Guidelines for Soil Description
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Soil Properties and Pre-Columbian Settlement Patterns in The
SOIL, 1, 65–81, 2015 www.soil-journal.net/1/65/2015/ doi:10.5194/soil-1-65-2015 SOIL © Author(s) 2015. CC Attribution 3.0 License. Soil properties and pre-Columbian settlement patterns in the Monumental Mounds Region of the Llanos de Moxos, Bolivian Amazon U. Lombardo1,2, S. Denier1, and H. Veit1 1Universität Bern, Geographisches Institut, Hallerstrasse 12, 3012 Bern, Switzerland 2CaSeS research group, IMF-CSIC, C/Egipciaques, 15-08001 Barcelona, Spain Correspondence to: U. Lombardo ([email protected]) Received: 5 May 2014 – Published in SOIL Discuss.: 15 May 2014 Revised: – – Accepted: 26 September 2014 – Published: 6 January 2015 Abstract. In the present paper we explore to what degree soil properties might have influenced pre-Columbian settlement patterns in the Monumental Mounds Region (MMR) of the Llanos de Moxos (LM), Bolivian Amazon. Monumental mounds are pre-Hispanic earth buildings and were preferentially built on mid- to late Holocene palaeolevees of the Grande River (here denominated PR1), while levees of older palaeorivers (PR0) were only sparsely occupied. We dug two transects across PR0 and PR1 levee–backswamp catenas and analysed them for grain size, pH, cation exchange capacity (CEC) and Corg. Our data show that PR1 soils, where the density of mounds is higher, have far greater agricultural potential than PR0 soils, which are affected by aluminium toxicity in the backswamps and by high levels of exchangeable sodium in the levees. This study provides new data on the soil properties of the south-eastern Bolivian Amazon and reinforces the hypothesis that environmental constraints and opportunities exerted an important role on pre-Columbian occupation patterns and the population density reached in the Bolivian Amazon. -
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. -
NRCS Keys to Soil Taxonomy
United States Department of Agriculture Keys to Soil Taxonomy Ninth Edition, 2003 Keys to Soil Taxonomy By Soil Survey Staff United States Department of Agriculture Natural Resources Conservation Service Ninth Edition, 2003 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250-9410, or call 202-720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Cover: A natric horizon with columnar structure in a Natrudoll from Argentina. 5 Table of Contents Foreword .................................................................................................................................... 7 Chapter 1: The Soils That We Classify.................................................................................. 9 Chapter 2: Differentiae for Mineral Soils and Organic Soils ............................................... 11 Chapter 3: Horizons and Characteristics Diagnostic for the Higher Categories ................. -
Eletrochemical Changes in Gleysol of the Amazon Estuary
http://dx.doi.org/10.4322/rca.1796 ORIGINAL ARTICLE George Rodrigues da Silva1* Paulo Augusto Lobato da Silva2 Sérgio Brazão e Silva1 Mário Lopes da Silva Junior1 Eletrochemical changes in Gleysol of the Marcos André Piedade Gama1 Antonio Rodrigues Fernandes1 Amazon estuary Alterações eletroquímicas em Gleissolo do estuário 1 Universidade Federal Rural da Amazônia – UFRA, Instituto de Ciências Agrárias, Av. Presidente Tancredo Neves, 2501, 66077-830, Belém, PA, amazônico Brasil 2 Empresa de Assistência Técnica e Extensão Rural do Estado do Pará – EMATER/PA, Rodovia BR- 316, km 12, s/n, 67105-970, Ananindeua, PA, ABSTRACT: Electrochemical reactions are intensified by soil flooding, which changes Brasil the dynamics of nutrients and negatively affects plant growth. In this work, we aimed to Corresponding Author: evaluate the changes in the redox potential (Eh), pH and nutrient availability in a Haplic E-mail: [email protected] Gleysol soil from a floodplain of the Guamá River, Belém, Pará State. During the period of floods (61 days), samples soils were collected on alternate days and analyzed in dry and wet conditions. Flooding resulted in higher pH values and decreased Eh, which stabilized after 32 days of flooding and did not affect the values of total nitrogen. An increase in the KEYWORDS Oxidation-reduction concentrations of phosphorus, sulfur, iron, manganese, copper and zinc were observed, and Availability of nutrients they were subsequently reduced with time of submergence. The reduction of sulfur occurred Waterlogged soils at low Eh and pH values near neutrality. The results show that nitrogen and sulfur do not limit agricultural production in the lowland soils of the Guamá River. -
Changes in Soil Properties in a Fluvisol (Calcaric) Amended with Coal Fly Ash A
Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann To cite this version: A. Riehl, F. Elsass, J. Duplay, F. Huber, M. Trautmann. Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash. Geoderma, Elsevier, 2010, 155 (1-2), pp.67-74. 10.1016/j.geoderma.2009.11.025. halsde-00546980 HAL Id: halsde-00546980 https://hal.archives-ouvertes.fr/halsde-00546980 Submitted on 30 May 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. Geoderma 155 (2010) 67–74 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Changes in soil properties in a fluvisol (calcaric) amended with coal fly ash A. Riehl a, F. Elsass b, J. Duplay a,⁎, F. Huber a, M. Trautmann c a Laboratoire d'Hydrologie et de Géochimie de Strasbourg, UMR 7517 CNRS, 1 rue Blessig 67084 Strasbourg Cedex, France b Institut National de Recherche Agronomique, route de Saint-Cyr 78026Versailles, France c UMS 830 UDS/CNRS, Laboratoire d'Analyses des Sols et des Formations Superficielles, 3 rue de l'Argonne 67083 Strasbourg Cedex, France article info abstract Article history: Fluidized bed combustion ash (FBC) is a by-product from coal-fired power stations used for many decades in Received 25 March 2009 concrete, cement and brick manufacturing and more recently for trace metal immobilization and pesticide Received in revised form 17 November 2009 retention in soils. -
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. -
Plant Uptake of Radionuclides in Lysimeter Experiments
AT9900006 Plant uptake of radionuclides in lysimeter experiments M.H. Gerzabek F. Strebl B. Temmel June 1998 OEFZS—4820 SEIBERSDORF 30-20 / OEFZS-4820 June 1998 Plant uptake of radionuclides in lysimeter experiments In: Environmental Pollution 99 (1998) 93-103 M.H. Gerzabek, F. Strebl, B. Temmel Department of Environmental Research Division of Life Sciences ENVIRONMENTAL POLLUTION ELSEVIER Environmental Pollution 99 (1998) 93-103 Plant uptake of radionuclides in lysimeter experiments M.H. Gerzabek*, F. Strebl, B. Temmel Austrian Research Centre Seibersdorf, Division of Life Sciences, A-2444 Seibersdorf Austria Received 20 June 1997; accepted 15 October 1997 Abstract The results of seven years lysimeter experiments to determine the uptake of 60 Co, 137Cs and 226 Ra into agricultural crops (endive, maize, wheat, mustard, sugarbeet, potato, Faba bean, rye grass) are described. The lysimeter consists of twelve monolithic soil profiles (four soil types and three replicates) and is located in Seibersdorf/Austria, a region with a pannonian climate (pronounced differences between hot and semi-arid summers and humid winter conditions, annual mean of precipitation: 517 mm, mean annual temperature: 9.8°C). Besides soil-to-plant transfer factors (TF), fluxes were calculated taking into account biomass production and growth time. Total median values of TF’s (dry matter basis) for the three radionuclides decreased from 226 Ra (0.068 kg kg" 1) to ,37Cs (0.043 kg kg" 1) and 60 Co (0.018 kg kg" 1); flux values exhibited the same ranking. The varying physical and chemical proper ties of the four experimental soils resulted in statistically significant differences in transfer factors or fluxes between the investigated soils for l37Cs and 226 Ra, but not for 60 Co. -
Choosing a Soil Amendment Fact Sheet No
Choosing a Soil Amendment Fact Sheet No. 7.235 Gardening Series|Basics by J.G. Davis and D. Whiting* A soil amendment is any material added not be used as a soil amendment. Don’t add Quick Facts to a soil to improve its physical properties, sand to clay soil — this creates a soil structure such as water retention, permeability, water similar to concrete. • On clayey soils, soil infiltration, drainage, aeration and structure. Organic amendments increase soil amendments improve the The goal is to provide a better environment organic matter content and offer many soil aggregation, increase for roots. benefits. Over time, organic matter improves porosity and permeability, and To do its work, an amendment must be soil aeration, water infiltration, and both improve aeration, drainage, thoroughly mixed into the soil. If it is merely water- and nutrient-holding capacity. Many and rooting depth. buried, its effectiveness is reduced, and it will organic amendments contain plant nutrients interfere with water and air movement and and act as organic fertilizers. Organic matter • On sandy soils, soil root growth. also is an important energy source for amendments increase the Amending a soil is not the same thing bacteria, fungi and earthworms that live in water and nutrient holding as mulching, although many mulches also the soil. capacity. are used as amendments. A mulch is left on the soil surface. Its purpose is to reduce Application Rates • A variety of products are available bagged or bulk for evaporation and runoff, inhibit weed growth, Ideally, the landscape and garden soils and create an attractive appearance. -
Diversity and Classification Problems of Sandy Soils in Subboreal Zone (Central Europe, Poland)
Diversity and classification problems of sandy soils in subboreal zone (Central Europe, Poland) Michał Jankowski Faculty of Biology and Earth Sciences, Nicolaus Copernicus University, Toruń, Poland, Email [email protected] Abstract The aim of this study was to present some examples of sandy soils and to discuss their position in soil systematics. 8 profiles represent: 4 soils widely distributed in postglacial landscapes of Poland (Central Europe), typical for different geomorphological conditions and vegetation habitats (according to regional soil classification: Arenosol, Podzolic soil, Rusty soil and Mucky soil) and 4 soils having unusual features (Gleyic Podzol and Rusty soil developed in a CaCO 3-rich substratum and two profiles of red-colored Ochre soils). According to WRB (IUSS Working Group WRB, 2007), almost all of these soils can be named Arenosols. Considering their individual morphological features (stage of development, sequence of horizons) and different ecological value, most of the studied soils should be classified into other Reference Soil Groups or even distinguished in individual units. Key Words Soil classification, Soil geography, Soil morphology, Arenosols, Podzols, Sand. Introduction Soils developed from loose quartz sands generally represent the least fertile mineral soils in the World. According to WRB soil classification (IUSS Working Group WRB 2007), one genetic variant - Podzols - is distinguished as individual unit from that textural group of soils. Most of the other sandy soils can only be classified as Arenosols, irrespective to their development rate, soil horizons sequence or ecological properties. Such arrangement does not reflect the real diversity of sandy soils, especially in comparison to the number of divisions covering soils of heavier texture. -
Alteration of Rocks by Endolithic Organisms Is One of the Pathways for the Beginning of Soils on Earth Received: 19 September 2017 Nikita Mergelov1, Carsten W
www.nature.com/scientificreports OPEN Alteration of rocks by endolithic organisms is one of the pathways for the beginning of soils on Earth Received: 19 September 2017 Nikita Mergelov1, Carsten W. Mueller 2, Isabel Prater 2, Ilya Shorkunov1, Andrey Dolgikh1, Accepted: 7 February 2018 Elya Zazovskaya1, Vasily Shishkov1, Victoria Krupskaya3, Konstantin Abrosimov4, Published: xx xx xxxx Alexander Cherkinsky5 & Sergey Goryachkin1 Subaerial endolithic systems of the current extreme environments on Earth provide exclusive insight into emergence and development of soils in the Precambrian when due to various stresses on the surfaces of hard rocks the cryptic niches inside them were much more plausible habitats for organisms than epilithic ones. Using an actualistic approach we demonstrate that transformation of silicate rocks by endolithic organisms is one of the possible pathways for the beginning of soils on Earth. This process led to the formation of soil-like bodies on rocks in situ and contributed to the raise of complexity in subaerial geosystems. Endolithic systems of East Antarctica lack the noise from vascular plants and are among the best available natural models to explore organo-mineral interactions of a very old “phylogenetic age” (cyanobacteria-to-mineral, fungi-to-mineral, lichen-to-mineral). On the basis of our case study from East Antarctica we demonstrate that relatively simple endolithic systems of microbial and/or cryptogamic origin that exist and replicate on Earth over geological time scales employ the principles of organic matter stabilization strikingly similar to those known for modern full-scale soils of various climates. Te pedosphere emergence is attributed to the most ancient forms of terrestrial life in the Early Precambrian which strongly aided the abiotic decay of rocks. -
Soil Taxonomy" in Particular ,
1. CONTROL NUMBER 2. SUBECT CLASSIFICATION (695) BIBLIOGRAPItlC DATA SHEET IN-AAJ-558 AF26-0000-0000 3. TITLE ANt) SUBTITLE (240) Experimental designs for predicting crop productivity with environmental and economic inputs for al rotcchnology transfer 4. PERSON.\I. AUTHORS (10P) Silva, J. A. 5. CORPORATE AUTHORS (101) Hawaii Univ. College of Tropical Agriculture 6. IDOCUMEN2< DATE (110)7. NUMBER OF PAGES (120) 8.ARC NUMBER [7 1981 13n631.5.S586b __ 9. R FRENCE ORGANIZATION (130) Hawaii 10. SUPI'PLEMENTARY NOTES (500) (In Departmental paper 49) 11. ABSTRACT (950) 12. DESCRIPTORS (920) 13. PROJECT NUMBER (150) Agricultural production Agricultural technology 931582C00 Technology transferi!Techoloy tansferYieldY e d14. CONTRACT NO.(I It)) 15. CONTRACT Soil fertility Experimentation TYPE (140) Tropics Productivity AID/ta-C-1108 Forecasting 16. TYPE OF DOCUMENT (160) AM 590-7 (10-79) Departmental Paper 49 Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva ...... ,..,... *** .......... ....* ...... .... .. 00400O 00€€€€*00 .. ...* Y Y*b***S4....... ~~~.eeeeeoeeeeeU ........ o .. *.4.............*e............ :0 ooee............. ........... ....... nae of T c.e Haw i. ns..ut. CollegeofTrpclgr.cut a UnversityoHa B....EMAR.SO University of Hawaiio~ee BENCHMAR SO I Le~eSPoJECTU/ADCotac o.t-C1 14.. C4 '4 t 10 wte IA:A 77 d E/ Adt , I 26Esi ',. ,~ )~'I *3-! * Ire ~ -I ~ 0 1 N Koel4 'I M M Experimental Designs for Predicting Crop Productivity with Environmental and Economic Inputs for Agrotechnology Transfer Edited by James A. Silva Benchmark Soils Project UH/AiD Contract No. to-C-1108 The Author James A. Silva is Soil Scientist and Principal Investigator, Benchmark Soils Project/Hawaii, Department of Agronomy and Soil Science, College of Tropical Agriculture and Human Resources, University of Hawaii, Honolulu. -
Evolution of Loess-Derived Soil Along a Topo-Climatic Sequence in The
European Journal of Soil Science, May 2017, 68, 270–280 doi: 10.1111/ejss.12425 Evolution of loess-derived soil along a climatic toposequence in the Qilian Mountains, NE Tibetan Plateau F. Yanga,c ,L.M.Huangb,c,D.G.Rossitera,d,F.Yanga,c,R.M.Yanga,c & G. L. Zhanga,c aState Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, NO. 71 East Beijing Road, Xuanwu District, Nanjing 210008, China, bKey Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, No. 11(A), Datun Road, Chaoyang District, Beijing 100101, China, cUniversity of the Chinese Academy of Sciences, No.19(A) Yuquan Road, Shijingshan District, Beijing 100049, China, and dSchool of Integrative Plant Sciences, Section of Soil and Crop Sciences, Cornell University, Ithaca NY 14853, USA Summary Holocene loess has been recognized as the primary source of the silty topsoil in the northeast Qinghai-Tibetan Plateau. The processes through which these uniform loess sediments develop into diverse types of soil remain unclear. In this research, we examined 23 loess-derived soil samples from the Qilian Mountains with varying amounts of pedogenic modification. Soil particle-size distribution and non-calcareous mineralogy were changed only slightly because of the weak intensity of chemical weathering. Accumulation of soil organic carbon (SOC) and leaching of carbonate were both identified as predominant pedogenic responses to soil forming processes. Principal component analysis and structural analysis revealed the strong correlations between soil carbon (SOC and carbonate) and several soil properties related to soil functions.