Developmental History of Soil Concepts Froma Scientific Perspective
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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. -
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. -
Progressive and Regressive Soil Evolution Phases in the Anthropocene
Progressive and regressive soil evolution phases in the Anthropocene Manon Bajard, Jérôme Poulenard, Pierre Sabatier, Anne-Lise Develle, Charline Giguet- Covex, Jeremy Jacob, Christian Crouzet, Fernand David, Cécile Pignol, Fabien Arnaud Highlights • Lake sediment archives are used to reconstruct past soil evolution. • Erosion is quantified and the sediment geochemistry is compared to current soils. • We observed phases of greater erosion rates than soil formation rates. • These negative soil balance phases are defined as regressive pedogenesis phases. • During the Middle Ages, the erosion of increasingly deep horizons rejuvenated pedogenesis. Abstract Soils have a substantial role in the environment because they provide several ecosystem services such as food supply or carbon storage. Agricultural practices can modify soil properties and soil evolution processes, hence threatening these services. These modifications are poorly studied, and the resilience/adaptation times of soils to disruptions are unknown. Here, we study the evolution of pedogenetic processes and soil evolution phases (progressive or regressive) in response to human-induced erosion from a 4000-year lake sediment sequence (Lake La Thuile, French Alps). Erosion in this small lake catchment in the montane area is quantified from the terrigenous sediments that were trapped in the lake and compared to the soil formation rate. To access this quantification, soil processes evolution are deciphered from soil and sediment geochemistry comparison. Over the last 4000 years, first impacts on soils are recorded at approximately 1600 yr cal. BP, with the erosion of surface horizons exceeding 10 t·km− 2·yr− 1. Increasingly deep horizons were eroded with erosion accentuation during the Higher Middle Ages (1400–850 yr cal. -
IMPROVING AGRICULTURAL RESILIENCE to CLIMATE CHANGE THROUGH SOIL MANAGEMENT Peningkatan Ketahanan Pertanian Terhadap Perubahan Iklim Melalui Pengelolaan Tanah
ImprovingJ. Litbang agricultural Pert. Vol. resilience 32 No. to2 Juniclimate 2013: change ....-.... .... (Fahmuddin Agus et al.) 147 IMPROVING AGRICULTURAL RESILIENCE TO CLIMATE CHANGE THROUGH SOIL MANAGEMENT Peningkatan Ketahanan Pertanian terhadap Perubahan Iklim melalui Pengelolaan Tanah Fahmuddin Agus, Husnain, and Rahmah Dewi Yustika Indonesian Soil Research Institute Jalan Tentara Pelajar No. 12, Bogor 16114, Indonesia Phone. (0251) 8336757, Fax. (0251) 8321608 E-mail: [email protected]; [email protected] Diterima: 29 Maret 2015; Direvisi: 7 Oktober 2015; Disetujui: 21 Oktober 2015 ABSTRACT musim hujan dan musim kemarau yang sulit diduga, dan penurunan atau kenaikan jumlah curah hujan merupakan kondisi yang tidak menguntungkan yang dapat memengaruhi pertumbuhan dan Climate change affects soil properties and hence crop growth. produksi tanaman. Beberapa pendekatan, baik secara tunggal atau Several soil management practices potentially reduce vulnerability kombinasi dari dua atau lebih tindakan, bisa dipilih untuk to unfavorable climate conditions. This paper reviews how climate beradaptasi dengan perubahan iklim. Ini termasuk olah tanah change affects soil properties and how should soil management be konservasi, konservasi tanah vegetatif dan mekanis, penggunaan tailored to increase adaptation capacity to extreme climatic mulsa, pemanenan air, pengelolaan hara, ameliorasi tanah, dan conditions. The main symptoms of climate change such as the manajemen biologi tanah. Pengelolaan bahan organik tanah sangat increase in the global atmospheric temperature, unpredictable sentral dalam praktik pengelolaan tanah karena bahan organik onset of the wet and dry seasons and excessive or substantial tanah berperan penting dalam meningkatkan kapasitas tanah decrease in rainfall are unfavorable conditions that affect crop memegang air, meningkatkan kapasitas infiltrasi dan perkolasi growth and production. -
Soil Resilience and Sustainability of Semi-Arid and Humid Tropical Soils of India: a Commentary*
Agropedology 2016, 26 (01), 1-9 Soil Resilience and Sustainability of Semi-Arid and Humid Tropical Soils of India: A Commentary* M. Velayutham1* and D.K. Pal2 1Former Director, Indian Council of Agricultural Research-National Bureau of Soil Survey and Land Use Planning (NBSS&LUP), Nagpur, India; and Former Executive Director, M.S. Swaminathan Research Foundation, Chennai, India. 2Former Head, Division of Soil Resource Studies, NBSS&LUP, Nagpur, India and Visiting Scientist, ICRISAT, Hyderabad, India. Introduction Historic non - resilient soil situation leading to abandoning of the site, due to man-made soil degradation has Soil is a dynamic and living natural resource, which been recorded as in the collapse of Harappan civilization of supports to produce goods and services of value to humans the Indo-Gangetic Plains. In present times we are witnessing but not necessarily with perpetual ability against the it in the shifting cultivation areas of North - East India, by the degradative processes. It is well known that soil formation is rapidity with which old sites are abandoned and new sites are a slow process, and a substantial amount of soil can form only chosen for cultivation. over a geologic timescale. Soil misuse and extreme climatic conditions can damage self-regulating capacity and give way A wealth of soil information has been developed by to regressive pedogenesis (Pal et al. 2013), and thus might the NARS, state government departments and ISRO. Pal lead to the soil to regress from higher to lower usefulness and et al. (2000), Bhattacharyya et al. (2013) have given a or drastically diminished productivity. -
A Review on the Interactive Exploration of Soil Health and How to Improve It to Boost Crop Production
International Journal of Innovative Agriculture & Biology Research 7(1):39-46, Jan.-Mar., 2019 © SEAHI PUBLICATIONS, 2019 www.seahipaj.org ISSN: 2354- 2934 A Review on the Interactive Exploration of Soil Health and How to Improve It to Boost Crop Production Mohammed D. Toungos (Ph.D.) Department Of Crop Science , Adamawa State University Mubi, Adamawa State, Nigeria Corresponding Author Email: [email protected]; [email protected] ABSTRACT Soil health is becoming so important these days as a result of more and more, producers are understanding that healthy soils are more productive and lead to healthier crops. This led to more about sustainable production practices that can help build healthy soil that can sustain the production of healthier crops to the populace. These can be achieved by exploring the on-farm benefits of using cover crops, crop rotation, manure amendments, composting and more on the complex web of life below the surface of the soil in order to improve them. Soil management encompasses a number of strategies used by farmers and ranchers to protect soil resources, one of their most valuable assets. By practicing soil conservation, including appropriate soil preparation methods, they reduce soil erosion and increase soil stabilization. Soil health is a state of a soil meeting its range of ecosystem functions as appropriate to its environment. Soil health testing is an assessment of this status. Soil health depends on soil biodiversity (with a robust soil biota), and it can be improved via soil conditioning. The underlying principle in the use of the term ―soil health‖ is that soil is not just an inert, lifeless growing medium, which modern farming tends to represent, rather it is a living, dynamic and ever-so-subtly changing whole environment. -
Sustaining the Pedosphere: Establishing a Framework for Management, Utilzation and Restoration of Soils in Cultured Systems
Sustaining the Pedosphere: Establishing A Framework for Management, Utilzation and Restoration of Soils in Cultured Systems Eugene F. Kelly Colorado State University Outline •Introduction - Its our Problems – Life in the Fastlane - Ecological Nexus of Food-Water-Energy - Defining the Pedosphere •Framework for Management, Utilization & Restoration - Pedology and Critical Zone Science - Pedology Research Establishing the Range & Variability in Soils - Models for assessing human dimensions in ecosystems •Studies of Regional Importance Systems Approach - System Models for Agricultural Research - Soil Water - The Master Variable - Water Quality, Soil Management and Conservation Strategies •Concluding Remarks and Questions Living in a Sustainable Age or Life in the Fast Lane What do we know ? • There are key drivers across the planet that are forcing us to think and live differently. • The drivers are influencing our supplies of food, energy and water. • Science has helped us identify these drivers and our challenge is to come up with solutions Change has been most rapid over the last 50 years ! • In last 50 years we doubled population • World economy saw 7x increase • Food consumption increased 3x • Water consumption increased 3x • Fuel utilization increased 4x • More change over this period then all human history combined – we are at the inflection point in human history. • Planetary scale resources going away What are the major changes that we might be able to adjust ? • Land Use Change - the world is smaller • Food footprint is larger (40% of land used for Agriculture) • Water Use – 70% for food • Running out of atmosphere – used as as disposal for fossil fuels and other contaminants The Perfect Storm Increased Demand 50% by 2030 Energy Climate Change Demand up Demand up 50% by 2030 30% by 2030 Food Water 2D View of Pedosphere Hierarchal scales involving soil solid-phase components that combine to form horizons, profiles, local and regional landscapes, and the global pedosphere. -
Evolution Education Around the Globe Evolution Education Around the Globe
Hasan Deniz · Lisa A. Borgerding Editors Evolution Education Around the Globe Evolution Education Around the Globe [email protected] Hasan Deniz • Lisa A. Borgerding Editors Evolution Education Around the Globe 123 [email protected] Editors Hasan Deniz Lisa A. Borgerding College of Education College of Education, Health, University of Nevada Las Vegas and Human Services Las Vegas, NV Kent State University USA Kent, OH USA ISBN 978-3-319-90938-7 ISBN 978-3-319-90939-4 (eBook) https://doi.org/10.1007/978-3-319-90939-4 Library of Congress Control Number: 2018940410 © Springer International Publishing AG, part of Springer Nature 2018 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. -
Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis C
Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis C. Laveuf, Sophie Cornu, Denis Baize, Michel Hardy, Olivier Josière, Sylvain Drouin, Ary Bruand, F. Juillot To cite this version: C. Laveuf, Sophie Cornu, Denis Baize, Michel Hardy, Olivier Josière, et al.. Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis. Pedosphere, Elsevier, 2009, 19 (3), pp.292-304. 10.1016/S1002-0160(09)60120-X. insu-00403877 HAL Id: insu-00403877 https://hal-insu.archives-ouvertes.fr/insu-00403877 Submitted on 21 Nov 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Zinc Redistribution in a Soil Developed from Limestone During Pedogenesis∗1 C. LAVEUF1,∗2,S.CORNU1, D. BAIZE1, M. HARDY1, O. JOSIERE1, S. DROUIN2, A. BRUAND2 and F. JUILLOT3 1INRA, UR0272 Science du Sol, Centre de recherche d’Orl´eans, 45075 Orl´eans cedex 2 (France) 2ISTO, UMR 6113, CNRS, Universit´ed’Orl´eans, 45071 Orl´eans cedex 2 (France) 3IMPMC, UMR CNRS 7590, Universit´e Paris 6 et 7, IPGC, 75252 Paris cedex 05 (France) (Received November 20, 2008; revised March 23, 2009) ABSTRACT The long-term redistribution of Zn in a naturally Zn-enriched soil during pedogenesis was quantified based on mass balance calculations. -
Soil Health Principles for Organic Production Systems
SOIL HEALTH PRINCIPLES FOR ORGANIC PRODUCTION SYSTEMS OUR APPROACH UNDERSTANDING SOIL HEALTH Iroquois Valley takes a systems-based approach to soil health, recognizing Iroquois Valley works with organic that soil health principles work together to maintain and improve soil and transitioning farmers because of function, and aims for continuous improvement over time. We work their commitment to the environment with a diverse set of farms, from grains production to agroforestry, and and human health. The USDA Organic our soil health principles were developed to be adapted to each. Standard requires that a certified operation must work to maintain or Iroquois Valley’s operations strive to improve soil health through seven improve natural resources, including principles: soil. Iroquois Valley’s farmers use natural processes and materials to manage their operations closer to how a natural system would. Our farmers use the shared intent of greater Eliminating soil health captured in both the Integrating livestock chemical Organic Standard and the Soil Health disturbance Principles for Organic Production to guide their management decisions. Iroquois Valley’s certified organic Keeping Appropriate farmer partners know that soil is a continuous use of living roots tillage living system that is integral to their SOIL operation. They use the knowledge HEALTH gained from one season to inform management decisions for the next, cumulatively leading to greater soil Maximizing Appropriate health over time. Our farmers see soil plant biological health as a continuous improvement diversity disturbance process and part of an overall system of management, not as a checklist Providing and of practices. The exact portfolio of maintaining practices implemented will vary from soil cover farm to farm as do soil types and the natural resources vary from place to place. -
Saitta, ET, Gelernter, R., & Vinther, J
Saitta, E. T., Gelernter, R., & Vinther, J. (2018). Additional information on the primitive contour and wing feathering of paravian dinosaurs. Palaeontology, 61(2), 273-288. https://doi.org/10.1111/pala.12342 Peer reviewed version Link to published version (if available): 10.1111/pala.12342 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via Wiley at http://onlinelibrary.wiley.com/doi/10.1111/pala.12342/abstract . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Additional information on the primitive contour and wing feathering of paravian dinosaurs Evan T. Saitta1, Rebecca Gelernter2, & Jakob Vinther1,3 1School of Earth Sciences, University of Bristol, Bristol, United Kingdom; e-mails: [email protected] (ORCiD ID: orcid.org/0000-0002-9306-9060), [email protected] (ORCiD ID: orcid.org/0000-0002-3584-9616) 2Near Bird Studios, New Haven, Connecticut, USA; e-mail: [email protected] 3School of Biological Sciences, University of Bristol, Bristol, United Kingdom ABSTRACT: Identifying feather morphology in extinct dinosaurs is challenging due to dense overlapping of filaments within fossilized plumage and the fact that some extinct feather morphologies are unlike those seen in extant birds or those predicted from an ‘evo-devo’ model of feather evolution. -
Science Destroys the Evolutionary Paradigm
SCIENCE DESTROYS THE EVOLUTIONARY PARADIGM An Inservice Manual for Young-Earth Creationists Free Images – Snappygoat.com Materialistic Naturalism, an Immoral and Incoherent Philosophy!!! Dr. Jim Pagels – 4/18/2018 1 For as the heavens are higher than the earth, so are my ways higher than your ways and my thoughts than your thoughts. For as the rain and the snow come down from heaven and do not return there but water the earth, making it bring forth and sprout, giving seed to the sower and bread to the eater, so shall my word be that goes out from my mouth; it shall not return to me empty, but it shall accomplish that which I purpose, and shall succeed in the thing for which I sent it. Isaiah 55:9-11 This book along with its predecessors including Apologetic Resources, Lesson Plans for Biblical Apologetics and Touching Lives through Apologetics, a Counseling Perspective are offered free for personal and professional use in ministry, being available as downloads on the Michigan District website under schools-curriculum. Scriptural references are typically taken from the English Standard Version (ESV) although the King James Version (KJV) is also periodically utilized. 2 Contents Acknowledgements………………………………………………………………………..…….5 Preface…………………………………………………………………………………………...6 Intended Audience ……………………………………………………………………………....8 Inservice Perspective……….…………………………………………………………….……..9 Inservice Questionnaire……………………………………………………………..…………10 1. Evolution, an Attack on the Supernatural Nature of God…………………………………..21 2. In Search of Truth…………………………………………………………………………..23 3. Creation Apologetics, Simple for Some, Incomprehensible to Others………..……..…….35 4. Two Typical Approaches to Young Earth Creationism……………………………………38 5. The Absolute Veracity of the Supernatural…………………….…………………………..40 6. A Tactical Approach to Creationism………………………….………………………..…..43 7.