the shaping forces exerted by soil versus the ecological behavior of MOs, is proposed. Plant-bacterial interactions in the rhizosphere are the determinants of plant health and soil fertility. Symbiotic nitrogen (N2)-fixing bacteria include the cyanobacteria of the genera Rhizobium, Free-livingBradyrhizobium, soil bacteria Azorhizobium, play a vital Allorhizobium, role in plant Sinorhizobium growth, usually and referred Mesorhizobium.
    [Show full text]
  • Dynamics of Soil Nitrogen and Carbon Accumulation for 61 Years After Agricultural Abandonment
    Ecology, 81(1), 2000, pp. 88±98 q 2000 by the Ecological Society of America DYNAMICS OF SOIL NITROGEN AND CARBON ACCUMULATION FOR 61 YEARS AFTER AGRICULTURAL ABANDONMENT JOHANNES M. H. KNOPS1 AND DAVID TILMAN Department of Ecology, Evolution and Behavior, University of Minnesota, St. Paul, Minnesota 55108 USA Abstract. We used two independent methods to determine the dynamics of soil carbon and nitrogen following abandonment of agricultural ®elds on a Minnesota sand plain. First, we used a chronosequence of 19 ®elds abandoned from 1927 to 1982 to infer soil carbon and nitrogen dynamics. Second, we directly observed dynamics of carbon and nitrogen over a 12-yr period in 1900 permanent plots in these ®elds. These observed dynamics were used in a differential equation model to predict soil carbon and nitrogen dynamics. The two methods yielded similar results. Resampling the 1900 plots showed that the rates of accumulation of nitrogen and carbon over 12 yr depended on ambient carbon and nitrogen levels in the soil, with rates of accumulation declining at higher carbon and nitrogen levels. A dynamic model ®tted to the observed rates of change predicted logistic dynamics for nitrogen and carbon accumulation. On average, agricultural practices resulted in a 75% loss of soil nitrogen and an 89% loss of soil carbon at the time of abandonment. Recovery to 95% of the preagricultural levels is predicted to require 180 yr for nitrogen and 230 yr for carbon. This model accurately predicted the soil carbon, nitrogen, and carbon : nitrogen ratio patterns observed in the chronosequence of old ®elds, suggesting that the chronose- quence may be indicative of actual changes in soil carbon and nitrogen.
    [Show full text]
  • Fundamentals in Soil Science Course a Course Offered by the Soil Science Society of America
    Fundamentals in Soil Science Course A course offered by the Soil Science Society of America. This course is divided into six modules: Fundamentals of Soil Genesis, Classification, and Morphology, Fundamentals in Soil Chemistry and Mineralogy, Fundamentals in Soil Fertility and Nutrient Management, Soil Biology and Soil Ecology, Influences and Management of Soil Physical Properties and Soil and Land Use Management. Each module contains 2 lessons. Lectures are approximately two hours. To maximize learning, students will be expected to spend time reading and studying outside of the recorded lesson. Course Description The Soil Science Fundamentals Review Course is designed to provide an overview of the fundamental concepts in soil science: Genesis, Classification and Morphology, Physics, Chemistry, Fertility, Biology, and Land Use. Instructors will use the Fundamentals Performance Objectives (POs) as a guide for discussing topics within each section, but will not go through each objective individually. However, students are encouraged to ask questions regarding specific POs if needed. The objective of the course is to provide the student with a formalized way to build their fundamental knowledge and skills within the different areas of soil science to enhance their professional skills and/or to prepare to take the Fundamentals of Soil Science Exam. Lecture material is supplemented with additional readings and practical examples to illustrate the concepts and provide practical examples of how the concepts are used in practice. This course is not designed to teach a student how to take the Fundamentals Exam, but instead is designed to complement the students existing knowledge of soil science and help the student understand the principles behind the POs.
    [Show full text]
  • Unit 2.3, Soil Biology and Ecology
    2.3 Soil Biology and Ecology Introduction 85 Lecture 1: Soil Biology and Ecology 87 Demonstration 1: Organic Matter Decomposition in Litter Bags Instructor’s Demonstration Outline 101 Step-by-Step Instructions for Students 103 Demonstration 2: Soil Respiration Instructor’s Demonstration Outline 105 Step-by-Step Instructions for Students 107 Demonstration 3: Assessing Earthworm Populations as Indicators of Soil Quality Instructor’s Demonstration Outline 111 Step-by-Step Instructions for Students 113 Demonstration 4: Soil Arthropods Instructor’s Demonstration Outline 115 Assessment Questions and Key 117 Resources 119 Appendices 1. Major Organic Components of Typical Decomposer 121 Food Sources 2. Litter Bag Data Sheet 122 3. Litter Bag Data Sheet Example 123 4. Soil Respiration Data Sheet 124 5. Earthworm Data Sheet 125 6. Arthropod Data Sheet 126 Part 2 – 84 | Unit 2.3 Soil Biology & Ecology Introduction: Soil Biology & Ecology UNIT OVERVIEW MODES OF INSTRUCTION This unit introduces students to the > LECTURE (1 LECTURE, 1.5 HOURS) biological properties and ecosystem The lecture covers the basic biology and ecosystem pro- processes of agricultural soils. cesses of soils, focusing on ways to improve soil quality for organic farming and gardening systems. The lecture reviews the constituents of soils > DEMONSTRATION 1: ORGANIC MATTER DECOMPOSITION and the physical characteristics and soil (1.5 HOURS) ecosystem processes that can be managed to In Demonstration 1, students will learn how to assess the improve soil quality. Demonstrations and capacity of different soils to decompose organic matter. exercises introduce students to techniques Discussion questions ask students to reflect on what envi- used to assess the biological properties of ronmental and management factors might have influenced soils.
    [Show full text]
  • Articles, and the Creation of New Soil Habitats in Other Scientific fields Who Also Made Early Contributions Through the Weathering of Rocks (Puente Et Al., 2004)
    Editorial SOIL, 1, 117–129, 2015 www.soil-journal.net/1/117/2015/ doi:10.5194/soil-1-117-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. The interdisciplinary nature of SOIL E. C. Brevik1, A. Cerdà2, J. Mataix-Solera3, L. Pereg4, J. N. Quinton5, J. Six6, and K. Van Oost7 1Department of Natural Sciences, Dickinson State University, Dickinson, ND, USA 2Departament de Geografia, Universitat de València, Valencia, Spain 3GEA-Grupo de Edafología Ambiental , Departamento de Agroquímica y Medio Ambiente, Universidad Miguel Hernández, Avda. de la Universidad s/n, Edificio Alcudia, Elche, Alicante, Spain 4School of Science and Technology, University of New England, Armidale, NSW 2351, Australia 5Lancaster Environment Centre, Lancaster University, Lancaster, UK 6Department of Environmental Systems Science, Swiss Federal Institute of Technology, ETH Zurich, Tannenstrasse 1, 8092 Zurich, Switzerland 7Georges Lemaître Centre for Earth and Climate Research, Earth and Life Institute, Université catholique de Louvain, Louvain-la-Neuve, Belgium Correspondence to: J. Six ([email protected]) Received: 26 August 2014 – Published in SOIL Discuss.: 23 September 2014 Revised: – – Accepted: 23 December 2014 – Published: 16 January 2015 Abstract. The holistic study of soils requires an interdisciplinary approach involving biologists, chemists, ge- ologists, and physicists, amongst others, something that has been true from the earliest days of the field. In more recent years this list has grown to include anthropologists, economists, engineers, medical professionals, military professionals, sociologists, and even artists. This approach has been strengthened and reinforced as cur- rent research continues to use experts trained in both soil science and related fields and by the wide array of issues impacting the world that require an in-depth understanding of soils.
    [Show full text]
  • RIVM Rapport 711701047 Ecological Risk Assessment of Contaminated Land
    Ecological Risk Assessment of Contaminated Land Risk of Contaminated Assessment Ecological This book is the outcome of the EU-funded research project ‘Liberation’ which looked to the development of a decision support system for sustainable Land Risk of Contaminated Assessment Ecological This book is the outcome of the EU-funded research project ‘Liberation’ which management of contaminated land by linking bioavailability, ecological risk Ecological Risk looked to the development of a decision support system for sustainable Ecological Risk and ground water pollution – focussing particularly on organic contaminants. management of contaminated land by linking bioavailability, ecological risk The aim is to provide guidance to risk assessors and stakeholders of and ground water pollution – focussing particularly on organic contaminants. AssessmentAssessment of of contaminated land in their decision making process. The book is organised in The aim is to provide guidance to risk assessors and stakeholders of two parts. contaminated land in their decision making process. The book is organised in Contaminated Land two parts. Chapters 1-3 give short introductions and an overview of relevant Contaminated Chapters 1-3 give short introductions and an overview of relevant topics, topics, whilst Chapters 4-7 give more detailed guidance on how to perform an whilst Chapters 4-7 give more detailed guidance on how to perform an Ecological Risk Assessment of contaminated sites using the Triad approach. Ecological Risk Assessment of contaminated sites using the Triad approach. Land Chapter One gives a brief introduction to the overall principles and concepts in Chapter One gives a brief introduction to the overall principles and concepts in ecological risk assessment and decision support systems.
    [Show full text]
  • Soil Science 1
    Soil Science 1 Soil Chemistry and Plant Nutrition: Nutrient cycling; nutrient recovery from wastewater; molecular visualization of soil minerals SOIL SCIENCE and molecules; soil acidification. The Department of Soil Science provides undergraduate and graduate Professor William Bleam education in the environmental, agricultural, and natural resource Surface and Colloid Chemistry: Physical chemistry of soil aspects of soils. Areas of emphasis include soil ecology; soil erosion colloids and sorption processes, chemistry of humic substances, management; soil fertility and plant nutrition; soil physical and chemical factors controlling biological availability of contaminants to characterization; biogeochemistry; urban soils; soil carbon; soil health; microorganisms, magnetic resonance and synchrotron studies of soil contaminants; waste management; pedology; and land-use analysis. adsorption and precipitation. Soils are a critical natural resource in environmental protection, food Assistant Professor Zachary Freedman and fiber production, turf and grounds management, rural and urban planning, and waste disposal. All of these facets are integrated into the Soil microbiology, ecology and sustainability: Effects of environmental department's course offerings and research programs. Soil Science change on biogeochemical cycles; community ecology and trophic majors prepare for professional, technical, consulting, and project dynamics; forest soil ecology; soil organic matter dynamics; sustainable positions in environmental sciences, ecology and restoration, crop and agroecosystems; bio-based product crop production on marginal lands. timber production, soil informatics, soil conservation, environmental pollution control, turf and grounds management, and land-use planning. Professor Alfred Hartemink Please contact the department for further information on career Pedology and Digital Soil Mapping: Pedology, soil carbon; digital soil opportunities. mapping; tropical soils; history and philosophy of soil science.
    [Show full text]
  • Methods of Analysis Soil Sampling
    Soil Sampling and Methods of Analysis Second Edition ß 2006 by Taylor & Francis Group, LLC. In physical science the first essential step in the direction of learning any subject is to find principles of numerical reckoning and practicable methods for measuring some quality connected with it. I often say that when you can measure what you are speaking about, and express it in numbers, you know something about it; but when you cannot measure it, when you cannot express it in numbers, your knowledge is of a meagre and unsatisfactory kind; it may be the beginning of knowledge, but you have scarcely in your thoughts advanced to the state of science, whatever the matter may be. Lord Kelvin, Popular Lectures and Addresses (1891–1894), vol. 1, Electrical Units of Measurement Felix qui potuit rerum cognoscere causas. Happy the man who has been able to learn the causes of things. Virgil: Georgics (II, 490) ß 2006 by Taylor & Francis Group, LLC. Soil Sampling and Methods of Analysis Second Edition Edited by M.R. Carter E.G. Gregorich Canadian Society of Soil Science ß 2006 by Taylor & Francis Group, LLC. CRC Press Taylor & Francis Group 6000 Broken Sound Parkway NW, Suite 300 Boca Raton, FL 33487-2742 © 2008 by Taylor & Francis Group, LLC CRC Press is an imprint of Taylor & Francis Group, an Informa business No claim to original U.S. Government works Printed in the United States of America on acid-free paper 10 9 8 7 6 5 4 3 2 1 International Standard Book Number-13: 978-0-8493-3586-0 (Hardcover) This book contains information obtained from authentic and highly regarded sources.
    [Show full text]
  • A Future for Soil Ecology ? Connecting the System Levels
    Eur. J. Soil Biol. 37 (2001) 213−220 © 2001 Éditions scientifiques et médicales Elsevier SAS. All rights reserved S1164556301010871/FLA A future for soil ecology ? Connecting the system levels: moving from genomes to ecosystems Opening Lecture to the XIII ICSZ “Biodiversity of soil organisms and ecosystem functioning” Herman Eijsackers* Alterra Green World Research, POB 47 6700 AA Wageningen, The Netherlands and Institute for Ecological Studies, Vrije Universiteit Amsterdam, Netherlands Received 18 August 2000; accepted 23 July 2001 Abstract − As an introduction to the XIII ICSZ “Biodiversity of soil organisms and ecosystem functioning” the question is raised what contribution soil ecology has made to general ecology. Although the appearance of soil ecological papers in general ecological journals is limited, soil ecologists have had a major contribution to especially functional aspects of ecology like nutrient release and energy turnover mechanisms, perhaps partly due to the applied character of soil ecology. As a way forward it is suggested to unify further work and scientific discussions according to five research themes: 1. Combined spatial and temporal heterogeneity; 2. Scaling up from individual mobility via distribution patterns to bio-geography; 3. Structural and functional biodiversity: from gene- to ecosystem level; 4. Nutrient cycling/energy transfer at the micro- to macro-level; 5. Adaptability from bacteria to ecosystems: is there a mutual mechanism connecting genetic variation with ecosystems´ adaptive mechanisms? © 2001 Éditions scientifiques et médicales Elsevier SAS micro- and macro-scale connections / nutrient cycling / organism adaptability / soil ecology / spatial and temporal heterogeneity 1. INTRODUCTION 2000 to discuss the way forward in the 21st century (see for an overview [27]).
    [Show full text]
  • Soil Biology and Land Management
    Soil Quality – Soil Biology Technical Note No. 4 Soil Biology and Land Management Table of contents The goal of soil biology management.......................................... 2 Why should land managers understand soil biology?.................. 2 The underground community....................................................... 4 What controls soil biology? ......................................................... 5 General management strategies ................................................... 7 Considerations for specific land uses......................................... 10 Cropland.............................................................................. 10 Soil Quality – Soil Biology Forestland............................................................................ 13 Technical Note No. 4 Rangeland............................................................................ 15 Assessment and monitoring....................................................... 17 January 2004 Summary.................................................................................... 19 NRCS file code: 190-22-15 References and further resources............................................... 19 Other titles in this series: #1 Soil Biology Primer Introduction #2 Introduction to Microbiotic Crusts The purpose of this technical note is to provide information about the #3 Soil Biology Slide Set effects of land management decisions on the belowground component of the food web. It points out changes in soil biological function that land managers should
    [Show full text]