Soil Physics and Agricultural Production
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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. -
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. -
Effects of Climatic Change on Soil Hydraulic Properties During
water Article Effects of Climatic Change on Soil Hydraulic Properties during the Last Interglacial Period: Two Case Studies of the Southern Chinese Loess Plateau Tieniu Wu 1,2 , Henry Lin 2, Hailin Zhang 1,*, Fei Ye 1, Yongwu Wang 1, Muxing Liu 1, Jun Yi 1 and Pei Tian 1 1 Key Laboratory for Geographical Process Analysis & Simulation, Hubei Province, Central China Normal University, Wuhan 430079, China; [email protected] (T.W.); [email protected] (F.Y.); [email protected] (Y.W.); [email protected] (M.L.); [email protected] (J.Y.); [email protected] (P.T.) 2 Department of Ecosystem Science and Management, The Pennsylvania State University, University Park, PA 16802, USA; [email protected] * Correspondence: [email protected]; Tel.: +86-27-6786-7503 Received: 16 January 2020; Accepted: 10 February 2020; Published: 12 February 2020 Abstract: The hydraulic properties of paleosols on the Chinese Loess Plateau (CLP) are closely related to agricultural production and are indicative of the environmental evolution during geological and pedogenic periods. In this study, two typical intact sequences of the first paleosol layer (S1) on the southern CLP were selected, and soil hydraulic parameters together with basic physical and chemical properties were investigated to reveal the response of soil hydraulic properties to the warm and wet climate conditions. The results show that: (1) the paleoclimate in the southern CLP during the last interglacial period showed a pattern of three warm and -
Soil Carbon Losses Due to Increased Cloudiness in a High Arctic Tundra Watershed (Western Spitsbergen)
SOIL CARBON LOSSES DUE TO INCREASED CLOUDINESS IN A HIGH ARCTIC TUNDRA WATERSHED (WESTERN SPITSBERGEN) Christoph WŸthrich 1, Ingo Mšller 2 and Dietbert Thannheiser2 1. Department of Geography, University of Basel, Spalenring 145, CH-4055 Basel, Switzerland; e-mail: [email protected]. 2. Department of Geography, University of Hamburg, Bundesstr. 55, D-20146 Hamburg, Germany. Abstract Carbon pool and carbon flux measurements of different habitats were made in the high Arctic coastal tundra of Spitsbergen. The studied catchment was situated on the exposed west coast, where westerly winds produce daily precipitation in form of rain, drizzle and fog. The storage of organic carbon in the catchment of Eidembukta amounts to 5.98 kg C m-2, mainly within the lower horizons of deep soils. Between 5.2 - 23.6 % of the carbon pool is stored in plant material. During the cold and cloudy summer of 1996, net CO2 flux measure- ments showed carbon fluxes from soil to atmosphere even during the brightest hours of the day. We estimate -2 -1 that the coastal tundra of Spitsbergen lost carbon at a rate of 0.581 g C m d predominantly as CO2-C. Carbon loss (7.625 mg C m-2 d-1) as TOC in small tundra rivers accounts only for a small proportion (1.31 %) of the total carbon loss. Introduction tetragona, Betula nana, and Empetrum hermaphroditum might accompany warming on Spitsbergen (WŸthrich, Large terrestrial carbon pools are found in the peat- 1991; Thannheiser, 1994; Elvebakk and Spjelkavik, lands of the boreal and subpolar zones that cover in 1995). -
Fundamentals of Geoenvironmental Engineering
NPTEL – Civil – Geoenvironmental Engineering Module 1 FUNDAMENTALS OF GEOENVIRONMENTAL ENGINEERING A) Scope of geoenvironmental engineering Any project that deals with the interrelationship among environment, ground surface and subsurface (soil, rock and groundwater) falls under the purview of geoenvironmental engineering (Fang and Daniels 2006). The scope is vast and requires the knowledge of different branches of engineering and science put together to solve the multi-disciplinary problems. A geoenvironmental engineer should work in an open domain of knowledge and should be willing to use any concepts of engineering and science to effectively solve the problem at hand. The most challenging aspect is to identify the unconventional nature of the problem, which may have its bearing on multiple factors. For example, an underground pipe leakage may not be due to the faulty construction of the pipe but caused due to the highly corrosive soil surrounding it. The reason for high corrosiveness may be attributed to single or multiple manmade factors, which need to be clearly identified for the holistic solution of the problem. The conventional approach of assessing the material strength of the pipe alone will not solve the problem at hand. A lot of emphasis has been laid for achieving a “green environment”. Despite a lot of effort, it is very difficult to cut off the harmful effects of pollutants disposed off into the geoenvironment. The damage has already been done to the subsurface and ground water resources, which is precious. An effective waste containment system is one of the solutions to this problem. However, such a project has different socio-economic and technical perspectives. -
Effects of Soil Health Management on Soil and Water Relations Paul Salon, Plant Materials Specialist, USDA-NRCS Big Flats Plant Materials Center 3266, Rt
The Effects of Soil Health Management on Soil and Water Relations Paul Salon, Plant Materials Specialist, USDA-NRCS Big Flats Plant Materials Center 3266, Rt. 352, Corning, NY 14830 Soil health, sometimes referred to as soil quality, is defined as the continued capacity of soil to function as a vital living ecosystem that sustains plants, animals, and humans. Soils have inherent characteristics or qualities which are not readily changed by management. These would include the soil texture, depth to impermeable layers and position in the landscape. Within these parameters a soil’s performance can be improved by maintaining and improving its health which can be done by following good soil health management practices. Only "living" things can have health, so viewing soil as a living ecosystem reflects a fundamental shift in the way we care for our soils. Soil is not an inert growing medium, but rather is teaming with billions of bacteria, fungi, and other microbes that are the foundation of a symbiotic ecosystem. One gram of soil can contain over 1 billion micro-organisms. The physical nature of a typical mineral soil contains about 50% solid particles and 50% pores on a volume basis. The pore space is made up of varying amounts of air and water. In mineral soils, of the 50% solid portion about 45 - 48% is minerals. Soil texture refers to the mineral component of the soil in terms of the proportion of small, medium, and large particles (clay, silt, and sand, respectively) in a specific soil mass. The larger the particle size the more permeable and the lower the water holding capacity is; and the more organic matter is needed to affect soil water relations. -
Introduction to Soil Physics - S.W
AGRICULTURAL SCIENCES – Vol. I - Introduction to Soil Physics - S.W. Duiker and D.D. Fritton INTRODUCTION TO SOIL PHYSICS S.W. Duiker and D.D. Fritton The Department of Crop and Soil Sciences, Pennsylvania State University, Pennsylvania, USA. Keywords: Soil physics, soil texture, organic matter, bulk density, porosity, infiltration, water holding capacity, soil temperature, erosion, compaction, irrigation, drainage, water use efficiency, systems approach, interdisciplinary Contents 1. The beginning of soil physics 2. Contemporary soil physics 2.1. Theory of soil physics 2.1.1. Solid phase 2.1.2. Liquid phase 2.1.3. Gaseous phase 2.1.4. Heat flow and temperature 2.2. Applications of soil physics 2.2.1. Soil erosion 2.2.2. Soil organic matter management 2.2.3. Soil compaction 2.2.4. Irrigation 2.2.5. Drainage 2.2.6. Water use efficiency 3. The future of soil physics Glossary Bibliography Biographical Sketches Summary Soil physics is the study of the solid, liquid, and gaseous phases of soils and of fluxes of fluids and energy in soils. The solid phase consists of mineral and organic matter. The dominantUNESCO liquid in soils is water, and the– dominant EOLSS gases are similar to those in the atmosphere, except that soils contain more CO2 and water vapor and less O2. Interactions between the three phases in soils determine the movement of fluids and energy. Soil physicsSAMPLE established itself as a scientific CHAPTERS discipline in the early 20th century. Much progress has been made since then in the characterization of the physical properties and processes in soils. -
Effect of Environmental Factors on Pore Water Pressure
Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 416 Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Påverkan av miljöfaktorer på porvattentryck i flodbanksediment, Sollefteå, Sverige Hanna Fritzson INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 416 Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Påverkan av miljöfaktorer på porvattentryck i flodbanksediment, Sollefteå, Sverige Hanna Fritzson ISSN 1650-6553 Copyright © Hanna Fritzson Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2017 Abstract Effect of Environmental Factors on Pore Water Pressure in River Bank Sediments, Sollefteå, Sweden Hanna Fritzson Pore water pressure in a silt slope in Sollefteå, Sweden, was measured from 2009-2016. The results from 2009-2012 were presented and evaluated in a publication by Westerberg et al. (2014) and this report is an extension of that project. In a silt slope the pore water pressures are generally negative, contributing to the stability of the slope. In this report the pore water pressure variations are analyzed using basic statistics and a connection between the pore water pressure variations, the geology and parameters such as temperature, precipitation and soil moisture are discussed. The soils in the slope at Nipuddsvägen consists of sandy silt, silt, clayey silt and silty clay. The main findings were that at 2, 4 and 6 m depth there are significant increases and decreases in the pore water pressure that can be linked with the changing of the seasons, for example there is a significant increase in the spring when the ground frost melts. -
Part 533 – Geotechnical Engineering
Title 210 – National Engineering Manual Part 533 – Geotechnical Engineering Subpart C – Operations 533.20 General A. Soil mechanics is a branch of soil physics and engineering mechanics that describes the behavior of soils and provides the theoretical basis for analysis in geotechnical engineering. Soil mechanics is the application of the laws and principles of mechanics and hydraulics to engineering problems dealing with soil as an engineering material. The testing of soil’s properties are typically done at a testing laboratory with specialized equipment or can be measured or correlated in the field. Soil mechanics is a subdivision of civil engineering and engineering geology that evaluates the action of forces within a soil mass for natural or artificial structures that are supported on or made of soil. B. Collection and analysis of geotechnical engineering data are essential in the investigation and design of engineering structures. The examination and verification of soil properties during construction are critical. Specialized training and experience in geotechnical engineering are needed due to the many factors which depend on interpretation and judgment of soil related issues. Close coordination is needed between the investigation, soil testing, design, and construction functions. C. Soil mechanics testing provides data for evaluating soil and rock as engineering materials for planning, design, and construction. Test results identify the index, chemical, and engineering properties used in the analysis and design of foundations and earth or earth-supported structures such as dams, buildings, bridge foundations, retaining walls, as well as the support structure of buried pipeline systems. 533.21 Data Collection A. The engineering staff or team that prepares the final design will assist in planning of the geotechnical site investigation, sample selection, and final soil testing program. -
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. -
The Soil Story Curricular Guide
THE SOIL STORY CURRICULUM Rebuilding Healthy Soil for Carbon Cycle Balance Earth’s Systems Photosynthesis Healthy Soil Lead Authors: Whitney Cohen | Education Director, Life Lab Food & Farming Carrie Strohl, PhD | Educational Consultant Taking Action Contributors: Annie Martin | Business Program, Kiss the Ground Arlae Castellanos | Sustainability Tracking Program Manager, Green Schools Alliance Craig Macmillan, PhD | Technical Program Manager, Vinyard Team Didi Pershouse | Director, Learning Resources Don Smith | Storytelling Team, Kiss the Ground Emily Harris, PhD | Research Scientist, BSCS Science Learning Finian Makepeace | Co-Founder, Kiss the Ground Ilana Lowe | 5th Grade Lead Science Teacher, Main Street Elementary Jessica Handy, RDN | Education Program, Kiss the Ground Karen Rodriguez | Former Operations Manager, Kiss the Ground A Middle School Lauren Tucker | Executive Director, Kiss the Ground Curriculum by Leslie Rogers | Director of Education, Atlas Organics Liz Henry | Senior Consultant, Crecer Strategies Markos Major | Director, Climate Action Now Paul Hawken | Author and Environmentalist Designer: Michelle Uyeda | Graphic Designer, Kiss the Ground + Thank you to our sponsors: About 1 THE SOIL STORY CURRICULAR GUIDE The Soil Story Curricular Guide was created through a collaborative partnership between Kiss the Ground and Life Lab. It serves as a supplemental material for teaching middle schoolers Next Generation Science Standards. Kiss the Ground (KTG) is a nonprofit with a mission to inspire participation in the regeneration of the planet, beginning with soil. The organization creates educational curriculum, campaigns, and media to raise awareness and empower individuals to purchase food that supports health soils and a balanced climate. KTG also works with farmers, educators, non government organizations, scientists, students, and policymakers to advocate for regenerative agriculture, raise funds to train farmers, and help brands and businesses to invest in healthy soils. -
Soil Erosion in Humid Regions: a Review Daniel J
48 UNIVERSITIES COUNCIL ON WATER RESOURCES JOURNAL OF CONTEMPORARY WATER RESEARCH & EDUCATION ISSUE 154, PAGES 48-59, APRIL 2015 Soil Erosion in Humid Regions: A Review Daniel J. Holz1, *Karl W.J. Williard1, Pamela J. Edwards2, and Jon E. Schoonover1 1Southern Illinois University, Carbondale, IL 2USDA Forest Service, Northern Research Station, Parsons, WV *Corresponding Author Abstract: Soil erosion has significant implications for land productivity and surface water quality, as sediment is the leading water pollutant worldwide. Here, erosion processes are defined. The dominant factors influencing soil erosion in humid areas are reviewed, with an emphasis on the roles of precipitation, soil moisture, soil porosity, slope steepness and length, vegetation, and soil organisms. Erosion dynamics in forested watersheds are the focus with some examples from agricultural watersheds included as well. Lastly, best management practices for controlling surface erosion are discussed. Keywords: best management practices, erosion control, forest, precipitation, sediment, surface erosion, water quality, watershed management rosion is a critical process for land and activates the second step of the erosion process, watershed managers to understand, as particle transport (Rose 1960; Savat and Poesen Esediment is the world’s leading surface 1981). Deposition is the third and final step in the water pollutant. Excessive erosion results in erosion process and occurs simultaneously with significant topsoil losses, leading to declines in the first two steps (Huang et al. 1999). When the agricultural productivity. Reservoir lifespans sediment load of moving water is greater than its can be shortened due to excessive sedimentation transport capacity, deposition occurs (Foster and behind dams. Sediment can carry bound nutrients Meyer 1972).