Unit 1.1, Managing Soil Health
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Topic: Soil Classification
Programme: M.Sc.(Environmental Science) Course: Soil Science Semester: IV Code: MSESC4007E04 Topic: Soil Classification Prof. Umesh Kumar Singh Department of Environmental Science School of Earth, Environmental and Biological Sciences Central University of South Bihar, Gaya Note: These materials are only for classroom teaching purpose at Central University of South Bihar. All the data/figures/materials are taken from several research articles/e-books/text books including Wikipedia and other online resources. 1 • Pedology: The origin of the soil , its classification, and its description are examined in pedology (pedon-soil or earth in greek). Pedology is the study of the soil as a natural body and does not focus primarily on the soil’s immediate practical use. A pedologist studies, examines, and classifies soils as they occur in their natural environment. • Edaphology (concerned with the influence of soils on living things, particularly plants ) is the study of soil from the stand point of higher plants. Edaphologist considers the various properties of soil in relation to plant production. • Soil Profile: specific series of layers of soil called soil horizons from soil surface down to the unaltered parent material. 2 • By area Soil – can be small or few hectares. • Smallest representative unit – k.a. Pedon • Polypedon • Bordered by its side by the vertical section of soil …the soil profile. • Soil profile – characterize the pedon. So it defines the soil. • Horizon tell- soil properties- colour, texture, structure, permeability, drainage, bio-activity etc. • 6 groups of horizons k.a. master horizons. O,A,E,B,C &R. 3 Soil Sampling and Mapping Units 4 Typical soil profile 5 O • OM deposits (decomposed, partially decomposed) • Lie above mineral horizon • Histic epipedon (Histos Gr. -
Basic Soil Science W
Basic Soil Science W. Lee Daniels See http://pubs.ext.vt.edu/430/430-350/430-350_pdf.pdf for more information on basic soils! [email protected]; 540-231-7175 http://www.cses.vt.edu/revegetation/ Well weathered A Horizon -- Topsoil (red, clayey) soil from the Piedmont of Virginia. This soil has formed from B Horizon - Subsoil long term weathering of granite into soil like materials. C Horizon (deeper) Native Forest Soil Leaf litter and roots (> 5 T/Ac/year are “bio- processed” to form humus, which is the dark black material seen in this topsoil layer. In the process, nutrients and energy are released to plant uptake and the higher food chain. These are the “natural soil cycles” that we attempt to manage today. Soil Profiles Soil profiles are two-dimensional slices or exposures of soils like we can view from a road cut or a soil pit. Soil profiles reveal soil horizons, which are fundamental genetic layers, weathered into underlying parent materials, in response to leaching and organic matter decomposition. Fig. 1.12 -- Soils develop horizons due to the combined process of (1) organic matter deposition and decomposition and (2) illuviation of clays, oxides and other mobile compounds downward with the wetting front. In moist environments (e.g. Virginia) free salts (Cl and SO4 ) are leached completely out of the profile, but they accumulate in desert soils. Master Horizons O A • O horizon E • A horizon • E horizon B • B horizon • C horizon C • R horizon R Master Horizons • O horizon o predominantly organic matter (litter and humus) • A horizon o organic carbon accumulation, some removal of clay • E horizon o zone of maximum removal (loss of OC, Fe, Mn, Al, clay…) • B horizon o forms below O, A, and E horizons o zone of maximum accumulation (clay, Fe, Al, CaC03, salts…) o most developed part of subsoil (structure, texture, color) o < 50% rock structure or thin bedding from water deposition Master Horizons • C horizon o little or no pedogenic alteration o unconsolidated parent material or soft bedrock o < 50% soil structure • R horizon o hard, continuous bedrock A vs. -
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. -
National University of Engineering Ge111
NATIONAL UNIVERSITY OF ENGINEERING COLLEGE OF ENVIRONMENTAL ENGINEERING ENVIRONMENTAL ENGINEERING PROGRAM GE111 – EDAPHOLOGY I. GENERAL INFORMATION CODE : GE111 – Edaphology SEMESTER : 5 CREDITS : 03 HOURS PER WEEK : 04 (Theory – Practices – Laboratory) PREREQUISITES : GE102 – Geography CONDITION : Mandatory II. COURSE DESCRIPTION Concept and importance of edaphological soil and its interest for Engineering. Detailed knowledge of the components, physical and chemical properties, genesis, classification and principles of cartography, of natural soils and anthropogenic urban soils. Principle of soil evaluation, as a starting point in studies of environmental planning, territorial planning and environmental impact assessment. Finally, it is intended that students understand the importance of soil as a non-renewable resource and the degradations to which its inappropriate use leads; It is also intended to train in the corrective and rehabilitating measures of degraded soils. III. COURSE OUTCOMES At the end of the course the student will: Organizes data for proper analysis and interpretation and calculations (soil densities, physical chemical and biological properties). Explains and determines the genesis of the soil, the physical properties of the soil, geo reference, physiographic units. Understand and apply densities, to determine the consistency of the soil, the probability of resistance in an earthquake. Interpret and perform types of soil sampling to take to the laboratory to determine their physical, chemical, and biological characteristics. Build models to determine the degree of contamination, is determined by the parameters, using the LMOs, ECAs, In soils. IV. LEARNING UNITS 1. SOIL GENESIS / 4 HOURS Objective of soil science: Interest in Engineering. Genesis. Pedological and edaphological approach. Factors of soil formation. Climate action. Properties of the soil affected by the climate. -
Dynamics of Carbon 14 in Soils: a Review C
Radioprotection, Suppl. 1, vol. 40 (2005) S465-S470 © EDP Sciences, 2005 DOI: 10.1051/radiopro:2005s1-068 Dynamics of Carbon 14 in soils: A review C. Tamponnet Institute of Radioprotection and Nuclear Safety, DEI/SECRE, CADARACHE, BP. 1, 13108 Saint-Paul-lez-Durance Cedex, France, e-mail: [email protected] Abstract. In terrestrial ecosystems, soil is the main interface between atmosphere, hydrosphere, lithosphere and biosphere. Its interactions with carbon cycle are primordial. Information about carbon 14 dynamics in soils is quite dispersed and an up-to-date status is therefore presented in this paper. Carbon 14 dynamics in soils are governed by physical processes (soil structure, soil aggregation, soil erosion) chemical processes (sequestration by soil components either mineral or organic), and soil biological processes (soil microbes, soil fauna, soil biochemistry). The relative importance of such processes varied remarkably among the various biomes (tropical forest, temperate forest, boreal forest, tropical savannah, temperate pastures, deserts, tundra, marshlands, agro ecosystems) encountered in the terrestrial ecosphere. Moreover, application for a simplified modelling of carbon 14 dynamics in soils is proposed. 1. INTRODUCTION The importance of carbon 14 of anthropic origin in the environment has been quite early a matter of concern for the authorities [1]. When the behaviour of carbon 14 in the environment is to be modelled, it is an absolute necessity to understand the biogeochemical cycles of carbon. One can distinguish indeed, a global cycle of carbon from different local cycles. As far as the biosphere is concerned, pedosphere is considered as a primordial exchange zone. Pedosphere, which will be named from now on as soils, is mainly located at the interface between atmosphere and lithosphere. -
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 -
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). -
Demonstration of Physical Separation/Leaching Methods for the Remediation of Heavy Metals Contaminated Soils at Small Arms Ranges
84 4 0 ,;*v , DEMONSTRATION OF PHYSICAL ftsJS1:3«*s SEPARATION/LEACHING METHODS FOR THE REMEDIATION OF HEAVY waBHi METALS CONTAMINATED SOILS AT SMALL ARMS RANGES m &r<&S?GtXl WBTMBUTION BTATEMEHTT Approved for pntfelie r*l«u«*f Dürtrlbattoa UnHmtaKl M£3 SEPTEMBER 1997 19980M 177 flTIC QUALITY DTS^EOTED S This Document Contains Missing Page/s That Are Unavailable In The Original Document AEC Form <t5, 1 Feb 93 replaces THAMA Form <t5 which is obsolete. Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Weshington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188), Washington, DC 20503. 1. AGENCY USE ONLY (Leave blank) REPORT DATE 3. REPORT TYPE AND DATES COVERED September 1997 Technology Demonstration, Nov 1995-Sep 1997 4. TITLE AND SUBTITLE 5. FUNDING NUMBERS Demonstration of Physical Separation/Leaching Methods for the Remediation of Heavy Metals Contaminated Soils at Small Arms Ranges 6. AUTHOR(S) BDM Engineering Services Company 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION BDM Engineering Services Company REPORT NUMBER 1801 Randolph Road, S.E. -
Soil Quality Characteristics As Affected by Continuous Rice Cultivation
agriculture Article Soil Quality Characteristics as Affected by Continuous Rice Cultivation and Changes in Cropping Systems in South China Xiangning Ren 1,2,3, Feixiang Chen 1,2,3, Tao Ma 1,2 and Yueming Hu 1,2,3,4,* 1 College of Natural Resources and Environment, South China Agricultural University, Guangzhou 510642, China; [email protected] (X.R.); [email protected] (F.C.); [email protected] (T.M.) 2 Guangdong Provincial Key Laboratory of Land Use and Consolidation, Guangzhou 510642, China 3 South China Academy of Natural Resources Science and Technology, Guangzhou 510610, China 4 State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, Xining 810016, China * Correspondence: [email protected]; Tel.: +86-186-8888-2020; Fax: +86-20-8528-3140 Received: 12 August 2020; Accepted: 23 September 2020; Published: 30 September 2020 Abstract: This study was conducted to elucidate how changes in critical soil quality characteristics relate to continuous rice cultivation and changes in cropping systems and fertilization in South China over the time span 1980 to 2017. Soil pH, soil organic matter (SOM), total nitrogen (TN), available phosphorus (AP) and potassium (AK) were determined for the samples taken in 2017 and compared to results from the paired samples collected in 1980 by grouping all samples into four cropping systems: continuous paddy fields, new paddy fields developed from uplands, continuous uplands, and new uplands developed from paddy soils. The results show a significant increase in soil pH, AP and AK in all cropping systems, which was, however, coupled with low fertilizer use efficiency. -
Behavior of Pesticides in Soils and Water 1
Archival copy: for current recommendations see http://edis.ifas.ufl.edu or your local extension office. SL 40 Behavior of Pesticides in Soils and Water 1 P.S.C. Rao and A.G. Hornsby2 During the past twenty years, concern has arisen applied, and to show how this information can be as to the presence of pesticides in the environment used, along with other factors, to select the proper and the threat they pose to wildlife and mankind. pesticide. Certainly, pesticides have improved longevity and the quality of life, chiefly in the area of public health. PATHWAYS OF PESTICIDE LOSS The use of pesticides also constitutes an important There are basically two ways properly-applied aspect of modern agriculture. Florida's temperate to pesticides may reach surface and ground waters- subtropical climate favors growth of many harmful through runoff and leaching. Runoff is the physical insects, weeds and diseases, thus making this state transport of pollutants over the ground surface by particularly dependent on pesticides for economical rainwater which does not penetrate the soil. Leaching crop management. is a process whereby pollutants are flushed through Unfortunately, pesticides are poisons and can be the soil by rain or irrigation water as it moves particularly dangerous when misused. Fish-kills, downward. In many areas of Florida, soils are sandy reproductive failure in birds, and acute illnesses in and permeable and leaching is likely to be a more people have all been attributed to exposure to or serious problem than runoff. We now have ingestion of pesticides - usually as a result of technology to help estimate the potential misapplication or careless disposal of unused contamination of water from a given pesticide.