Field Book for Describing and Sampling Soils
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Coastal Processes and Causes of Shoreline Erosion and Accretion Causes of Shoreline Erosion and Accretion
Coastal Processes and Causes of Shoreline Erosion and Accretion and Accretion Erosion Causes of Shoreline Heather Weitzner, Great Lakes Coastal Processes and Hazards Specialist Photo by Brittney Rogers, New York Sea Grant York Photo by Brittney Rogers, New New York Sea Grant Waves breaking on the eastern Lake Ontario shore. Wayne County Cooperative Extension A shoreline is a dynamic environment that evolves under the effects of both natural 1581 Route 88 North and human influences. Many areas along New York’s shorelines are naturally subject Newark, NY 14513-9739 315.331.8415 to erosion. Although human actions can impact the erosion process, natural coastal processes, such as wind, waves or ice movement are constantly eroding and/or building www.nyseagrant.org up the shoreline. This constant change may seem alarming, but erosion and accretion (build up of sediment) are natural phenomena experienced by the shoreline in a sort of give and take relationship. This relationship is of particular interest due to its impact on human uses and development of the shore. This fact sheet aims to introduce these processes and causes of erosion and accretion that affect New York’s shorelines. Waves New York’s Sea Grant Extension Program Wind-driven waves are a primary source of coastal erosion along the Great provides Equal Program and Lakes shorelines. Factors affecting wave height, period and length include: Equal Employment Opportunities in 1. Fetch: the distance the wind blows over open water association with Cornell Cooperative 2. Length of time the wind blows Extension, U.S. Department 3. Speed of the wind of Agriculture and 4. -
Editorial for Special Issue “Ore Genesis and Metamorphism: Geochemistry, Mineralogy, and Isotopes”
minerals Editorial Editorial for Special Issue “Ore Genesis and Metamorphism: Geochemistry, Mineralogy, and Isotopes” Pavel A. Serov Geological Institute of the Kola Science Centre, Russian Academy of Sciences, 184209 Apatity, Russia; [email protected] Magmatism, ore genesis and metamorphism are commonly associated processes that define fundamental features of the Earth’s crustal evolution from the earliest Precambrian to Phanerozoic. Basically, the need and importance of studying the role of metamorphic processes in formation and transformation of deposits is of great value when discussing the origin of deposits confined to varied geological settings. In synthesis, the signatures imprinted by metamorphic episodes during the evolution largely indicate complicated and multistage patterns of ore-forming processes, as well as the polygenic nature of the mineralization generated by magmatic, postmagmatic, and metamorphic processes. Rapid industrialization and expanding demand for various types of mineral raw ma- terials require increasing rates of mining operations. The current Special Issue is dedicated to the latest achievements in geochemistry, mineralogy, and geochronology of ore and metamorphic complexes, their interrelation, and the potential for further prospecting. The issue contains six practical and theoretical studies that provide for a better understanding of the age and nature of metamorphic and metasomatic transformations, as well as their contribution to mineralization in various geological complexes. The first article, by Jiang et al. [1], reports results of the first mineralogical–geochemical Citation: Serov, P.A. Editorial for studies of gem-quality nephrite from the major Yinggelike deposit (Xinjiang, NW China). Special Issue “Ore Genesis and The authors used a set of advanced analytical techniques, that is, electron probe microanaly- Metamorphism: Geochemistry, sis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry Mineralogy, and Isotopes”. -
Nichols Arboretum: Soil Types
Nichols Arboretum: Soil Types Not Present in Arboretum Boyer Sandy Loam 0-6% Slopes Fox Sandy Loam 6-12% Slopes Miami Loam 2-6% Slopes Miami Loam 6-12% Slopes Miami Loam 12-18% Slopes Miami Loam 18-25% Slopes Miami Loam 25-35% Slopes Sloan Silt Loam, Wet Water Wasepi Sandy Loam 0-4% Slopes Mary Hejna : September 2012 0 0.125 0.25 Miles Data from NRCS Soil Survey t Soil Series Descriptions BOYER SERIES The Boyer series consists of very deep, well drained soils formed in USE AND VEGETATION sandy and loamy drift underlain by sand or gravelly sand outwash at Soils are cultivated in most areas. Principal crops are corn, small depths of 51 to 102 cm (20 to 40 inches). grain, soybeans, field beans, and alfalfa hay. A few areas remain in GEOGRAPHIC SETTING permanent pasture or forest. The dominant forest trees are oaks, hickories, and maples. Boyer soils are on outwash plains, valley trains, kames, beach ridges, river terraces, lake terraces, deltas, and moraines of Wisconsinan age. TYPICAL PEDON The slope gradients are dominantly 0 to 12 percent, but range from 0 Boyer loamy sand, on a 4 percent slope in a cultivated field. (Colors to 50 percent. Boyer soils formed in sandy and loamy drift underlain are for moist soil unless otherwise stated.) by sand or gravelly sand outwash at depths of 51 to 102 cm (20 to 40 inches). Quartz is the dominant mineral in the 3C horizon, which Ap--0 to 18 cm (7 inches); dark grayish brown (10YR 4/2) loamy contains, in addition, varying amounts of material from igneous and sand, light brownish gray (10YR 6/2) dry; weak fine granular metamorphic rocks, limestone, and dolomite. -
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 ................. -
Hydrogeology of Near-Shore Submarine Groundwater Discharge
Hydrogeology and Geochemistry of Near-shore Submarine Groundwater Discharge at Flamengo Bay, Ubatuba, Brazil June A. Oberdorfer (San Jose State University) Matthew Charette, Matthew Allen (Woods Hole Oceanographic Institution) Jonathan B. Martin (University of Florida) and Jaye E. Cable (Louisiana State University) Abstract: Near-shore discharge of fresh groundwater from the fractured granitic rock is strongly controlled by the local geology. Freshwater flows primarily through a zone of weathered granite to a distance of 24 m offshore. In the nearshore environment this weathered granite is covered by about 0.5 m of well-sorted, coarse sands with sea water salinity, with an abrupt transition to much lower salinity once the weathered granite is penetrated. Further offshore, low-permeability marine sediments contained saline porewater, marking the limit of offshore migration of freshwater. Freshwater flux rates based on tidal signal and hydraulic gradient analysis indicate a fresh submarine groundwater discharge of 0.17 to 1.6 m3/d per m of shoreline. Dissolved inorganic nitrogen and silicate were elevated in the porewater relative to seawater, and appeared to be a net source of nutrients to the overlying water column. The major ion concentrations suggest that the freshwater within the aquifer has a short residence time. Major element concentrations do not reflect alteration of the granitic rocks, possibly because the alteration occurred prior to development of the current discharge zones, or from elevated water/rock ratios. Introduction While there has been a growing interest over the last two decades in quantifying the discharge of groundwater to the coastal zone, the majority of studies have been carried out in aquifers consisting of unlithified sediments or in karst environments. -
Landform Regions of Iowa — 2000
LANDFORM REGIONS OF IOWA LANDFORM REGIONS2000 OF IOWA — 2000 0 20 40 60 miles 0 20 40 60 miles 0 40 80 kilometers 0 40 80 kilometers 327 Trowbridge Hall Iowa Department of NaturalIowa City, Resources Iowa 52242-1319 Geological Survey Bureau 109 Trowbridge Hallwww.iowageologicalsurvey.org Iowa City, Iowa 52242-1319 319-335-1575 Hydroscience & Engineering www.igsb.uiowa.edu Printed on recycled paper A landscape is a collection of shapes or landforms. LANDFORM REGIONS In Iowa, these shapes are composed of earth materials OF IOWA derived from glacial, wind, river, and marine environments of the geologic past. This map is a guide to seeing the state’s remarkably diverse landscapes and www.iowageologicalsurvey.org landform features. 319-335-1575 The Des Moines Lobe Southern Iowa Drift Plain Paleozoic Plateau The last glacier to enter Iowa advanced in a series of surges This region is dominated by glacial deposits left by ice Narrow valleys deeply carved into sedimentary rock beginning just 15,000 years ago and reached its southern sheets that extended south into Missouri over 500,000 of Paleozoic age and a near-absence of glacial deposits limit, the site of modern-day Des Moines, 14,000 years years ago. The deposits were carved by deepening define this scenic region. Fossil-bearing strata originated ago. By 12,000 years ago, the ice sheet was gone, leaving episodes of stream erosion so that only a horizon line as sediment on tropical sea floors between 300 and 550 behind a poorly drained landscape of pebbly deposits of hill summits marks the once-continuous glacial plain. -
Metamorphic Rocks (Lab )
Figure 3.12 Igneous Rocks (Lab ) The RockSedimentary Cycle Rocks (Lab ) Metamorphic Rocks (Lab ) Areas of regional metamorphism Compressive Compressive Stress Stress Products of Regional Metamorphism Products of Contact Metamorphism Foliated texture forms Non-foliated texture forms during compression during static pressure Texture Minerals Other Diagnostic Metamorphic Protolith Features Rock Name Non-foliated calcite, dolomite cleavage faces of Marble Limestone calcite usually visible quartz quartz grains are Quartzite Quartz Sandstone intergrown Foliated clay looks like shale but Slate Shale breaks into layers muscovite, biotite very fine-grained, but Phyllite Shale has a sheen like satin muscovite, biotite, minerals are large Schist Shale may have garnet enough to see easily, muscovite and biotite grains are parallel to each other feldspar, biotite, has layers of different Gneiss Any protolith muscovite, quartz, minerals garnet amphibole layered black Amphibolite Basalt or Andesite amphibole grains Texture Minerals Other Diagnostic Metamorphic Protolith Features Rock Name Non-foliated calcite, dolomite cleavage faces of Marble Limestone calcite usually visible quartz quartz grains are Quartzite Quartz Sandstone intergrown Foliated clay looks like shale but Slate Shale breaks into layers muscovite, biotite very fine-grained, but Phyllite Shale has a sheen like satin muscovite, biotite, minerals are large Schist Shale may have garnet enough to see easily, muscovite and biotite grains are parallel to each other feldspar, biotite, has layers of different Gneiss Any protolith muscovite, quartz, minerals garnet amphibole layered black Amphibolite Basalt or Andesite amphibole grains Identification of Metamorphic Rocks 12 samples 7 are metamorphic 5 are igneous or sedimentary Protoliths and Geologic History For 2 of the metamorphic rocks: Match the metamorphic rock to its protolith (both from Part One) Write a short geologic history of the sample 1. -
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. -
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. -
NSF 03-021, Arctic Research in the United States
This document has been archived. Home is Where the Habitat is An Ecosystem Foundation for Wildlife Distribution and Behavior This article was prepared The lands and near-shore waters of Alaska remaining from recent geomorphic activities such by Page Spencer, stretch from 48° to 68° north latitude and from 130° as glaciers, floods, and volcanic eruptions.* National Park Service, west to 175° east longitude. The immense size of Ecosystems in Alaska are spread out along Anchorage, Alaska; Alaska is frequently portrayed through its super- three major bioclimatic gradients, represented by Gregory Nowacki, USDA Forest Service; Michael imposition on the continental U.S., stretching from the factors of climate (temperature and precipita- Fleming, U.S. Geological Georgia to California and from Minnesota to tion), vegetation (forested to non-forested), and Survey; Terry Brock, Texas. Within Alaska’s broad geographic extent disturbance regime. When the 32 ecoregions are USDA Forest Service there are widely diverse ecosystems, including arrayed along these gradients, eight large group- (retired); and Torre Arctic deserts, rainforests, boreal forests, alpine ings, or ecological divisions, emerge. In this paper Jorgenson, ABR, Inc. tundra, and impenetrable shrub thickets. This land we describe the eight ecological divisions, with is shaped by storms and waves driven across 8000 details from their component ecoregions and rep- miles of the Pacific Ocean, by huge river systems, resentative photos. by wildfire and permafrost, by volcanoes in the Ecosystem structures and environmental Ring of Fire where the Pacific plate dives beneath processes largely dictate the distribution and the North American plate, by frequent earth- behavior of wildlife species. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Soil Survey of Walworth County, Wisconsin
Issued February 1971 . SOIL SURVEY . .W alworthCounty I Wisconsin UNITED STATES DEPARTMENT OF AGRICULTURE Soil Conservation Service In cooperation with -- .. UNIVERSITY OF WISCONSIN Wisconsin Geological and Natural History Survey Soils Department, and Wisconsin Agricultural Experiment Station Major fieldwork for this soil survey was done in the period 1959-64. Soil names and descriptions were approved in 1966. Unless otherwise indicated, statements in this publication refer- to conditions in the county in 1966. This survey was made cooperatively by the Soil Conservation Service and the Wisconsin Geological and Natural History Survey, Soils Department, and the Wisconsin Agricultural Experiment Station, University of Wisconsin. It is part of the technical assistance furnished to the Walworth County Soil and Water Conservation District. The fieldwork that is the basis for this soil survey was partly financed. by the Southeastern Wisconsin Regional Planning Commission; by a joint planning grant from the State Highway Commission of Wisconsin; by the U.S. Department of Commerce, Bureau of Public Roads; and by the Department of Housing and Urban Development under the provisions of the Federal Aid to Highways legislation and section 701 of the Housing Act of 1954, as amended. Either enlarged or reduced copies of the soil map in this publication can be made by commercial photographers, or they can be purchased on individual order from the Cartographic Division, Soil Conservation Service, U.S. Department of Agriculture, Washington, D.C. 20250. HOW TO USE THIS SOIL SURVEY HIS SOIL SURVEY contains informa- an oved.ay over the soil map an? ?olo!,ed to Ttion that can be applied in managing farms sh?w ?(:nls that have ,bhe sal!le hm~tatIOn or .