Synthesis of Short- and Long-Term Studies Reporting Soil Quality
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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. -
A Mathematical Representation of Microalgae
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-359 Manuscript under review for journal Biogeosciences Discussion started: 14 September 2017 c Author(s) 2017. CC BY 4.0 License. A mathematical representation of microalgae distribution in aridisol and water scarcity Abdolmajid Lababpour1 1Department of Mechanical Engineering, Shohadaye Hoveizeh University of Technology, Dasht-e Azadeghan, 64418-78986, 5 Iran Correspondence to: Abdolmajid Lababpour ([email protected]) Abstract. The restoration technologies of biological soil crust (BSC) in arid and semi-arid areas can be supported by simulations performed by mathematical models. The present study represents a mathematical model to describe behaviour of the complex microalgae development on the soil surface. A diffusion-reaction system was used in the model formulation which 10 incorporating parameters of photosynthetic organisms, soil water content and physical parameter of soil porosity, extendable for substrates and exchanged gases. For the photosynthetic microalgae, the dynamic system works as a batch mode, while input and output are accounted for soil water-limited substrate. The coupled partial differential equations (PDEs) of model were solved by numerical finite-element method (FEM) after determining model parameters, initial and boundary conditions. The MATLAB features, were used in solving and simulation of model equations. The model outputs reveals that soil water 15 balance shift in microalgae inoculated lands compare to bare lands. Refining and application of the model for the biological soil stabilization and the biocrust restoration process will provide us with an optimized mean for biocrust restoration activities and success in the challenge with land degradation, regenerating a favourable ecosystem state, and reducing dust emission- related problems in the arid and semi-arid areas of the world. -
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. -
Response of Soil Respiration to Drying and Rewetting
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 12, 8723–8745, 2015 www.biogeosciences-discuss.net/12/8723/2015/ doi:10.5194/bgd-12-8723-2015 BGD © Author(s) 2015. CC Attribution 3.0 License. 12, 8723–8745, 2015 This discussion paper is/has been under review for the journal Biogeosciences (BG). Response of soil Please refer to the corresponding final paper in BG if available. respiration to drying and rewetting Response of respiration and nutrient Q. Sun et al. availability to drying and rewetting in soil from a semi-arid woodland depends on Title Page vegetation patch and a recent wild fire Abstract Introduction Conclusions References 1 1 1 2 Q. Sun , W. S. Meyer , G. Koerber , and P. Marschner Tables Figures 1Department of Ecology and Environmental Science, School of Biological Sciences, The University of Adelaide, Adelaide, SA 5005, Australia J I 2 Soils, School of Agriculture, Food and Wine, The University of Adelaide, Adelaide, SA 5005, J I Australia Back Close Received: 16 April 2015 – Accepted: 23 May 2015 – Published: 12 June 2015 Full Screen / Esc Correspondence to: Q. Sun ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 8723 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract BGD Semi-arid woodlands, which are characterised by patchy vegetation interspersed with bare, open areas, are frequently exposed to wild fire. During summer, long dry peri- 12, 8723–8745, 2015 ods are occasionally interrupted by rainfall events. It is well-known that rewetting of dry 5 soil induces a flush of respiration. -
Pedogenic Gypsum of Southern New Mexico: Genesis, Morphology, and Stable Isotopic Signature
UNLV Retrospective Theses & Dissertations 1-1-2000 Pedogenic gypsum of southern New Mexico: Genesis, morphology, and stable isotopic signature John Grant Van Hoesen University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/rtds Repository Citation Van Hoesen, John Grant, "Pedogenic gypsum of southern New Mexico: Genesis, morphology, and stable isotopic signature" (2000). UNLV Retrospective Theses & Dissertations. 1186. http://dx.doi.org/10.25669/cudd-yb7b This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Retrospective Theses & Dissertations by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print colored or poor quality illustrations and photographs, print bieedthrough, substandard margins, arxl improper alignment can adversely affect reproduction. -
Land Use and Climatic Factors Structure Regional Patterns in Soil Microbialcommunities Rebecca E
John Carroll University Carroll Collected Biology 2010 Land use and climatic factors structure regional patterns in soil microbialcommunities Rebecca E. Drenovsky John Carroll University, [email protected] Kerri L. Steenworth Louise E. Jackson Kate M. Scow Follow this and additional works at: http://collected.jcu.edu/biol-facpub Part of the Biology Commons, and the Plant Sciences Commons Recommended Citation Drenovsky, Rebecca E.; Steenworth, Kerri L.; Jackson, Louise E.; and Scow, Kate M., "Land use and climatic factors structure regional patterns in soil microbialcommunities" (2010). Biology. 20. http://collected.jcu.edu/biol-facpub/20 This Article is brought to you for free and open access by Carroll Collected. It has been accepted for inclusion in Biology by an authorized administrator of Carroll Collected. For more information, please contact [email protected]. RESEARCH Land use and climatic factors structure PAPER regional patterns in soil microbial communitiesgeb_486 27..39 Rebecca E. Drenovsky1*, Kerri L. Steenwerth2, Louise E. Jackson3 and Kate M. Scow3 1Biology Department, John Carroll University, ABSTRACT 20700 North Park Boulevard, University Aim Although patterns are emerging for macroorganisms, we have limited under- Heights, OH 44118 USA, 2USDA/ARS, Crops Pathology and Genetics Research Unit, Davis, standing of the factors determining soil microbial community composition and CA 95616, USA, 3Department of Land, Air productivity at large spatial extents. The overall objective of this study was to and Water Resources, University of California, discern the drivers of microbial community composition at the extent of biogeo- Davis, One Shields Avenue, Davis, CA 95616 graphical provinces and regions. We hypothesized that factors associated with land USA use and climate would drive soil microbial community composition and biomass. -
Soils – Fundamental Concepts
NRCS Soil: Fundamental Concepts Scoop on Soil Educational CD May 2006 Soils – Fundamental Concepts The Soil In Perspective: A fundamental knowledge of soil science is a prerequisite to meeting the many natural resource challenges that will face humanity in the 21st Century. It is also true that the study of soils can be both fascinating and intellectually satisfying. It is in the soils that we are able to observe all of the principles of biology, chemistry, and physics at work. It is the understanding of these principles which enables us to minimize the degradation and destruction of one of our most important natural resources. Much of our life’s activities and pursuits are related to and influenced by the behavior of the soil around our houses, roads, septic and sewage disposal systems, airports, parks, farms, forests, schools, and shopping centers. It is essential that conservation professionals understand the soils on which we build and design and work. In any field of natural resources, it is important to understand the soil properties which impact the application of technology as we use it to preserve and protect our most basic natural resource, our soils. Soil Defined: We have several definitions of soil depending on the discipline providing the definition: Geologic definition – loose surface of the earth as distinguished from solid bedrock. (Support of plant life not required) Traditional definition – material which nourishes and supports growing plants. (Includes rocks, water, snow, and even air – all of which are capable of supporting plant life) Component definition – mixture of mineral matter, organic matter, water and air. -
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 Food Web: Implications to Soil Health
Soil Food Web: Implications to Soil Health Dr. Sajeemas “Mint” Pasakdee, Soil Scientist/Agronomist Advisor, Student Operated Organic Farm CIT-Jordan College of Agri. Sci. & Tech., Fresno State 1 Outline • Soil organisms and their interactions • What do soil organisms do? • Where do soil organisms live? • Food web structure • When are soil organisms active? • How is the food web measured? • Living soils—Bacteria; Fungi; Earthworms • Soil Environment 2 Organisms & Their Interaction 3 4 What do soil organisms do? Soil organisms support plant health as • decompose organic matter, • cycle nutrients, • enhance soil structure, • control the populations of soil organisms including crop pests. 5 Organic Matter • Food sources for soil organisms • Agricultural top soil ~1-6% (In CA, ~1-3% SOM) 6 Where do soil organisms live? • Around roots(rhizosphere) • Plant litter (C sources) • Humus (stabilized organic matter) • Surface of soil aggregates 7 Typical Food Web Structure • bacterial-dominated food webs o Grassland & Agri Soils o Ratio of fungi to bacteria, ~1:1 for productive agri. soils • fungal-dominated food webs o Ratio of fungal to bacterial, ~5:1 to 10:1 in a deciduous forest and 100:1 to 1000:1 in a coniferous forest 8 9 When are soil organisms active? 10 How is the food web measured? • Counting. Organism groups (bacteria, protozoa, arthropods, etc.); or subgroups (bacterial-feeding, fungal-feeding, and predatory nematodes), are counted and through calculations, can be converted to biomass. • Measuring activity levels. The amount of by-products, i.e., respiration (CO2); nitrification and decomposition rates • Measuring cellular constituents. Biomass carbon, nitrogen, or phosphorus; Enzymes; Phospholipids and other lipids; DNA and RNA 11 12 Soil Bacteria • One-celled organisms – generally 4/100,000 of an inch wide (1 µm) • A teaspoon of productive soil generally contains between 100 million and 1 billion bacteria (~two cows per acre). -
Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UNL | Libraries University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 2012 Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico Stephen A. Hall Red Rock Geological Enterprises, Santa Fe, NM, [email protected] Ronald J. Goble University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Hall, Stephen A. and Goble, Ronald J., "Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico" (2012). Papers in the Earth and Atmospheric Sciences. 325. https://digitalcommons.unl.edu/geosciencefacpub/325 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Berino Paleosol, Late Pleistocene Argillic Soil Development on the Mescalero Sand Sheet in New Mexico Stephen A. Hall1,* and Ronald J. Goble2 1. Red Rock Geological Enterprises, 3 Cagua Road, Santa Fe, New Mexico 87508, U.S.A.; 2. Department of Earth and Atmospheric Sciences, 214 Bessey Hall, University of Nebraska, Lincoln, Nebraska 68588, U.S.A. ABSTRACT The Berino paleosol is the first record of a directly dated Aridisol in the American Southwest where paleoclimatic conditions during the time of pedogenesis can be estimated. -
Soil Health and Global Sustainability: Translating Science Into Practice
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. Department of Agriculture: Agricultural Publications from USDA-ARS / UNL Faculty Research Service, Lincoln, Nebraska January 2002 Soil health and global sustainability: translating science into practice John W. Doran University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/usdaarsfacpub Part of the Agricultural Science Commons Doran, John W., "Soil health and global sustainability: translating science into practice" (2002). Publications from USDA-ARS / UNL Faculty. 181. https://digitalcommons.unl.edu/usdaarsfacpub/181 This Article is brought to you for free and open access by the U.S. Department of Agriculture: Agricultural Research Service, Lincoln, Nebraska at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications from USDA-ARS / UNL Faculty by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Agriculture, Ecosystems and Environment 88 (2002) 119–127 Soil health and global sustainability: translating science into practiceଝ John W. Doran∗ USDA-ARS, 116 Keim Hall, University of Nebraska, Lincoln, NE 68583-0934, USA Abstract Interest in the quality and health of soil has been stimulated by recent awareness that soil is vital to both production of food and fiber and global ecosystems function. Soil health, or quality, can be broadly defined as the capacity of a living soil to func- tion, within natural or managed ecosystem boundaries, to sustain plant and animal productivity, maintain or enhance water and air quality, and promote plant and animal health. Soil quality and health change over time due to natural events or human im- pacts.