Site Evaluation and Soil Physical Modification
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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 -
Interim Soil Survey of the Gerber Block – Map Unit Descriptions 1
300A--Norcross very cobbly loam, 0 to 10 percent slopes Map Unit Setting MLRA: 21 Landscape: Tableland Elevation: 4800 to 5400 feet Precipitation: 16 to 20 inches Air temperature: 43 to 45 degrees Fahrenheit Frost-free period: 50 to 80 days Composition Norcross very cobbly ashy loam, 0 to 10 percent slopes--85 percent Casebeer very cobbly loam, 0 to 6 percent slopes--10 percent Rock Outcrop, 15 to 40 percent slopes--5 percent Component Description Norcross and similar soils Landform: Plateaus Parent material: Volcanic ash and residuum weathered from basalt Typical vegetation: low sagebrush, bluebunch wheatgrass, onespike oatgrass, Sandberg bluegrass, Idaho fescue Typical profile: A1--0 to 3 inches; very cobbly ashy loam A2--3 to 6 inches; cobbly ashy loam Bt1--6 to 10 inches; cobbly ashy clay loam Bt2--10 to 18 inches; clay Bt3--18 to 20 inches; clay Bqm--20 to 31 inches; duripan R--31 to 35 inches; unweathered bedrock See "Chemical Properties of Soils" table and the "Physical Properties of Soils" table for more information. Component Properties and Qualities Slope: 0 to 10 percent Runoff: High Depth to Restrictive Feature: Duripan: 12 to 20 inches Bedrock (lithic): 18 to 46 inches Permeability class (root zone): Slow Available water capacity: About 3 inches Present flooding: None Natural drainage class: Well drained Interpretive Groups Nonirrigated land capability: 6e Ecological site: 021XY216OR--Stony Claypan 14-20 Pz Typical soil descriptions including ranges in characteristics are in the "Classification of the Soils" section. Contrasting -
(Hardpan) for Precision Agriculture on So
SITE - SPECIFIC CHARACTERIZATION, MODELING AND SPATIAL ANALYSIS OF SUB-SOIL COMPACTION (HARDPAN) FOR PRECISION AGRICULTURE ON SOUTHEASTERN US SOILS by MEHARI ZEWDE TEKESTE (Under the Direction of Randy L. Raper and Ernest W. Tollner) ABSTRACT Natural and machinery traffic-induced subsoil compacted layers (soil hardpans) that are found in many southeastern US soils limit root growth with detrimental effects on crop productivity and the environment. Due to the spatial variability of hardpans, tillage management systems that use site-specific depth tillage applications may reduce fuel consumption compared to the conventional uniform depth tillage. The success of site-specific tillage or variable depth tillage depends on an accurate sensing of the hardpan layers, field positioning, and controlling the application of real-time or prescribed tillage. The over arching objective of the work was to understand and advance the art and science of soil compaction analysis and prediction with an eye towards compaction management in precision farming. The specific objectives were (1) To investigate the influences of soil parameters (soil moisture and bulk density), and the soil-cone frictional property on the interpretations of cone penetrometer data in predicting the magnitude and depth of hardpans, (2) To determine spatial variability for creating hardpan maps and (3) To investigate a passive acoustic based real-time soil compaction sensing method. The soil cone penetration problems were also modeled using finite element modeling to investigate the soil deformation patterns and evaluate the capability of the finite element method to predict the magnitude and depth of the hardpan. Laboratory experiments in a soil column study indicated that the soil cone penetration resistances were affected by soil moisture, bulk density and cone material type. -
HOW to IMPROVE SOIL DRAINAGE Charlotte Germane, Nevada County Master Gardener
GOT COMPACTION? HOW TO IMPROVE SOIL DRAINAGE Charlotte Germane, Nevada County Master Gardener From The Curious Gardener, Summer 2011 Do you suspect you might have a drainage problem in your garden? If your soil does not drain quickly enough, your plants will drown. Soils in the foothills Your soil drainage may not be as bad as you think it is. There’s so much talk in the foothills about clay soil that some gardeners assume they have poorly draining soil, and grumble about it, when they actually have pretty respectable loam. The USDA has mapped soil types and found that in the lower foothills the soil can be sandy loam over heavy sandy loam, or loam over clay loam. Above 2000 feet, it is typically loam over clay loam with cobblestones. An unusual feature of foothills soil is the serpentine outcropping. This combines poor drainage with toxic levels of magnesium. If you need to grow in a serpentine soil area, use raised beds. The serpentine soil under the beds will not provide adequate drainage. Another foothill soil issue that makes for poor drainage is “layered soil”. Soil naturally transitions from one kind to another, but layered soil means soil that changes abruptly, making it hard for water to move through easily. Layered soil occurs naturally (soil on top of rock or a clay pan) and can also be created by digging with rototillers and heavy equipment. Check for poor grading, over-irrigation, and thatched lawns Before you label your soil the culprit, walk your garden and evaluate the grading. It is possible that at the time of your home’s construction, or during a later landscaping project,the soil was graded so the water drained toward an area with no easy outlet. -
Agricultural Soil Compaction: Causes and Management
October 2010 Agdex 510-1 Agricultural Soil Compaction: Causes and Management oil compaction can be a serious and unnecessary soil aggregates, which has a negative affect on soil S form of soil degradation that can result in increased aggregate structure. soil erosion and decreased crop production. Soil compaction can have a number of negative effects on Compaction of soil is the compression of soil particles into soil quality and crop production including the following: a smaller volume, which reduces the size of pore space available for air and water. Most soils are composed of • causes soil pore spaces to become smaller about 50 per cent solids (sand, silt, clay and organic • reduces water infiltration rate into soil matter) and about 50 per cent pore spaces. • decreases the rate that water will penetrate into the soil root zone and subsoil • increases the potential for surface Compaction concerns water ponding, water runoff, surface soil waterlogging and soil erosion Soil compaction can impair water Soil compaction infiltration into soil, crop emergence, • reduces the ability of a soil to hold root penetration and crop nutrient and can be a serious water and air, which are necessary for water uptake, all of which result in form of soil plant root growth and function depressed crop yield. • reduces crop emergence as a result of soil crusting Human-induced compaction of degradation. • impedes root growth and limits the agricultural soil can be the result of using volume of soil explored by roots tillage equipment during soil cultivation or result from the heavy weight of field equipment. • limits soil exploration by roots and Compacted soils can also be the result of natural soil- decreases the ability of crops to take up nutrients and forming processes. -
Soils and Soil-Forming Material Technical Information Note 04 /2017 30Th November 2017
Soils and Soil-forming Material Technical Information Note 04 /2017 30th November 2017 Contents 1. Introduction to Soils ........................................................................................................................ 2 2. Components and Properties of Soil ................................................................................................ 7 3. Describing and Categorising soils .................................................................................................. 29 4. Policy, Regulation and Roles ......................................................................................................... 34 5. Soil Surveys, Handling and Management ..................................................................................... 40 6. Recommended Soil Specifications ................................................................................................ 42 7. References .................................................................................................................................... 52 “Upon this handful of soil our survival depends. Husband it and it will grow our food, our fuel, and our shelter and surround us with beauty. Abuse it and the soil will collapse and die, taking humanity with it.” From Vedas Sanskrit Scripture – circa 1500 BC The aim of this Technical Information Note is to assist Landscape Professionals (primarily landscape architects) when considering matters in relation to soils and soil-forming material. Soil is an essential requirement for providing -
EFFECT of TILLAGE on the HYDROLOGY of CLAYPAN SOILS in KANSAS by MEGHAN ELIZABETH BUCKLEY B.S., Iowa State University, 2002 M.S
CORE Metadata, citation and similar papers at core.ac.uk Provided by K-State Research Exchange EFFECT OF TILLAGE ON THE HYDROLOGY OF CLAYPAN SOILS IN KANSAS by MEGHAN ELIZABETH BUCKLEY B.S., Iowa State University, 2002 M.S., Kansas State University, 2004 AN ABSTRACT OF A DISSERTATION submitted in partial fulfillment of the requirements for the degree DOCTOR OF PHILOSOPHY Department of Agronomy College of Agriculture KANSAS STATE UNIVERSITY Manhattan, Kansas 2008 Abstract The Parsons soil has a sharp increase in clay content from the upper teens in the A horizon to the mid fifties in the Bt horizon. The high clay content continues to the parent material resulting in 1.5 m of dense, slowly permeable subsoil over shale residuum. This project was designed to better understand soil-water management needs of this soil. The main objective was to determine a comprehensive hydrologic balance for the claypan soil. Specific objectives were a) to determine effect of tillage management on select water balance components including water storage and evaporation, b) to quantify relationship between soil water status and crop variables such as emergence and yield, and c) to verify balance findings with predictions from a mechanistic model, specifically HYDRUS 1-D. The study utilized three replicates of an ongoing project in Labette County, Kansas in which till and no-till plots had been maintained in a sorghum [ Sorghum bicolor (L.) Moench] – soybean [Glycine max (L.) Merr.] rotation since 1995. Both crops are grown each year in a randomized complete block design. The sorghum plots were equipped with Time Domain Reflectometry (TDR) probes to measure A horizon water content and neutron access tubes for measurement of water throughout the profile. -
Hydraulic Properties in Different Soil Architectures of a Small Agricultural Watershed
water Article Hydraulic Properties in Different Soil Architectures of a Small Agricultural Watershed: Implications for Runoff Generation Cuiting Dai, Tianwei Wang, Yiwen Zhou, Jun Deng and Zhaoxia Li * College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China; [email protected] (C.D.); [email protected] (T.W.); [email protected] (Y.Z.); [email protected] (J.D.) * Correspondence: [email protected] Received: 25 October 2019; Accepted: 26 November 2019; Published: 1 December 2019 Abstract: Soil architecture exerts an important control on soil hydraulic properties and hydrological responses. However, the knowledge of hydraulic properties related to soil architecture is limited. The objective of this study was to investigate the influences of soil architecture on soil physical and hydraulic properties and explore their implications for runoff generation in a small agricultural watershed in the Three Gorges Reservoir Area (TGRA) of southern China. Six types of soil architecture were selected, including shallow loam sandy soil in grassland (SLSG) and shallow loam sandy soil in cropland (SLSC) on the shoulder; shallow sandy loam in grassland (SSLG) and shallow sandy loam in cropland (SSLC) on the backslope; and deep sandy loam in grassland (DSLG) and deep sandy loam in cropland (DSLC) on the footslope. The results showed that saturated hydraulic conductivity 1 (Ksat) was significantly higher in shallow loamy sand soil under grasslands (8.57 cm h− ) than under 1 croplands (7.39 cm h− ) at the topsoil layer. Total porosity was highest for DSLC and lowest for SSLG, averaged across all depths. The proportion of macropores under SLSG was increased by 60% compared with under DSLC, which potentially enhanced water infiltration and decreased surface runoff. -
Sustainable Soil Management
Top of Form ATTRAv2 page skip navigation 500 500 500 500 500 0 Search Bottom of Form 800-346-9140 Home | Site Map | Who We Are | Contact (English) Us | Calendar | Español | Text Only 800-411-3222 (Español) Home > Master Publication List > Sustainable Soil Management What Is Sustainable Soil Management Sustainable Agriculture? The printable PDF version of the Horticultural By Preston Sullivan entire document is available at: Crops NCAT Agriculture Specialist http://attra.ncat.org/attra- © NCAT 2004 pub/PDF/soilmgmt.pdf Field Crops ATTRA Publication #IP027/133 31 pages — 1.5 mb Download Acrobat Reader Soils & Compost Water Management Pest Management Organic Farming Livestock Marketing, Business & Risk Abstract Soybeans no-till planted into Management wheat stubble. This publication covers basic soil Photo by: Preston Sullivan Farm Energy properties and management steps toward building and maintaining healthy soils. Part I deals with basic Education soil principles and provides an understanding of living soils and how they work. In this section you will find answers to why soil organisms Other Resources and organic matter are important. Part II covers management steps to build soil quality on your farm. The last section looks at farmers who Master have successfully built up their soil. The publication concludes with a Publication List large resource section of other available information. Table of Contents Top of Form Part I. Characteristics of Sustainable Soils o Introduction o The Living Soil: Texture and Structure o The Living Soil: The Importance of Soil Organisms 1011223551022 o Organic Matter, Humus, and the Soil Foodweb o Soil Tilth and Organic Matter oi o Tillage, Organic Matter, and Plant Productivity o Fertilizer Amendments and Biologically Active Soils Go o Conventional Fertilizers Enter your o Top$oil—Your Farm'$ Capital email above o Summary of Part I and click Go. -
Nitrate Distribution in a Deep, Alluvial Unsaturated Zone: Geologic Control Vs
Nitrate Distribution in a Deep, Alluvial Unsaturated Zone: Geologic Control vs. Fertilizer Management Thomas Harter*, Katrin Heeren, William R. Horwath Department of Land, Air, and Water Resources University of California Davis, CA 95616 * corresponding author ph/530-752-2709; [email protected]; http://groundwater.ucdavis.edu Introduction For decades, nitrate leaching from agricultural sources (among others) has been a concern to agronomists, soil scientists, and hydrologists. Federal legislation first recognized the potential impacts to water resources in the early 1970s, when the Clean Water Act (CWA), the Safe Drinking Water Act (SDWA), the Federal Insecticide, Fungicide, and Rodenticide Act (FIFRA), and other water pollution related legislation was enacted. Since then, countless efforts have been mounted by both the scientific-technical community and the agricultural industry to better understand the role of agricultural practices in determining the fate of fertilizer and pesticides in watersheds (including groundwater) and to improve agricultural management accordingly. From a groundwater perspective, much of the scientific work relating to nitrate has focused on two areas: documenting the extent of groundwater nitrate contamination; and investigating the fate of nitrogen in the soil root zone (including the potential for groundwater leaching) as it relates to particular agricultural crops and management practices. Rarely, these two research areas are linked within a single study and if they are, groundwater levels are typically close to the soil surface (less than 10 feet). In California’s valleys and basins, particularly in Central and Southern California, groundwater levels are frequently much deeper than 20 feet. The unsaturated zone between the land surface and the water table may therefore be from 20 to over 100 feet thick. -
Seed and Soil Dynamics in Shrubland Ecosystems: Proceedings; 2002 August 12–16; Laramie, WY
United States Department of Agriculture Seed and Soil Dynamics in Forest Service Rocky Mountain Shrubland Ecosystems: Research Station Proceedings Proceedings RMRS-P-31 February 2004 Abstract Hild, Ann L.; Shaw, Nancy L.; Meyer, Susan E.; Booth, D. Terrance; McArthur, E. Durant, comps. 2004. Seed and soil dynamics in shrubland ecosystems: proceedings; 2002 August 12–16; Laramie, WY. Proc. RMRS-P-31. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 216 p. The 38 papers in this proceedings are divided into six sections; the first includes an overview paper and documentation of the first Shrub Research Consortium Distinguished Service Award. The next four sections cluster papers on restoration and revegetation, soil and microsite requirements, germination and establishment of desired species, and community ecology of shrubland systems. The final section contains descriptions of the field trips to the High Plains Grassland Research Station and to the Snowy Range and Medicine Bow Peak. The proceedings unites many papers on germination of native seed with vegetation ecology, soil physio- chemical properties, and soil biology to create a volume describing the interactions of seeds and soils in arid and semiarid shrubland ecosystems. Keywords: wildland shrubs, seed, soil, restoration, rehabilitation, seed bank, seed germination, biological soil crusts Acknowledgments The symposium, field trips, and subsequent publication of this volume were made possible through the hard work of many people. We wish to thank everyone who took a part in ensuring the success of the meetings, trade show, and paper submissions. We thank the University of Wyoming Office of Academic Affairs, the Graduate School, and its Dean, Dr. -
Earthworms by Clarence Chavez
Of all the members of the soil food web, earthworms need the least introduction Charles Darwin wrote: “It may be doubted whether there are many other animals which have played so important a part in the history of the world, as have these lowly organized creatures.” Earthworms By Clarence Chavez Where and how many? Count and Sort Dig a hole 1’ X 1’ x 1’ Add Mustard Solution (optional): about 1/2 cup of mustard to 3 or 4 gallons of water. Stir well so that the solution is thoroughly mixed. Pour into the hole. Interpretation of earthworms Earthworm populations may vary with site characteristics (food availability and soil conditions), season, and species. Note: About 10 earthworms per square foot of soil (100 worms/m2) is generally considered a good, higher counts are better. Earthworms - reproduction Earthworms are hermaphrodites, meaning that they exhibit both male and female characteristics. But you still need two to start a colony. Earthworm Cocooning Young worms hatch from their cocoons in three weeks to five months as the gestation period varies for different species of worms. Conditions like temperature and soil moisture factor in here...if conditions are not great then hatching is delayed The ideal temperature is around fifty-five degrees, allowing earthworms to mate in the spring or fall. Earthworms - decomposers Soil and Water Management Research Unit Management Research and Water Soil Earthworms derive their nutrition from dead and decomposing organic matter. Things like decaying roots and leaves, and living organisms such as nematodes, protozoan's, rotifers, bacteria, fungi. They fragment organic matter and make major contributions to recycling the nutrients it contains.