Agricultural Soil Carbon Credits: Making Sense of Protocols for Carbon Sequestration and Net Greenhouse Gas Removals
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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. -
1 the Background for Carbon Finance and Carbon Credits
CHAPTER 1 THE BACKGROUND FOR CARBON FINANCE AND CARBON CREDITS THE LINK BETWEEN CLIMATE CHANGE, GHG EMISSIONS, AGRICULTURE AND FORESTRY Climate change is one of the biggest threats we face. Everyday activities like driving a car or a motorbike, using air conditioning and/or heating and lighting houses consume energy and produce emissions of greenhouse gases (GHG), which contribute to climate change. When the emissions of GHGs are rising, the Earth’s climate is affected, the average weather changes and average temperatures increase. FIGURE 1 Sources of agricultural GHGs in megatons (Mt) CO2-eq 2128 1792 672 616 369 158 410 CO2 CO2 CH 413 CH4+ N2O 4 CO2 + N2O Irrigation N02 Farm Rice machinery Biomass production CH4 N0 +CH burning 2 4 Fertiliser production Nitrous oxide from fertilised soils + land conversion Manure to agriculture 5900 Mt CO2-eq Methane from cattle enteric fermentation Source: Greenpeace International, 2008. In agriculture and forestry different sources and sinks release, take up and store three types of GHGs: carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O). Many agricultural and forestry practices emit GHGs to the atmosphere. Figure 1 shows the main sources of agricultural GHGs: for example, by using fertilizers N2O is released from the soil and by burning agricultural residues CO2 levels rise. CH4 is set free in the digestion 1 ] process of livestock, as well as if rice is grown under flooded conditions. When land is converted to cropland and trees are felled, a source of CO2 emissions is created. Agriculture is an important contributor to climate change, but it also provides a sink and has the potential to lessen climate change. -
Carbon Dioxide Removal Policy in the Making: Assessing Developments in 9 OECD Cases
POLICY AND PRACTICE REVIEWS published: 04 March 2021 doi: 10.3389/fclim.2021.638805 Carbon Dioxide Removal Policy in the Making: Assessing Developments in 9 OECD Cases Felix Schenuit 1,2*, Rebecca Colvin 3, Mathias Fridahl 4, Barry McMullin 5, Andy Reisinger 6, Daniel L. Sanchez 7, Stephen M. Smith 8, Asbjørn Torvanger 9, Anita Wreford 10 and Oliver Geden 2 1 Center for Sustainable Society Research, University of Hamburg, Hamburg, Germany, 2 German Institute for International and Security Affairs (SWP), Berlin, Germany, 3 Crawford School of Public Policy, Australian National University, Canberra, ACT, Australia, 4 Department of Thematic Studies, Environmental Change, Centre for Climate Science and Policy Research, Linköping University, Linköping, Sweden, 5 Dublin City University, Dublin, Ireland, 6 Ministry for the Environment, Wellington, New Zealand, 7 Department of Environmental Science, Policy, and Management (ESPM), University of California, Berkeley, Berkeley, CA, United States, 8 Smith School of Enterprise and the Environment, Oxford University, Oxford, United Kingdom, 9 Center for International Climate Research (CICERO), Oslo, Norway, 10 Agribusiness and Economics Research Unit (AERU), Lincoln University, Christchurch, New Zealand Edited by: William C. Burns, Since the adoption of the Paris Agreement in 2015, spurred by the 2018 IPCC Special American University, United States Report on Global Warming of 1.5◦C, net zero emission targets have emerged as a Reviewed by: new organizing principle of climate policy. In this context, climate policymakers and Phillip Williamson, University of East Anglia, stakeholders have been shifting their attention to carbon dioxide removal (CDR) as United Kingdom an inevitable component of net zero targets. The importance of CDR would increase Charithea Charalambous, Heriot-Watt University, further if countries and other entities set net-negative emissions targets. -
Ecological Restoration for Protected Areas Principles, Guidelines and Best Practices
Ecological Restoration for Protected Areas Principles, Guidelines and Best Practices Prepared by the IUCN WCPA Ecological Restoration Taskforce Karen Keenleyside, Nigel Dudley, Stephanie Cairns, Carol Hall and Sue Stolton, Editors Peter Valentine, Series Editor Developing capacity for a protected planet Best Practice Protected Area Guidelines Series No.18 IUCN WCPA’s BEST PRACTICE PROTECTED AREA GUIDELINES SERIES IUCN-WCPA’s Best Practice Protected Area Guidelines are the world’s authoritative resource for protected area managers. Involving collaboration among specialist practitioners dedicated to supporting better implementation in the field, they distil learning and advice drawn from across IUCN. Applied in the field, they are building institutional and individual capacity to manage protected area systems effectively, equitably and sustainably, and to cope with the myriad of challenges faced in practice. They also assist national governments, protected area agencies, non- governmental organisations, communities and private sector partners to meet their commitments and goals, and especially the Convention on Biological Diversity’s Programme of Work on Protected Areas. A full set of guidelines is available at: www.iucn.org/pa_guidelines Complementary resources are available at: www.cbd.int/protected/tools/ Contribute to developing capacity for a Protected Planet at: www.protectedplanet.net/ IUCN PROTECTED AREA DEFINITION, MANAGEMENT CATEGORIES AND GOVERNANCE TYPES IUCN defines a protected area as: A clearly defined geographical space, -
Port Silt Loam Oklahoma State Soil
PORT SILT LOAM Oklahoma State Soil SOIL SCIENCE SOCIETY OF AMERICA Introduction Many states have a designated state bird, flower, fish, tree, rock, etc. And, many states also have a state soil – one that has significance or is important to the state. The Port Silt Loam is the official state soil of Oklahoma. Let’s explore how the Port Silt Loam is important to Oklahoma. History Soils are often named after an early pioneer, town, county, community or stream in the vicinity where they are first found. The name “Port” comes from the small com- munity of Port located in Washita County, Oklahoma. The name “silt loam” is the texture of the topsoil. This texture consists mostly of silt size particles (.05 to .002 mm), and when the moist soil is rubbed between the thumb and forefinger, it is loamy to the feel, thus the term silt loam. In 1987, recognizing the importance of soil as a resource, the Governor and Oklahoma Legislature selected Port Silt Loam as the of- ficial State Soil of Oklahoma. What is Port Silt Loam Soil? Every soil can be separated into three separate size fractions called sand, silt, and clay, which makes up the soil texture. They are present in all soils in different propor- tions and say a lot about the character of the soil. Port Silt Loam has a silt loam tex- ture and is usually reddish in color, varying from dark brown to dark reddish brown. The color is derived from upland soil materials weathered from reddish sandstones, siltstones, and shales of the Permian Geologic Era. -
Pacific Biochar What Is Biochar?
Soil Health & Carbon Farming Charlie McIntosh, Pacific Biochar What is Biochar? Biochar: biomass charcoal when used or found in soils Biochar + Soil Health SOIL ORGANIC MATTER ! Biochar is a natural component of soil organic matter ! Seasonal fires deposit biochar in soils where it accumulates over time ! People have used biochar to improve soils for millenia (ex. Terra Preta soils of the Amazon Basin) ! Fertile soils around the world often contain high levels of biochar ~30-50% of SOM Photo courtesy of Julie Major and Bruno Glaser Biochar forms a portion of the “Stabilized Organic Matter” pool in soils Biochar + Soil Health SOIL BIOLOGY ! Biochar provides an ideal micro- habitat for soil organisms ! Porous surfaces retain air, water and nutrients available for microorganisms and root hairs ! Studies consistently demonstrate enhanced biological activity in soils & composting using biochar Photo showing microstructure of biochar particle and Photo showing the organic coating formed on biochar fungal hyphae extending from spore, courtesy of Ogawa surfaces and pores, courtesy of Yoshizawa Biochar + Soil Health WATER & NUTRIENT CONSERVATION ! Biochar acts like a sponge ! Micropores retain moisture while macropores allow drainage ! Improves plant available water in sandy and heavy clay soils ! Biochar acts like a filter ! Reduces leaching & volatilization of nutrients, especially nitrogen Biochar + Compost COMPOST QUALITY ! Biochar-amended compost improves compost quality and maturity while the biochar is improved by microbe colonization and -
This Ubiquitous Carbon…
Engineering Physics Department Presents Dr. Cristian Contescu Senior Research Staff, Materials Science and Technology Division Oak Ridge National Laboratory This ubiquitous carbon… Abstract: After Stone Age, Bronze Age, and Iron Age, and after the Silicon Age of the informational revolution, the technologies of 21st century are marked by the ubiquitous presence of various forms of carbon allotropes. For a very long time, diamond and graphite were the only known carbon allotropes, but that has changed with the serendipitous discovery of fullerenes, carbon nanotubes, and graphene. Every ten or fifteen years scientists unveil new forms of carbons with new and perplexing properties, while computations suggest that the carbon’s family still has members unknown to us today. At a dramatically accelerated pace, new carbon forms find their place at the leading edge of scientific and technological innovations. At the same time traditional forms of carbon are being used in new and exciting applications that make our life safer, healthier, and more enjoyable. The 21st century may soon be recognized as the Age of Carbon forms. This educational talk will show how carbon, the fourth most abundant element in the Galaxy and the basis of life on Earth, was the engine of most important technological developments throughout the history of civilization. It will emphasize the ability of carbon atoms to generate a variety of mutual combinations and with many other chemical elements. These properties have placed carbon at the core of numerous inventions that define our civilization, while emerging new technologies open a rich path for value-added products in today’s market. -
Properties of Carbon the Atomic Element Carbon Has Very Diverse
Properties of Carbon The atomic element carbon has very diverse physical and chemical properties due to the nature of its bonding and atomic arrangement. fig. 1 Allotropes of Carbon Some allotropes of carbon: (a) diamond, (b) graphite, (c) lonsdaleite, (d–f) fullerenes (C60, C540, C70), (g) amorphous carbon, and (h) carbon nanotube. Carbon has several allotropes, or different forms in which it can exist. These allotropes include graphite and diamond, whose properties span a range of extremes. Despite carbon's ability to make 4 bonds and its presence in many compounds, it is highly unreactive under normal conditions. Carbon exists in 2 main isotopes: 12C and 13C. There are many other known isotopes, but they tend to be short-lived and have extremely short half-lives. Allotropes The different forms of a chemical element. Cabon is the chemical element with the symbol C and atomic number 6. As a member of group 14 on the periodic table, it is nonmetallic and tetravalent—making four electrons available to form covalent chemical bonds. Carbon has 6 protons and 6 Source URL: https://www.boundless.com/chemistry/nonmetallic-elements/carbon/properties-carbon/ Saylor URL: http://www.saylor.org/courses/chem102#6.1 Attributed to: Boundless www.saylor.org Page 1 of 2 neutrons, and has a standard atomic weight of 12.0107 amu. Its electron configuration is denoted as 1s22s22p2. It is a solid, and sublimes at 3,642 °C. It's oxidation state ranges from 4 to -4, and it has an electronegativity rating of 2.55 on the Pauling scale. Carbon has several allotropes, or different forms in which it exists. -
Agricultural Soil Compaction: Causes and Management
October 2010 Agdex 510-1 Agricultural Soil Compaction: Causes and Management oil compaction can be a serious and unnecessary soil aggregates, which has a negative affect on soil S form of soil degradation that can result in increased aggregate structure. soil erosion and decreased crop production. Soil compaction can have a number of negative effects on Compaction of soil is the compression of soil particles into soil quality and crop production including the following: a smaller volume, which reduces the size of pore space available for air and water. Most soils are composed of • causes soil pore spaces to become smaller about 50 per cent solids (sand, silt, clay and organic • reduces water infiltration rate into soil matter) and about 50 per cent pore spaces. • decreases the rate that water will penetrate into the soil root zone and subsoil • increases the potential for surface Compaction concerns water ponding, water runoff, surface soil waterlogging and soil erosion Soil compaction can impair water Soil compaction infiltration into soil, crop emergence, • reduces the ability of a soil to hold root penetration and crop nutrient and can be a serious water and air, which are necessary for water uptake, all of which result in form of soil plant root growth and function depressed crop yield. • reduces crop emergence as a result of soil crusting Human-induced compaction of degradation. • impedes root growth and limits the agricultural soil can be the result of using volume of soil explored by roots tillage equipment during soil cultivation or result from the heavy weight of field equipment. • limits soil exploration by roots and Compacted soils can also be the result of natural soil- decreases the ability of crops to take up nutrients and forming processes. -
Advanced Crop and Soil Science. a Blacksburg. Agricultural
DOCUMENT RESUME ED 098 289 CB 002 33$ AUTHOR Miller, Larry E. TITLE What Is Soil? Advanced Crop and Soil Science. A Course of Study. INSTITUTION Virginia Polytechnic Inst. and State Univ., Blacksburg. Agricultural Education Program.; Virginia State Dept. of Education, Richmond. Agricultural Education Service. PUB DATE 74 NOTE 42p.; For related courses of study, see CE 002 333-337 and CE 003 222 EDRS PRICE MF-$0.75 HC-$1.85 PLUS POSTAGE DESCRIPTORS *Agricultural Education; *Agronomy; Behavioral Objectives; Conservation (Environment); Course Content; Course Descriptions; *Curriculum Guides; Ecological Factors; Environmental Education; *Instructional Materials; Lesson Plans; Natural Resources; Post Sc-tondary Education; Secondary Education; *Soil Science IDENTIFIERS Virginia ABSTRACT The course of study represents the first of six modules in advanced crop and soil science and introduces the griculture student to the topic of soil management. Upon completing the two day lesson, the student vill be able to define "soil", list the soil forming agencies, define and use soil terminology, and discuss soil formation and what makes up the soil complex. Information and directions necessary to make soil profiles are included for the instructor's use. The course outline suggests teaching procedures, behavioral objectives, teaching aids and references, problems, a summary, and evaluation. Following the lesson plans, pages are coded for use as handouts and overhead transparencies. A materials source list for the complete soil module is included. (MW) Agdex 506 BEST COPY AVAILABLE LJ US DEPARTMENT OFmrAITM E nufAT ION t WE 1. F ARE MAT IONAI. ItiST ifuf I OF EDuCATiCiN :),t; tnArh, t 1.t PI-1, t+ h 4t t wt 44t F.,.."11 4. -
Drummer Illinois State Soil
Drummer Illinois State Soil Soil Science Society of America Introduction Many states have designated state symbols such as bird, flower, fish, tree, rock, and more. Many states also have a state soil – one that has significance or is important to the state. As there are many types of birds, flowers, and trees, there are hundreds of soil types in our state but Drummer is the official state soil of Illinois. How important is the Drummer soil to Illinois? History Drummer was first established as a type of soil in Ford County in 1929. It was named after Drummer Creek in Drummer Township. 1n 1987, Drummer was selected as the state soil by the Illinois Soil Classifiers Association over other soils such as Cisne, Flanagan, Hoyleton, Ipava, Sable, and Saybrook. Since then, Drummer has been repeatedly chosen by other as- sociations who work with soil. In 1992, the Illinois Association of Vocational Agriculture Teachers sponsored a state soil election in their classrooms and Drummer won by a margin of 2 to 1. In 1993, the statewide 4H Youth Conference also selected Drummer out of 6 nomi- nees. Also in 1993 at the FFA state convention, Drummer and Ipava were tied in the contest. Finally, in 2001, after many attempts, it was finally passed by the Illinois Legislature and signed into law by Governor George Ryan. What is Drummer Soil? It is the most common among the dark colored soils or “black dirt” of Illinois. The dark color is due to the high amount of organic matter inherited from the decomposition of the prairie vegetation that is growing on the soil. -
Soil Organic Carbon Scoping Paper
DISCUSSION PAPER Standardized GHG Accounting for Soil Organic Carbon Accrual on Non-Forest Lands: Challenges and Opportunities September 23, 2019 Discussion Paper for Soil Organic Carbon Accrual September 23, 2019 About this document This paper is meant to take stock of the current “state of play” with respect to the creation of tradable offsets to incentivize building soil carbon in non-forested soils. The document discusses the potential for developing a carbon offset protocol for soil organic carbon (SOC) accrual. The document first discusses challenges, including quantification, permanence and additionality. Then, new technologies and approaches are presented as options to overcome the challenges, and there is a short overview of how some offset programs are addressing SOC. We conclude the document with a general description of the approaches that could be used in a Reserve SOC protocol. Executive summary Soil organic carbon (SOC) sequestration practices have a high potential for GHG emission reductions, but these practices remain underutilized by carbon offset programs due to several challenges, including costs, uncertainty, permanence, and additionality. This document evaluates the potential for developing a Reserve SOC accrual protocol that is applicable to the United States, Mexico, and Canada. Potential practices would increase carbon stocks mainly in cropland and grassland, and would include conservation tillage, efficient irrigation, sustainable grazing, nutrient management, and cover-cropping. There are several technologies in use and in development to achieve certain and cost-effective quantification at varying degrees. Traditional lab-based dry combustion methods combined with bulk density tests are the gold standard for SOC quantification, but direct sampling and laboratory analysis are costly and time intensive.