Soil Orders in Hawaii Andisol Aridisol Entisol Histosol Inceptisol

Total Page:16

File Type:pdf, Size:1020Kb

Soil Orders in Hawaii Andisol Aridisol Entisol Histosol Inceptisol Prepared by Ike Ikawa, Nguyen Hue and Russell Yost Soil Orders In Hawaii Andisol Aridisol Entisol Histosol Inceptisol Kula Series, Maui Hilo Series, Hawaii Kawaihae Series, Hawaii Jaucas Series, Maui Papai Series, Hawaii Alakai Series, Oahu Kolekole Series, Oahu Andisols are soils derived from volca- Aridisols are soils of the arid areas or Entisols are least-developed soils show- Histosols are organic soils with a high Inceptisols are soils showing minimal nic ash. The less weathered Kula soil on soils with high salt content. The Kawaihae ing only a weak surface development. The organic matter content in the surface ho- development of soil horizons. The Maui is quite productive, while the Hilo soil soil of the Big Island has features of an calareous Jaucas soil on Maui is an ex- rizon. The Papai soil on the Big Island has Kolekole soil on Oahu is an example. on the Big Island is highly weathered and arid area of light color, low organic mat- ample with sandy texture, and excessive lost almost all of the surface organic mat- requires lots of fertilizers for crop produc- ter, and shallow depth. drainage. ter (OM), but the Alakai soil atop Mt. Kaala tion. on Oahu is high in OM. Mollisol Oxisol Spodosol-like soil Ultisol Vertisol Kawaihapai Series, Oahu Makawele Series, Kauai Halii Series, Kauai Oahu Alaeloa Series, Oahu Haiku Series, Maui Lualualei Series, Oahu Mollisols are fertile soils with high Oxisols are the most weathered soils of Spodosols are soils with leached Al, Fe, Ultisols are highly weathered infertile Vertisols are soils that shrink when dry organic C and high base saturation. the tropics with low nutrient holding ca- and organic materials in the subsoil, show- soils with clay accumulation in the sub- and swell when wet. They usually occur Although the Kawaihapai soil on Oahu is pacity and high Fe and Al oxides. The Halii ing a distinct layer. soils. Examples are Alaeloa soil on Oahu in valleys with poor drainage. They are dark, the Makawele soil on Kauai is red soil on Kauai is an example. and Haiku soil on Maui. fertile, but pose severe limitations for because of Fe oxides. roads, housing, and related uses. The Lualualei soil on Oahu is an example..
Recommended publications
  • Engineering Behavior and Classification of Lateritic Soils in Relation to Soil Genesis Erdil Riza Tuncer Iowa State University
    Iowa State University Capstones, Theses and Retrospective Theses and Dissertations Dissertations 1976 Engineering behavior and classification of lateritic soils in relation to soil genesis Erdil Riza Tuncer Iowa State University Follow this and additional works at: https://lib.dr.iastate.edu/rtd Part of the Civil Engineering Commons Recommended Citation Tuncer, Erdil Riza, "Engineering behavior and classification of lateritic soils in relation to soil genesis " (1976). Retrospective Theses and Dissertations. 5712. https://lib.dr.iastate.edu/rtd/5712 This Dissertation is brought to you for free and open access by the Iowa State University Capstones, Theses and Dissertations at Iowa State University Digital Repository. It has been accepted for inclusion in Retrospective Theses and Dissertations by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image.
    [Show full text]
  • 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.
    [Show full text]
  • Soils Section
    Soils Section 2003 Florida Envirothon Study Sections Soil Key Points SOIL KEY POINTS • Recognize soil as an important dynamic resource. • Describe basic soil properties and soil formation factors. • Understand soil drainage classes and know how wetlands are defined. • Determine basic soil properties and limitations, such as mottling and permeability by observing a soil pit or soil profile. • Identify types of soil erosion and discuss methods for reducing erosion. • Use soil information, including a soil survey, in land use planning discussions. • Discuss how soil is a factor in, or is impacted by, nonpoint and point source pollution. Florida’s State Soil Florida has the largest total acreage of sandy, siliceous, hyperthermic Aeric Haplaquods in the nation. This is commonly called Myakka fine sand. It does not occur anywhere else in the United States. There are more than 1.5 million acres of Myakka fine sand in Florida. On May 22, 1989, Governor Bob Martinez signed Senate Bill 525 into law making Myakka fine sand Florida’s official state soil. iii Florida Envirothon Study Packet — Soils Section iv Contents CONTENTS INTRODUCTION .........................................................................................................................1 WHAT IS SOIL AND HOW IS SOIL FORMED? .....................................................................3 SOIL CHARACTERISTICS..........................................................................................................7 Texture......................................................................................................................................7
    [Show full text]
  • World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
    ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO.
    [Show full text]
  • Diagnostic Horizons
    Exam III Wednesday, November 7th Study Guide Posted Tomorrow Review Session in Class on Monday the 4th Soil Taxonomy and Classification Diagnostic Horizons Epipedons Subsurface Mollic Albic Umbric Kandic Ochric Histic Argillic Melanic Spodic Plaggen Anthropic Oxic 1 Surface Horizons: Mollic- thick, dark colored, high %B.S., structure Umbric – same, but lower B.S. Ochric – pale, low O.M., thin Histic – High O.M., thick, wet, dark Sub-Surface Horizons: Argillic – illuvial accum. of clay (high activity) Kandic – accum. of clay (low activity) Spodic – Illuvial O.M. accumulation (Al and/or Fe) Oxic – highly weathered, kaolinite, Fe and Al oxides Albic – light colored, elluvial, low reactivity Elluviation and Illuviation Elluviation (E horizon) Organic matter Clays A A E E Bh horizon Bt horizon Bh Bt Spodic horizon Argillic horizon 2 Soil Taxonomy Diagnostic Epipedons Diagnostic Subsurface horizons Moisture Regimes Temperature Regimes Age Texture Depth Soil Taxonomy Soil forming processes, presence or Order Absence of major diagnostic horizons 12 Similar genesis Suborder 63 Grasslands – thick, dark Great group 250 epipedons High %B.S. Sub group 1400 Family 8000 Series 19,000 Soil Orders Entisols Histosols Inceptisols Andisols Gelisols Alfisols Mollisols Ultisols Spodosols Aridisols Vertisols Oxisols 3 Soil Orders Entisol Ent- Recent Histosol Hist- Histic (organic) Inceptisol Incept- Inception Alfisol Alf- Nonsense Ultisol Ult- Ultimate Spodosol Spod- Spodos (wood ash) Mollisol Moll- Mollis (soft) Oxisol Ox- oxide Andisol And- Ando (black) Gelisol
    [Show full text]
  • 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.
    [Show full text]
  • Stone to Soil Elemental Flux Rates During Pedogenesis
    2010 GSA Denver Annual Meeting (31 October –3 November 2010) Paper No. 146-3 Presentation Time: 2:20 PM-2:35 PM STONE TO SOIL: ELEMENTAL FLUX RATES DURING PEDOGENESIS ON THE SOUTH CAROLINA PIEDMONT BACON, Allan Roy1, RICHTER, Daniel deB.1, BIERMAN, Paul R.2, and ROOD, Dylan H.3, (1) University Program in Ecology and Nicholas School of Environment and Earth Sciences, Duke University, Durham, NC 27708, [email protected], (2) Department of Geology, University of Vermont, Delehanty Hall, 180 Colchester Ave, Burlington, VT 05405, (3) Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA 94550-9234 Opportunities to investigate pedogenic processes in undisturbed soil-bedrock profiles on the southern Piedmont are rare. Historic agriculture was widespread, physically and chemically altering most southern Piedmont soils. We sampled the granitic gneiss parent material and the overlying 6m soil profile from a historically uncultivated, stable, Ultisol located on the Calhoun Experimental Forest in Union County, SC. Our objectives were 3-fold: (1) to quantify flux rates of 8 elements (Si, Al, Fe, Mg, Ca, Na, K, and Mn) during in-situ soil formation on the southern Piedmont using chemical mass balance equations that reference soil horizons to parent material and meteoric 10Be soil residence times, (2) to characterize the distribution of meteoric 10Be in a highly-weathered Ultisol profile through measurement of other soil properties (including pH, %C, exchangeable cations, KCl acidity, texture, and effective CEC and base saturation) and multivariate analysis, and (3) to estimate Be mobility in soil during granitic gneiss weathering in the southern Piedmont using the mass balance approach described above.
    [Show full text]
  • Examining Local Climate Variability in the Late Pennsylvanian Through Paleosols: an Example from the Lower Conemaugh Group of Southeastern Ohio, USA
    Geosciences 2012, 2, 260-276; doi:10.3390/geosciences2040260 OPEN ACCESS geosciences ISSN 2076-3263 www.mdpi.com/journal/geosciences Article Examining Local Climate Variability in the Late Pennsylvanian Through Paleosols: An Example from the Lower Conemaugh Group of Southeastern Ohio, USA Nicole D. Dzenowski and Daniel I. Hembree * Department of Geological Sciences, Ohio University, 316 Clippinger Laboratories, Athens, OH 45701, USA; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-740-597-1495; Fax: +1-740-593-0486. Received: 14 September 2012; in revised form: 18 October 2012/ Accepted: 29 October 2012/ Published: 1 November 2012 Abstract: Three temporally close stratigraphic sections were excavated in Glenshaw Formation of Athens County, Ohio. The described units are Upper Pennsylvanian (Gzhelian, 305–302 Ma) and located in the distal portion of the Appalachian foreland basin. Mudstone units interpreted as paleosols were identified across all three sections. Detailed field and micromorphological studies lead to the recognition of two separate paleosols within the profile. The profile consists of a composite paleosol composed of two cumulative paleosols. The lower paleosol is interpreted as a calcic Vertisol which formed in a seasonally dry environment whereas the upper paleosol is interpreted as a gleyed Inceptisol which formed in a seasonally wet environment. The change in paleosol types is the result of increased precipitation which led to saturation of the soil and surface ponding. Pedogenic carbonate nodules are a common feature throughout the entire profile as are stress cutans. A coalesced carbonate horizon (Bk) was observed approximate 120 cm from the top of the profile in all three sections.
    [Show full text]
  • SAINS TANAH – Journal of Soil Science and Agroclimatology, 17(2), 2020, 135-143
    SAINS TANAH – Journal of Soil Science and Agroclimatology, 17(2), 2020, 135-143 SAINS TANAH – Journal of Soil Science and Agroclimatology Journal homepage: http://jurnal.uns.ac.id/tanah Characteristics of Ultisols derived from basaltic andesite materials and their association with old volcanic landforms in Indonesia Setiyo Purwanto*, Rachmat Abdul Gani1 Erna Suryani1 Indonesian Center for Agricultural Land Resource Research and Development - ICALRRD ARTICLE INFO ABSTRACT Keywords: The common problem with Ultisols is their low pH and soil fertility, with liming and Pedon fertilization being common solutions to overcome this problem; however, studies on Minerals Ultisol soil parent materials are still rare. This study aimed to examine the characteristics Parent material of Ultisols derived from andesite and basaltic andesite parent materials. In 2016–2017, five Weathering Ultisol pedons (P8, P9, P10, P11, and P15) were sampled from basaltic andesites and other Soil fertility associations. The five pedons consisted of 19 soil samples. The chemical and mineralogical properties of the soils were analyzed. It was found that the color of the basaltic andesite Article history Ultisols varied from hue of 2.5 YR to 10 YR, with value of 3–5 and chroma of 2–8. The Submitted: 2019-12-23 Ultisols derived from andesite/diorite (P8) were dominated by rock fragments (52–77%), Accepted: 2020-12-11 while those derived from andesitic breccia (P9) were dominated by opaques (62–67%), those from basaltic andesite tuff/lava by weathering minerals (44–52%) and hydragilite * Corresponding Authors (28–34%), those from basaltic andesite (P11) by quartz (48%) and (P15) by opaques (79– Email address: 89%).
    [Show full text]
  • Wade Et Al., 2019) and Inversely Et Al., 2012; Lehmann Et Al., 2008)
    Geoderma 366 (2020) 114235 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Assessing the sensitivity and repeatability of permanganate oxidizable T carbon as a soil health metric: An interlab comparison across soils ⁎ Jordon Wadea, , Gabriel Maltais-Landryb, Dawn E. Lucasb, Giulia Bongiornoc,d, Timothy M. Bowlese, Francisco J. Calderónf, Steve W. Culmang, Rachel Daughtridgeh, Jessica G. Ernakovichi, Steven J. Fontej, Dinh Giangk, Bethany L. Hermang, Lindsey Guane, Julie D. Jastrowl, Bryan H.H. Lohi, Courtland Kellyj, Meredith E. Manng, Roser Matamalal, Elizabeth A. Miernickia, Brandon Petersonf, Mirjam M. Pullemanc,m, Kate M. Scowk, Sieglinde S. Snappn,o, Vanessa Thomasn, Xinyi Tun, Daoyuan Wangk, Nicolas A. Jelinskip, Garrett C. Lilesq, Felipe H. Barrios-Masiasr, Devin A. Rippnerk, Maria L. Silveirab,s, ⁎ Andrew J. Margenota, a Department of Crop Sciences, University of Illinois at Urbana-Champaign, United States b Soil and Water Sciences Department, University of Florida, United States c Soil Biology Group, Wageningen University, the Netherlands d Department of Soil Science, Research Institute of Organic Agriculture (FiBL), Germany e Department of Environmental Science, Policy, & Management, University of California, Berkeley, United States f Central Great Plains Research Station, USDA-ARS, United States g School of Environment & Natural Resources, The Ohio State University, United States h Department of Natural Resources and Environmental Sciences, University of Illinois at Urbana-Champaign,
    [Show full text]
  • Soil Properties Database of Spanish Soils. Volumen
    65°^ e 0 6,2.1 Centro de Investigaciones Energeticas, Medioambientales y Tecnoldgicas Miner A, is /X Base de Dates de Propiedades Edafoldgicas de los Suelos Espanoles. VolumenXI. CASTHIA-LEON(b): Palentia, Valladolid y Avila C. Trueba RMillan T. Schmid received C. Lago JUL 121999 C. Roquero M. Magister OSTl MormesTecnicosCiemat 898 julio,1999 1. -a;:' ' > DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. Informes T ecnicos Ciemat 898 julio, 1999 Base de Dates dePropiedades Edafologicas de los Suelos Espanoles. VohnnenXL CASHLLA-LEON(b): Palencia, Valladolid y Avila C. Trueba (*) R. Millan(*) T. Schmid (*) C. Lago (*) C. Roquero (**) M.Magister (**) (*) CIEMAT (**)UPM Departamento de Impacto Ambiental de la Energia Toda correspondenica en relation con este trabajo debe dirigirse al Servicio de Information y Documentation, Centro de Investigaciones Energeticas, Medioambientales y Tecnoldgicas, Ciudad Universitaria, 28040-MADRID, ESPANA. Las solicitudes de ejemplares deben dirigirse a este mismo Servicio. Los descriptores se ban seleccionado del Thesauro del DOE para describir las materias que contiene este informe con vistas a su recuperation. La catalogacidn se ha hecho utilizando el documento DOE/TIC-4602 (Rev. 1) Descriptive Cataloguing On-Line, y la clasificacion de acuerdo con el documento DOE/TIC.4584-R7 Subject Categories and Scope publicados por el Office of Scientific and Technical Information del Departamento de Energia de los Estdos Unidos. Se autoriza la reproduction de los resumenes analiticos que aparecen en esta publication. Deposito Legal: M -14226-1995 ISSN: 1135-9420 NIRO: 238-99-003-5 Editorial CIEMAT CLASIFICACION DOE Y DESCRIPTORES 540230 SOILS; SOIL CHEMISTRY; SOIL MECHANICS; RADIONUCLIDE MIGRATION; DATA BASE MANAGEMENT; DATA COMPILATION; SPAIN; “Base de Dates de Propiedades Edafologicas de los Suelos Espanoles.
    [Show full text]
  • Characterization of Several Paddy Soil Types in Bogor, West Java, Indonesia
    Available online at: http://journal.unila.ac.id/index.php/tropicalsoilJ Trop Soils, Vol. 20, No. 1, 2016: 27-32 27 DOI: 10.5400/jts.2016.21.1.27 Characterization of Several Paddy Soil Types in Bogor, West Java, Indonesia Kurniati, Sudarsono and Suwardi Department of Soil Science and Land Resource, Bogor Agricultural University Bogor 16680, Indonesia, e-mail: [email protected] Received 23 October 2015/ accepted 04 January 2016 ABSTRACT Paddy soil has different morphology and pedogenic characteristics compared to dry land, due to the influence of inundation during several months in a year. Puddling and drying that occurs in turns (redox cycle) in paddy soil can lead to the formation of concretions or rusty Fe and Mn. The main purpose of this study was to understand the changing of the morphological and chemical properties as a result of changing of the dry land to paddy soil. Besides, the study also aimed to understand plow pan layer formation in Podsolic, Latosol, Regosol, and Andosol soil type. Results showed that content of soil density (bulk density) of dry land ranged from 0.5 to 1.0, while paddy soil is 0.8 to 1.0 (g cm-3). Bulk density values in all four types of soils increased after the changing. Observation also demonstrated that severity levels of paddy soil is higher than dry land, especially in the second and third soil layers or under the surface of soils. Acidity of dry land was likely to be higher than paddy soil. There were no significant differences in nutrient such as C-organic, P and N.
    [Show full text]