Biodiversity and Pedodiversity: a Matter of Coincidence?
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Profile 113 Jan 1998
PROFILE THE OFFICIAL NEWSLETTER OF THE AUSTRALIAN SOCIETY OF SOIL SCIENCE WA soil assessment and management SSSI's Western Australian branch held its fourth triennial conference at Geraldton in October. A one day preconference bus tour from Perth to Geraldton looked at sandplain productivity, and management tech- Aniques for hardsetting soils. After the two day conference, the branch held a one day workshop on potassium in agriculture to look at current and future directions for research and development to improve the efficiency of agri- cultural potassium use. Full reports on the conference and workshop appear on pages 8 and 9. Above: John Bartle, Department of Conservation and Land Management, addresses the preconference tour group on the use of oil mallees as a means of increasing water use while providing and alternative cash crop for farmers. In this issue • National conference update Listing of all accredited soil scientists • Review: Australian Soil Classification • Leeper lecture • What is a soil scientist? AUSTRALIAN SOCIETY OF SOIL SCIENCE The Australian Society of Soil Science Incorporated (ASSSI) was founded in 1955 to Contents work towards the advancement of soil science in the professional, academic and technical fields. It 3 From the president comprises a Federal Council and seven branches (Qld, NSW, Riverina, ACT, Vic, SA and WA). Liability of members is limited. 4 Accredited soil scientists Objectives • To advance soil science • To provide a link between soil scientists and 5 Conference update members of kindred bodies -
Biomechanical and Biochemical Effects Recorded in the Tree Root Zone – Soil Memory, Historical Contingency and Soil Evolution Under Trees
Plant Soil (2018) 426:109–134 https://doi.org/10.1007/s11104-018-3622-9 REGULAR ARTICLE Biomechanical and biochemical effects recorded in the tree root zone – soil memory, historical contingency and soil evolution under trees Łukasz Pawlik & Pavel Šamonil Received: 17 September 2017 /Accepted: 1 March 2018 /Published online: 15 March 2018 # The Author(s) 2018 Abstract increase in soil spatial complexity. We hypothesized that Background and aims The changing soils is a never- trees can be a strong local factor intensifying, blocking ending process moderated by numerous biotic and abi- or modifying pedogenetic processes, leading to local otic factors. Among these factors, trees may play a changes in soil complexity (convergence, divergence, critical role in forested landscapes by having a large or polygenesis). These changes are hypothetically con- imprint on soil texture and chemical properties. During trolled by regionally predominating soil formation their evolution, soils can follow convergent or divergent processes. development pathways, leading to a decrease or an Methods To test the main hypothesis, we described the pedomorphological features of soils under tree stumps of fir, beech and hemlock in three soil regions: Haplic Highlights Cambisols (Turbacz Reserve, Poland), Entic Podzols 1) The architecture of tree root systems controls soil physical and (Žofínský Prales Reserve, Czech Republic) and Albic chemical properties. Podzols (Upper Peninsula, Michigan, USA). Soil pro- 2) The predominating pedogenetic process significantly modifies files under the stumps, as well as control profiles on sites the effect of trees on soil. 3) Trees are a factor in polygenesis in Haplic Cambisols at the currently not occupied by trees, were analyzed in the pedon scale. -
The Use of Proximal Soil Sensor Data Fusion and Digital Soil Mapping For
The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, Raphael Viscarra Rossel To cite this version: Wenjun Ji, Viacheslav Adamchuk, Songchao Chen, Asim Biswas, Maxime Leclerc, et al.. The use of proximal soil sensor data fusion and digital soil mapping for precision agriculture. Pedometrics 2017, Jun 2017, Wageningen, Netherlands. 298 p. hal-01601278 HAL Id: hal-01601278 https://hal.archives-ouvertes.fr/hal-01601278 Submitted on 2 Jun 2020 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. Distributed under a Creative Commons Attribution - ShareAlike| 4.0 International License Abstract Book Pedometrics 2017 Wageningen, 26 June – 1 July 2017 2 Contents Evaluating Use of Ground Penetrating Radar and Geostatistic Methods for Mapping Soil Cemented Horizon .................................... 13 Digital soil mapping in areas of mussunungas: algoritmos comparission .......... 14 Sensing of farm and district-scale soil moisture content using a mobile cosmic ray probe (COSMOS Rover) .................................... 15 Proximal sensing of soil crack networks using three-dimensional electrical resistivity to- mography ......................................... 16 Using digital microscopy for rapid determination of soil texture and prediction of soil organic matter ..................................... -
Pedometric Mapping of Key Topsoil and Subsoil Attributes Using Proximal and Remote Sensing in Midwest Brazil
UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 UNIVERSIDADE DE BRASÍLIA FACULDADE DE AGRONOMIA E MEDICINA VETERINÁRIA PROGRAMA DE PÓS-GRADUAÇÃO EM AGRONOMIA PEDOMETRIC MAPPING OF KEY TOPSOIL AND SUBSOIL ATTRIBUTES USING PROXIMAL AND REMOTE SENSING IN MIDWEST BRAZIL RAÚL ROBERTO POPPIEL ORIENTADOR: Profa. Dra. MARILUSA PINTO COELHO LACERDA CO-ORIENTADOR: Prof. Titular JOSÉ ALEXANDRE MELO DEMATTÊ TESE DE DOUTORADO EM AGRONOMIA BRASÍLIA/DF MARÇO/2020 ii iii REFERÊNCIA BIBLIOGRÁFICA POPPIEL, R. R. Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. Faculdade de Agronomia e Medicina Veterinária, Universidade de Brasília- Brasília, 2019; 105p. (Tese de Doutorado em Agronomia). CESSÃO DE DIREITOS NOME DO AUTOR: Raúl Roberto Poppiel TÍTULO DA TESE DE DOUTORADO: Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil. GRAU: Doutor ANO: 2020 É concedida à Universidade de Brasília permissão para reproduzir cópias desta tese de doutorado e para emprestar e vender tais cópias somente para propósitos acadêmicos e científicos. O autor reserva outros direitos de publicação e nenhuma parte desta tese de doutorado pode ser reproduzida sem autorização do autor. ________________________________________________ Raúl Roberto Poppiel CPF: 703.559.901-05 Email: [email protected] Poppiel, Raúl Roberto Pedometric mapping of key topsoil and subsoil attributes using proximal and remote sensing in Midwest Brazil/ Raúl Roberto Poppiel. -- Brasília, 2020. -
Evolution of the Landscape and Pedodiversity on Volcanic Deposits
Evolution of the landscape and pedodiversity on volcanic deposits in the south of the Basin of Mexico and its relationship with agricultural activities Evolución del paisaje y pedodiversidad sobre depósitos volcánicos en el sur de la Cuenca de México y su relación con actividades agrícolas Elizabeth Solleiro-Rebolledo1‡ , Yazmín Rivera-Uria1 , Bruno Chávez-Vergara1,2 , Jaime Díaz-Ortega1 , Sergey Sedov1 , Jorge René Alcalá-Martínez 1,2 , Ofelia Ivette Beltrán-Paz1 , and Luis Gerardo Martínez-Jardines1 1 Instituto de Geología; 2 Laboratorio Nacional de Geoquímica y Mineralogía. Circuito de la Investigación Científica s/n. Cd. Universitaria. 04510 Ciudad de México, México. ‡ Corresponding author ([email protected]) SUMMARY carbonates places their formation in the mid-Holocene, an epoch for which drier conditions are detected in In this work, we present the results of a soil study other sites of the Basin of Mexico. The agricultural land in the Teuhtli volcano, located to the south of the Basin use has also promoted morphological, chemical and of Mexico with the aim to understand the pedogenetic physical changes in the soils. The continuous tillage pathways and the evolution of the landscape dynamics. of the sites has prevented the soils from developing. Two different types of soil prof iles were sampled: in This could have a negative effect on the fertility of “conserved” areas, with less anthropogenic influence those soils currently used to sustain the peri-urban and in sites with intense agriculture activities since agroecosystems of Mexico City. pre-Hispanic times. The three conserved prof iles are located in different landscape positions: the Cima Index words: andosolization, land use change, prof ile in the summit, the Ladera prof ile in the high pedogenic carbonates, Teuhtli volcano. -
421136 1 En Bookbackmatter 229..393
Appendix A Formative Elements for Wisconsin Soils in Soil Taxonomy Taxonomic level Formative element Meaning Orders -alf Alfisols -ent Entisols -ist Histosols -ept Inceptisols -oll Mollisols -od Spodosols -ult Ultisols Suborders aqu Aquic conditiions (wet) fibr Fibric organic materials (least decomposed) fluv Floodplain hem Hemic organic materials (intermediate in decomposition) orth Central concept psamm Sandy textures sapr Sapric organic materials (most decomposed) ud Udic soil-moisture class (never dry for >90 cumulative days or >45 consecutive days) ust Ustic soil-moisture class (dry for >180 cumulative days or >90 consecutive days) Great groups Alb Contains an albic € horizon Arg Contains an argillic (Bt) horizon Dystr Base saturation <60% Endo Saturated from below Epi Saturated from above Eutr Base saturation >60% Fluv Floodplain Fragi Contains a fragipan (Bx) horizon Gloss Contains a glossic (E/B, B/E) horizon Hapl Minimum horizon development Hum Presence of organic matter Pale Excessive development Psamm Sandy texture Quartzi Quartz-rich Sphagno From Sphagnum mosses Ud Udic soil-moisture class (never dry for >90 cumulative days or >45 consecutive days) (continued) © Springer International Publishing AG 2017 229 J.G. Bockheim and A.E. Hartemink, The Soils of Wisconsin, World Soils Book Series, DOI 10.1007/978-3-319-52144-2 230 Appendix A: Formative Elements for Wisconsin Soils in Soil Taxonomy (continued) Taxonomic level Formative element Meaning Subgroup Aeric Aeration Alfic Contains argillic (Bt) horizon Aquertic Intergrade with -
Rusell Review
European Journal of Soil Science, March 2019, 70, 216–235 doi: 10.1111/ejss.12790 Rusell Review Pedology and digital soil mapping (DSM) Yuxin Ma , Budiman Minasny , Brendan P. Malone & Alex B. Mcbratney Sydney Institute of Agriculture, School of Life and Environmental Sciences, The University of Sydney, Eveleigh, New South Wales, Australia Summary Pedology focuses on understanding soil genesis in the field and includes soil classification and mapping. Digital soil mapping (DSM) has evolved from traditional soil classification and mapping to the creation and population of spatial soil information systems by using field and laboratory observations coupled with environmental covariates. Pedological knowledge of soil distribution and processes can be useful for digital soil mapping. Conversely, digital soil mapping can bring new insights to pedogenesis, detailed information on vertical and lateral soil variation, and can generate research questions that were not considered in traditional pedology. This review highlights the relevance and synergy of pedology in soil spatial prediction through the expansion of pedological knowledge. We also discuss how DSM can support further advances in pedology through improved representation of spatial soil information. Some major findings of this review are as follows: (a) soil classes can bemapped accurately using DSM, (b) the occurrence and thickness of soil horizons, whole soil profiles and soil parent material can be predicted successfully with DSM techniques, (c) DSM can provide valuable information on pedogenic processes (e.g. addition, removal, transformation and translocation), (d) pedological knowledge can be incorporated into DSM, but DSM can also lead to the discovery of knowledge, and (e) there is the potential to use process-based soil–landscape evolution modelling in DSM. -
Pedodiversity in the United States of America
Geoderma 117 (2003) 99–115 www.elsevier.com/locate/geoderma Pedodiversity in the United States of America Yinyan Guo, Peng Gong, Ronald Amundson* Division of Ecosystem Sciences and Center for Assessment and Monitoring of Forest and Environmental Resources (CAMFER), 151 Hilgard Hall, College of Natural Resources, University of California, Berkeley, CA 94720-3110, USA Received 8 July 2002; accepted 17 March 2003 Abstract Little attention has been paid to analyses of pedodiversity. In this study, quantitative aspects of pedodiversity were explored for the USA based on the State Soil Geographic database (STATSGO). First, pedodiversity indices for the conterminous USA were estimated. Second, taxa–area relationships were investigated in each soil taxonomic category. Thirdly, differences in pedodiversity between the USDA-NRCS geographical regions were compared. Fourth, the possible mechanisms underlying the observed relative abundance of soil taxa were explored. Results show that as the taxonomic category decreases from order to series, Shannon’s diversity index increases because taxa richness increased dramatically. The relationship between the number of taxa (S) and area (A) is formulated as S=cAz. The exponent z reflects the taxa-richness of soil ‘communities’ and increases constantly as taxonomic categories decrease from order to series. The ‘‘West’’ USDA-NRCS geographical region has the highest soil taxa richness, followed by the ‘‘Northern Plains’’ region. The ‘‘South Central’’ region has the highest taxa evenness, while taxa evenness in the ‘‘West’’ region is the lowest. The ‘‘West’’ or the ‘‘South Central’’ regions have the highest overall soil diversity in the four highest taxonomic categories, while the ‘‘West’’ or ‘‘Northern Plains’’ regions have the highest diversity in the two lowest taxonomic levels. -
A Review of Methods in Natural Diversity Studies: the Need for Standardization 1 Juan-José Ibáñeza, Eric C. Brevikb*
*Manuscript Click here to view linked References 1 A Review of Methods in Natural Diversity Studies: The Need for Standardization 2 Juan-José Ibáñeza, Eric C. Brevikb* 3 a - National Museum of Natural History of Spain, Spanish National Research Council (CSIC), Serrano 115 4 dpdo, 28006 Madrid, Spain 5 b - Department of Natural Sciences, Dickinson State University, Dickinson, ND 58601 USA 6 (*) Corresponding Author: [email protected] 7 8 Abstract 9 There has been considerable interest in geodiversity and pedodiversity studies over the last 10 approximately 30 years. Pedodiversity is considered part of geodiversity. However in practice they 11 involved different experts and traditions. There are many common aspects that could be shared by all 12 natural diversity studies, however, these common aspects have not been adequately studied and 13 debated. Quantitative techniques that were developed and refined by biodiversity researchers over 14 multiple decades of biodiversity studies should also be applicable to geodiversity and pedodiversity 15 studies. Soil scientists studying pedodiversity followed the same techniques as mathematical ecologists, 16 but geologists studying geodiversity focused on the implementation of proposals aimed at preserving 17 geological heritage and popularising it among the general public. Therefore, pedodiversity and 18 geodiversity diverged and it is not currently possible to compare the results of geodiversity and 19 pedodiversity research. To reach a point where these research results could be compared, it will be 20 necessary to (i) follow uniform mathematical procedures in both these fields and their subfields and (ii) 21 develop universal taxonomies that will be followed for each of the natural resources (fossils, landforms, 22 minerals, soils, etc.) being investigated. -
Strategies for State Policies and Spending
STATE OF DELAWARE EXECUTIVE DEPARTMENT OFFICE OF STATE PLANNING COORDINATION May 21, 2013 Mr. Jeff Clark Land Tech Land Planning 118 Atlantic Avenue, Ste. 202 Ocean View, DE 19970 RE: PLUS review – 2013-04-05; Del-Mar Subdivision Dear Mr. Clark: Thank you for meeting with State agency planners on April 24, 2013 to discuss the proposed plans for the Del-Mar Subdivision located at 39726 Dukes Dune Road near Bethany Beach. According to the information received, you are seeking a subdivision of two existing lots to create 5 lots. It is our understanding that the two existing homes will stay and 3 additional homes will be built. Please note that changes to the plan, other than those suggested in this letter, could result in additional comments from the State. Additionally, these comments reflect only issues that are the responsibility of the agencies represented at the meeting. The developers will also need to comply with any Federal, State and local regulations regarding this property. We also note that as Sussex County is the governing authority over this land, the developers will need to comply with any and all regulations/restrictions set forth by the County. Strategies for State Policies and Spending This project is located in Investment Level 3 according to the Strategies for State Policies and Spending. Investment Level 3 reflects areas where growth is anticipated by local, county, and state plans in the longer term future, or areas that may have environmental or other constraints to development. State investments may support future growth in these areas, but please be advised that the State has other priorities for the near future. -
2005 Newsletters
Illinois Soil Classifiers Association Newsletter Spring 2005 Upcoming Events • Early Fall ISCA Meeting - East Central Message from the President Illinois. Come see soils behind, on top of, I would like to encourage our membership to participate in upcoming ISCA sponsored and in front of the activities. The annual ISCA Summer Meeting is one example where we spend time in the Shelbyville Moraine. field discussing current soils related issues and findings. Over the past couple of years we have looked at the variability of loam tills in Northern Illinois and visited the Central Illinois soils along the Illinois River. Late summer or most likely early fall, our plans are to visit East Central Illinois and check out the soils north of, on top of, and south of the Shelbyville Moraine. Lunch is provided at our cost, the atmosphere is more informal than at the annual winter meeting, and the weather is always better. So be there! Inside this issue: Our website keeps getting better. The address is www.illinoissoils.org. Mark Bramstedt has done a great job to build this up and keep it current. From the web site you can find out about upcoming events and programs, find contact numbers and address of many ISCA members, and view our most recent version of the Membership Handbook. Steps to Achieving 2 Soils Licensing in As a final comment, one surprise I had from our annual winter meeting was the great success Your State of the Drummer t-shirt sales. I bought some as gifts and gave one to my son’s high school science teacher. -
Trenching and Excavation: Safety Principles
Ohio State University Extension Fact Sheet Food, Agricultural and Biological Engineering 590 Woody Hayes Dr., Columbus, Ohio 43210 Trenching and Excavation: Safety Principles AEX-391-92 Larry C. Brown Kent L. Kramer Thomas L. Bean Timothy J. Lawrence Trenching and excavation procedures are performed thousands of times a day across the United States. Unfortunately, about 60 people are killed in trenching accidents each year. Contractors and construction laborers should understand the laws and regulations applicable to trenching and excavation occupations. These statutes are in effect for the express purpose of protecting those who work in trenching and excavation situations. Although farmers are generally exempt from the state trenching and excavation statutes, they may still be held liable for accidents and loss of life resulting from trenching and excavation activities conducted under their direction. This publication provides Ohio's construction contractors, laborers and farmers with an overview of soil mechanics relating to trench and excavation failures, and of Ohio's trenching and excavation laws. It is not intended to provide the reader a strict legal interpretation, but to increase his/her awareness of excavation and trench safety, and provide guidance on where to obtain more information. Soil Mechanics In trenching and excavation practices, "soil" is defined as any material removed from the ground to form a hole, trench or cavity for the purpose of working below the earth's surface. This material is most often weathered rock and humus known as clays, silts and loams, but also can be gravel, sand and rock. It is necessary to know the characteristics of the soil at the particular job site.