Appendices Soil Quality/Soil Health Cards
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Non-Timber Forest Products
Agrodok 39 Non-timber forest products the value of wild plants Tinde van Andel This publication is sponsored by: ICCO, SNV and Tropenbos International © Agromisa Foundation and CTA, Wageningen, 2006. All rights reserved. No part of this book may be reproduced in any form, by print, photocopy, microfilm or any other means, without written permission from the publisher. First edition: 2006 Author: Tinde van Andel Illustrator: Bertha Valois V. Design: Eva Kok Translation: Ninette de Zylva (editing) Printed by: Digigrafi, Wageningen, the Netherlands ISBN Agromisa: 90-8573-027-9 ISBN CTA: 92-9081-327-X Foreword Non-timber forest products (NTFPs) are wild plant and animal pro- ducts harvested from forests, such as wild fruits, vegetables, nuts, edi- ble roots, honey, palm leaves, medicinal plants, poisons and bush meat. Millions of people – especially those living in rural areas in de- veloping countries – collect these products daily, and many regard selling them as a means of earning a living. This Agrodok presents an overview of the major commercial wild plant products from Africa, the Caribbean and the Pacific. It explains their significance in traditional health care, social and ritual values, and forest conservation. It is designed to serve as a useful source of basic information for local forest dependent communities, especially those who harvest, process and market these products. We also hope that this Agrodok will help arouse the awareness of the potential of NTFPs among development organisations, local NGOs, government officials at local and regional level, and extension workers assisting local communities. Case studies from Cameroon, Ethiopia, Central and South Africa, the Pacific, Colombia and Suriname have been used to help illustrate the various important aspects of commercial NTFP harvesting. -
BEYOND the STATUS QUO: 2015 EQB Water Policy Report
BEYOND THE STATUS QUO: 2015 EQB Water Policy Report LAKE ST. CROIX TABLE OF CONTENTS Introduction . 4 Health Equity and Water. 5 GOAL #1: Manage Water Resources to Meet Increasing Demands . .6 GOAL #2: Manage Our Built Environment to Protect Water . 14 GOAL #3: Increase and Maintain Living Cover Across Watersheds .. 20 GOAL #4: Ensure We Are Resilient to Extreme Rainfall . .28 Legislative Charge The Environmental Quality Board is mandated to produce a five year water Contaminants of Emerging Concern . .34 policy report pursuant to Minnesota Statutes, sections 103A .204 and 103A .43 . Minnesota’s Water Technology Industry . 36 This report was prepared by the Environmental Quality Board with the Board More Information . .43 of Water and Soil Resources, Department of Agriculture, Department of Employment and Economic Development, Department of Health, Department Appendices available online: of Natural Resources, Department of Transportation, Metropolitan Council, • 2015 Groundwater Monitoring Status Report and Pollution Control Agency . • Five-Year Assessment of Water Quality Degradation Trends and Prevention Efforts Edited by Mary Hoff • Minnesota’s Water Industry Economic Profile Graphic Design by Paula Bohte • The Agricultural BMP Handbook for Minnesota The total cost of preparing this report was $76,000 • Water Availability Assessment Report 2 Beyond the Status Quo: 2015 EQB Water Policy Report Minnesota is home to more than 10,000 lakes, 100,000 miles of rivers and streams, and abundant groundwater resources. However, many of these waters are not clean enough. In 2015, we took a major step toward improving our water by enacting a law that protects water quality by requiring buffers on more than 100,000 acres of land adjacent to water. -
Gender and Non-Timber Forest Products
Gender and non-timber forest products Promoting food security and economic empowerment Marilyn Carr, international consultant on gender, technology, rural enterprise and poverty reduction, prepared this paper in collaboration with Maria Hartl, technical adviser for gender and social equity in the IFAD Technical Advisory Division. Other staff members of the IFAD Technical Advisory Division contributing to the paper included: Annina Lubbock, senior technical adviser for gender and poverty targeting, Sheila Mwanundu, senior technical adviser for environment and natural resource management, and Ilaria Firmian, associate technical adviser for environment and natural resource management. The following people reviewed the content: Rama Rao and Bhargavi Motukuri (International Network for Bamboo and Rattan), Kate Schreckenberg (Overseas Development Institute), Nazneen Kanji (Aga Khan Development Network), Sophie Grouwels (Food and Agriculture Organization of the United Nations) and Stephen Biggs (School of Development Studies, University of East Anglia). The opinions expressed in this book are those of the authors and do not necessarily represent those of the International Fund for Agricultural Development (IFAD). The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of IFAD concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The designations ‘developed’ and ‘developing’ countries are intended for statistical convenience and do not necessarily express a judgement about the stage reached by a particular country or area in the development process. Cover: Women make panels and carpets from braided coconut leaves at this production unit near Naickenkottai, India. -
Irrigation Management Effects on Soil Fertility and Environmental Impacts
Irrigation Management Effects on Soil Fertility and Environmental Impacts Mike Cahn, Irrigation and Water Resources Advisor, UCCE Monterey Water Management Needs to be Factored into Soil Fertility Management Costly to build up soil fertility in organic systems Poor water management can lead to loss of nutrients (mostly N and P) Potential water quality impairments from sediment and nutrients in run-off and leachate from organic fields Organic Liquid Fertilizers* (0.1 – 7% N) Activate, Micronized Fertall Liquid Iron Aqua Power Liquid Fish Fertall Liquid MB Azomite Fertall Liquid Zinc Biolink Organic 0/5/5 HFPC Hydrolyzed Fish Powder Biolink Organic 5/5/5 Maxicrop Kelp Extract Biolink•5-1-1 Organic liquidMicronutrients costs $9.6Micro Hume per lb of N Cranford's Micronized Compost Micro Phos Diamond•13-0-0 K Solution dry grade Gypsumcosts $4 Multi-Ke-Min per lb of N Earth Juice Bloom 0/3/1 Neptune's Harvest Liquid Fish Earth Juice Catalyst Nutra Min Earth Juice Grow 2/1/1 Omega 1/5/5 Eco-Hydro•A substantial fish Liquid amountOmega 6/6/6of the N Eco-Nereo Kelp and Humic Acids Phytamin 800 Eco-Polycould 21 mciro be Shrimp in mineralSolubor form Boron (12-50%) Feather Tea Sulfate of Potash, Diamond K Soluble Fertall Liquid Chelate Calcium *Organic Material Research Institute, National Organic Program Compost sources of Nitrogen • $1.5 - $2 per lb of N (1.4% N product) Cover Crops as a Source of Nitrogen •100 – 150 lb of N/acre in above ground Biomass •Production costs of $150 – $200/acre for a winter cover crop •$1-2 per lb of Nitrogen •Roughly -
Soils and Soil-Forming Material Technical Information Note 04 /2017 30Th November 2017
Soils and Soil-forming Material Technical Information Note 04 /2017 30th November 2017 Contents 1. Introduction to Soils ........................................................................................................................ 2 2. Components and Properties of Soil ................................................................................................ 7 3. Describing and Categorising soils .................................................................................................. 29 4. Policy, Regulation and Roles ......................................................................................................... 34 5. Soil Surveys, Handling and Management ..................................................................................... 40 6. Recommended Soil Specifications ................................................................................................ 42 7. References .................................................................................................................................... 52 “Upon this handful of soil our survival depends. Husband it and it will grow our food, our fuel, and our shelter and surround us with beauty. Abuse it and the soil will collapse and die, taking humanity with it.” From Vedas Sanskrit Scripture – circa 1500 BC The aim of this Technical Information Note is to assist Landscape Professionals (primarily landscape architects) when considering matters in relation to soils and soil-forming material. Soil is an essential requirement for providing -
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020
REGENERATIVE AGRICULTURE and the SOIL CARBON SOLUTION SEPTEMBER 2020 AUTHORED BY: Jeff Moyer, Andrew Smith, PhD, Yichao Rui, PhD, Jennifer Hayden, PhD REGENERATIVE AGRICULTURE IS A WIN-WIN-WIN CLIMATE SOLUTION that is ready for widescale implementation now. WHAT ARE WE WAITING FOR? Table of Contents 3 Executive Summary 5 Introduction 9 A Potent Corrective 11 Regenerative Principles for Soil Health and Carbon Sequestration 13 Biodiversity Below Ground 17 Biodiversity Above Ground 25 Locking Carbon Underground 26 The Question of Yields 28 Taking Action ACKNOWLEDGMENTS 30 Soil Health for a Livable Future Many thanks to the Paloma Blanca Foundation and Tom and Terry Newmark, owners of Finca Luna Nueva Lodge and regenerative farm in 31 References Costa Rica, for providing funding for this paper. Tom is also the co-founder and chairman of The Carbon Underground. Thank you to Roland Bunch, Francesca Cotrufo, PhD, David Johnson, PhD, Chellie Pingree, and Richard Teague, PhD for providing interviews to help inform the paper. EXECUTIVE SUMMARY The environmental impacts of agricultural practices This introduction is co-authored by representatives of two The way we manage agricultural land 140 billion new tons of CO2 contamination to the blanket of and translocation of carbon from terrestrial pools to formative organizations in the regenerative movement. matters. It matters to people, it matters to greenhouse gases already overheating our planet. There is atmospheric pools can be seen and felt across a broad This white paper reflects the Rodale Institute’s unique our society, and it matters to the climate. no quarreling with this simple but deadly math: the data are unassailable. -
The Soil Fertility and Drainage Indexes: 2 United States Forest Service, Fort Collins, CO Taxonomically Based, Ordinal Estimates of Relative Soil Properties Bradley A
1 Michigan State University, East Lansing, MI The Soil Fertility and Drainage Indexes: 2 United States Forest Service, Fort Collins, CO taxonomically based, ordinal estimates of relative soil properties Bradley A. Miller1, Randall J. Schaetzl1, Frank Krist Jr.2 Validation of the Soil Fertility Index Among other validation approaches with different data sets, 2009 crop yield data for 11 Midwestern states were used to evaluate the FI. In a GIS, we determined the soils and crops in particular fields, and thus were able to ascertain the mean FI value per soil, per crop, per county. These crop specific, mean, county level FI values were then compared with the county yield values reported by USDA-NASS. Statewide summaries of these data produced correlations among yields of specific crops and FI values that were all positive. Below are selected examples. Illinois Crop Rs value Corn 0.73 Soybeans 0.75 Winter Wheat 0.78 Minnesota Crop Rs value Corn 0.29 Soybeans 0.23 Oats 0.80 Sugar Beets 0.24 Low Soil Fertility Index Soil Drainage Index This poster introduces a new, ordinally based, Soil Fertility Index (FI). The above map shows the FI for the lower 48 states. The FI uses family-level The map above shows the natural, inherent, soil wetness of the lower 48 states, as determined by the ordinally based Soil Taxonomy information, i.e., interpretations of taxonomic features or properties that tend to be associated with natural low or high soil Natural Soil Drainage Index (DI). The DI is intended to reflect the amount of water that a soil can supply to growing plants under Wisconsin fertility, to rank soils from 0 (least fertile) to 19 (most fertile). -
The Soil Food Web
THE SOIL FOOD WEB HEALTHY SOIL HEALTHY ENVIRONMENT The Soil Food Web Alan Sundermeier Extension Educator and Program Leader, Wood County Extension, The Ohio State University. Vinayak Shedekar Postdoctural Researcher, The Ohio State University. A healthy soil depends on the interaction of many organisms that make up the soil food web. These organisms live all or part of their life cycle in the soil and are respon- sible for converting energy as one organism consumes another. Source: Soil Biology Primer The phospholipid fatty acid (PLFA) test can be used to measure the activity of the soil food web. The following chart shows that mi-crobial activity peaks in early summer when soil is warm and moisture is adequate. Soil sampling for detecting soil microbes should follow this timetable to better capture soil microbe activity. The soil food web begins with the ener- gy from the sun, which triggers photo- synthesis in plants. Photosynthesis re- sults in plants using the sun’s energy to fix carbon dioxide from the atmosphere. This process creates the carbon and organic compounds contained in plant material. This is the first trophic level. Then begins building of soil organic matter, which contains both long-last- ing humus, and active organic matter. Active organic matter contains readily available energy, which can be used by simple soil organisms in the second trophic level of the soil food web. Source: Soil Biology Primer SOILHEALTH.OSU.EDU THE SOIL FOOD WEB - PAGE 2 The second trophic level contains simple soil organisms, which Agriculture can enhance the soil food web to create more decompose plant material. -
Soil Ph and Soil Fertility
Soil pH and Soil Fertility Dave Wilson Research Agronomist March 7, 2013 Environmental factors influencing plant growth – Which can we manage? 1. Temperature 2. Moisture Supply 3. Radiant Energy (Sunlight: quality, intensity & duration) 4. Composition of the atmosphere 5. Gas content of the soil 6. Soil reaction (Soil pH) Degree of acidity or alkalinity 7. Biotic factors (Plant variety type- genetics, soil biology) 8. Supply of mineral nutrient elements What is pH? • pH can be viewed as an abbreviation for Power of concentration of Hydrogen ion in solution • pH = - [log (H+)] in solution, The pH of a soil is a measure of hydrogen ion activity or concentration ([H+]) in the soil solution. Impact of soil PH changes As the H+ activity increases, soil pH decreases. As the soil pH decreases, most desirable crop nutrients become less available while others, often undesirable, become more available and can reach toxic levels. Total pH scale: 0 ------------------------------ 7 -------------------------------- 14 Acid Neutral Basic or Alkaline The relative availability of Nutrients as a function of pH Color coded chart of relative nutrient availability with change in pH. The darker the blue the more available the nutrient Logarithmic Scale of pH Total pH scale: 10x 0 ---1----2----3----4-----5-----6----- 7 -----8-----9----10-----11-----12-----13--- 14 100x Acid Neutral Basic or Alkaline • Hydrogen activity is mathematically expressed as a negative logarithm: • pH = -log[H+]. Because of the logarithmic scale, one unit decrease in pH implies a 10 -
Soil Life in Reconstructed Ecosystems: Initial Soil Food Web Responses After Rebuilding a Forest Soil Profile for a Climate Change Experiment
Soil life in reconstructed ecosystems: Initial soil food web responses after rebuilding a forest soil profile for a climate change experiment Paul T. Rygiewicza,*, Vicente J. Monleonb, Elaine R. Inghamc, Kendall J. Martind, Mark G. Johnsona ABSTRACT Disrupting ecosystem components. while transferring and reconstructing them for experiments can produce myriad responses. Establishing the extent of these biological responses as the system approaches a new equilibrium allows us more reliably to emulate comparable native systems. That is, the sensitivity of analyzing ecosystem processes in a reconstructed system is improved by excluding the period when observed phenomena are primarily responses caused by establishing the experiment rather than effects of imposed treatments; achieved by determining the extent of any pulse of activity caused by preparatory procedures. A native forest soil was physically disrupted when it was collected. sieved. and then rebuilt in lysimeters in a controlled-environment study evaluating the influence of elevated atmospheric CO2 concentration and elevated atmospheric temperature on the reconstructed soil that was planted with Douglas-fir (Pseudotsugo menziesii Mirb. Franco) seedlings. Generally. soil food web populations responded in two phases during the exposure as indicated by preliminary evaluation of the 4.5-year dataset. Also. previous work indicated that relatively elevated soil CO2 effluxes occurred during the first phase. suggesting that food web populations may have responded to carbon sources made available when the soil was harvested and its profile reconstructed in the lysimeters, Results are presented for bacterial and fungal biomass. numbers of protozoa and nematodes to gain insight on whether the first phase responses are attributable to the acute stress of physically disrupting the soil. -
Sustainable Soil Management
Top of Form ATTRAv2 page skip navigation 500 500 500 500 500 0 Search Bottom of Form 800-346-9140 Home | Site Map | Who We Are | Contact (English) Us | Calendar | Español | Text Only 800-411-3222 (Español) Home > Master Publication List > Sustainable Soil Management What Is Sustainable Soil Management Sustainable Agriculture? The printable PDF version of the Horticultural By Preston Sullivan entire document is available at: Crops NCAT Agriculture Specialist http://attra.ncat.org/attra- © NCAT 2004 pub/PDF/soilmgmt.pdf Field Crops ATTRA Publication #IP027/133 31 pages — 1.5 mb Download Acrobat Reader Soils & Compost Water Management Pest Management Organic Farming Livestock Marketing, Business & Risk Abstract Soybeans no-till planted into Management wheat stubble. This publication covers basic soil Photo by: Preston Sullivan Farm Energy properties and management steps toward building and maintaining healthy soils. Part I deals with basic Education soil principles and provides an understanding of living soils and how they work. In this section you will find answers to why soil organisms Other Resources and organic matter are important. Part II covers management steps to build soil quality on your farm. The last section looks at farmers who Master have successfully built up their soil. The publication concludes with a Publication List large resource section of other available information. Table of Contents Top of Form Part I. Characteristics of Sustainable Soils o Introduction o The Living Soil: Texture and Structure o The Living Soil: The Importance of Soil Organisms 1011223551022 o Organic Matter, Humus, and the Soil Foodweb o Soil Tilth and Organic Matter oi o Tillage, Organic Matter, and Plant Productivity o Fertilizer Amendments and Biologically Active Soils Go o Conventional Fertilizers Enter your o Top$oil—Your Farm'$ Capital email above o Summary of Part I and click Go. -
Soil Microbiology
Module 5 TAKING CARE OF OUR PLANET • Unit 1 PLANET EARTH IS IN THE DANGER ZONE SOIL MICROBIOLOGY 1 Read the following text and decide which of these adjectives could be used instead of those underlined in the passage: abundant, available, better, big, dangerous, entire, minute, productive, several, supreme, useful, vital. Inorganic constituents (minerals, water, process that crop residues, grass clippings, air), dead organic matter and soil life are leaves, organic wastes, etc., are decomposed the components that make up the total soil and converted to forms useable for plant environment. The living portion of the soil can growth as well as converted to stable soil be divided into macro- and micro-organisms. organic matter called ‘humus’. Macro-organisms play an important role in The large organisms function as grinders in organic decomposition by chewing plant that they reduce the particle size of organic and animal residues into fine particles. residues making them more accessible and Though the micro-organic portion represents decomposable by the soil microbes. The soil considerably less than 1% of the soil mass, it microbial population also further decomposes is on this tiny fraction that the continued re- the waste products of the larger animals. cycling of nutrients mainly depends. Thus, the activities of different groups of soil Normal, fertile soils teem with soil microbes. organisms are linked in complex “food webs”. The most numerous microbes in soil are the One beneficial process carried out exclusively bacteria followed by the actinomycetes, the by soil microbes is called nitrogen fixation, the fungi, soil algae and cyanobacteria (“blue- capture of inert N2 gas (dinitrogen) from the air green algae”) and soil protozoa.