Continuous Cropping Alters Multiple Biotic and Abiotic Indicators of Soil Health
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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 -
Evaluation of Humic Substances Used in Commercial Fertilizer Formulations
Final report FREP Project 07-0174 Evaluation of humic substances used in commercial fertilizer formulations T.K. Hartz Extension Specialist Department of Plant Sciences University of California 1 Shields Ave Davis, CA 95616 (530) 752-1738 [email protected] Executive summary: This project examined the effects of five commercial humic acid formulations on soil microbial activity, seed germination, early growth, nutrient uptake and crop productivity of lettuce and processing tomato. Humic acid solutions ranging from 250-750 PPM a.i. were used to imbibe coated lettuce seed; those seeds germinated at the same rate and frequency as seed imbibed with deionized water. In a greenhouse trial lettuce plants were grown from seed in pots of four field soils differing in phosphorus availability. The pots received pre-seeding banded application of humic acid alone, P fertilization (liquid 10-34- 0) alone, both humic acid and P fertilization, or neither treatment. In one of the four soils humic acid plus P increased lettuce growth above that of P fertilization alone. In the absence of P fertilization, no humic acid formulation increased lettuce growth in any soil. P fertilization increased plant P uptake in all soils, but humic acid did not increase P uptake in any soil. The effect of humic acid on soil microbial activity was evaluated in a laboratory assay using a low organic matter soil and a high organic matter soil (0.8 and 2.5% organic matter, respectively). The soils were wetted with tap water alone, P fertilizer solution, humic acid solution, or a solution containing both humic acid and P fertilizer. -
Hydrologic Soil Groups
AppendixExhibitAppendix A: Hydrologic AB Soil Synthetic Groups Hydrologic for theRainfall United SoilStates Distributions Groups and Rainfall Data Sources Soils are classified into hydrologic soil groups (HSG’s) Disturbed soil profiles to indicate the minimum rate of infiltration obtained for bareThe highest soil after peak prolonged discharges wetting. from Thesmall HSG watersheds’s, which arein the UnitedAs a result States of areurbanization, usually caused the soil by profileintense, may brief be rain- con- A,falls B, that C, and may D, occur are one as distinctelement eventsused in or determining as part of a longersiderably storm. These altered intense and the rainstorms listed group do not classification usually ex- may runofftended curve over anumbers large area (see and chapter intensities 2). For vary the greatly. conve- One commonno longer practice apply. inIn rainfall-runoffthese circumstances, analysis use is tothe develop follow- niencea synthetic of TR-55 rainfall users, distribution exhibit A-1 to uselists in the lieu HSG of actualclassifi- storming events. to determine This distribution HSG according includes to themaximum texture rainfall of the cationintensities of United for the States selected soils. design frequency arranged in a sequencenew surface that soil, is critical provided for thatproducing significant peak compaction runoff. has not occurred (Brakensiek and Rawls 1983). TheSynthetic infiltration raterainfall is the rate distributions at which water enters the soil at the soil surface. It is controlled by surface condi- HSG Soil textures tions.The length HSG ofalso the indicates most intense the transmission rainfall period rate contributing—the rate to the peak runoff rate is related to the time of concen- A Sand, loamy sand, or sandy loam attration which (T thec) for water the watershed.moves within In thea hydrograph soil. -
COONAWARRA \ Little Black Book Cover Image: Ben Macmahon @Macmahonimages COONAWARRA \
COONAWARRA \ Little Black Book Cover image: Ben Macmahon @macmahonimages COONAWARRA \ A small strip of land in the heart of the Limestone Coast in South Australia. Together our landscape, our people and our passion, work in harmony to create a signature wine region that delivers on a myriad of levels - producing wines that unmistakably speak of their place and reflect the character of their makers. It’s a place that gets under your skin, leaving an indelible mark, for those who choose it as home and for those who keep coming back. We invite you to Take the Time... Visit. Savour. Indulge. You’ll smell it, taste it and experience it for yourself. COONAWARRA \ Our Story Think Coonawarra, and thoughts of There are the ruddy cheeks of those who tend the vines; sumptuous reds spring to mind – from the the crimson sunsets that sweep across a vast horizon; and of course, there’s the fiery passion in the veins of our rich rust-coloured Terra Rossa soil for which vignerons and winemakers. Almost a million years ago, it’s internationally recognised, to the prized an ocean teeming with sea-life lapped at the feet of the red wines that have made it famous. ancient Kanawinka Escarpment. Then came an ice age, and the great melt that followed led to the creation of the chalky white bedrock which is the foundation of this unique region. But nature had not finished, for with her winds, rain and sand she blanketed the plain with a soil rich in iron, silica and nutrients, to become one of the most renowned terroir soils in the world. -
Phosphorus Adsorption of Some Brazilian Soils in Relations to Selected Soil Properties
Open Journal of Soil Science, 2015, 5, 101-109 Published Online May 2015 in SciRes. http://www.scirp.org/journal/ojss http://dx.doi.org/10.4236/ojss.2015.55010 Phosphorus Adsorption of Some Brazilian Soils in Relations to Selected Soil Properties Valdinar Ferreira Melo1*, Sandra Cátia Pereira Uchôa1, Zachary N. Senwo2*, Ronilson José Pedroso Amorim3 1Department of Soil and Agricultural Engineering, Federal University of Roraima, Boa Vista, Brazil 2Department of Biological & Environmental Sciences, Alabama A&M University, Huntsville, USA 3Agronomy, Federal University of Roraima, Boa Vista, Brazil Email: *[email protected], *[email protected] Received 3 April 2015; accepted 17 May 2015; published 20 May 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract A major nutritional problem to crops grown in highly weathered Brazilian soils is phosphorus (P) deficiencies linked to their low availability and the capacity of the soils to fix P in insoluble forms. Our studies examined factors that might influence P behavior in soils of the Amazon region. This study was conducted to evaluate the maximum phosphate adsorption capacity (MPAC) of the soils developed from mafic rocks (diabase), their parent materials and other factors resulting in the formation of eutrophic soils having A chernozemic horizon associated with Red Nitosols (Alfisol) and Red Latosols (Oxisol) of the Amazonian environment. The MPAC was determined in triplicates as a function of the remnant P values. The different concentrations used to determine the MPAC allowed maximum adsorption values to be reached for all soils. -
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 -
Soil Fertility Research in Sugarcane in 2007
SOIL FERTILITY RESEARCH IN SUGARCANE IN 2007 Brenda S. Tubaña, Chuck Kennedy, Allen Arceneaux and Jasper Teboh School of Plant, Environmental and Soil Sciences In Cooperation with Sugar Research Station Summary Two experiments were conducted in 2007 to test the effect of different N rates on the yield and yield components of current sugarcane varieties. Spring application of N at rates of 0, 40, 80 and 120 lbs N ac -1 to LCP85-384, HoCP96-540 and L99-226 had no effect on plantcane yield. However, 40 and 80 lbs N ac -1 resulted in significantly higher sugar yield when compared with 120 lbs N ac -1 application rate. Stubble cane yield of LCP85-384, Ho95-988, and L97-128 showed response to spring N fertilization. Linear-plateau models estimated N rates that ranged from 42 to 80 lbs N ac -1 for optimum cane and sugar yield of these varieties. Two trials were also conducted to determine the effect of fertilizer adjuvant. Applications of Trimat, PGR and foliar NPK in addition with normal fertilization did not result in significant increases in the first- stubble cane and sugar yield of Ho95-988 and L97-128. Similarly, application of Helena Chemical products on top on standard practices did not result in significant increases in second- stubble cane and sugar yield of L97-128. Objectives This research was designed to provide information on soil fertility in an effort to help cane growers produce maximum economic yields and increase profitability in sugarcane production. This annual progress report is presented to provide the latest available data on certain practices and not as a final recommendation for growers to use all of these practices. -
Soil Survey of Sequoia National Forest, California (1996) Part II of II
622 Dome-Chaix outcrop association, 30 to 50 percent slopes. Illlil This map unit is on mountainsides and ridges. Slope is 30 to 50 percent. The native plant communities are Yellow Pine Forest and Mixed Conifer Forest. Elevation is 5,000 to 8,040 feet. The average annual precipitation is about 24 to 51 inches. This unit is 35 percent Dome sandy loam, 30 percent Chaix sandy loam, and 20 percent Rock outcrop. Dome Chaix Rock outcrop 40 to 60 in 20 to 40 in Moderate to low Low t 5 to 6 in 3 to 4 in | 2 in 2 in I Moderately rapid Moderately rapid B B Well drained Well drained or somewhat excessively drained Rapid Rapid Moderate Moderate 0.20 0.24 ^ SM SM Intermediate Intermediate 2ep 3eP 85 to 164 50 to 84 Suitable Suitable Regeneration difficulty—d and f Summer Summer Plant competition, steep slopes II II Included in this unit are small areas of Chawanakee soils and Junipero family soils. Included areas make up about 15 percent of the total acreage. The Dome soil is deep and formed in residuum derived from granitic rock. Typically, the surface layer is grayish brown sandy loam about 7 inches thick. The subsoil is pale brown sandy loam about 21 inches thick. The subsoil is very pale brown sandy loam about 22 inches thick over highly weathered granitic rock. In some areas the surface layer is coarse sandy loam. The Chaix soil is moderately deep and formed in residuum derived from granitic rock. Typically, the surface layer is brown sandy loam about 7 inches thick. -
Geology As a Georegional Influence on Quercus Fagaceae Distribution
GEOLOGY AS A GEOREGIONAL INFLUENCE ON Quercus FAGACEAE DISTRIBUTION IN DENTON AND COKE COUNTIES OF CENTRAL AND NORTH CENTRAL TEXAS AND CHOCTAW COUNTY OF SOUTHEASTERN OKLAHOMA, USING GIS AS AN ANALYTICAL TOOL George F. Maxey, B.S., M.S. Dissertation Prepared for the Degree of DOCTOR OF PHILOSOPHY UNIVERSITY OF NORTH TEXAS December 2007 APPROVED: C. Reid Ferring, Major Professor Miguel Avevedo, Committee Member Kenneth Dickson, Committee Member Donald Lyons, Committee Member Paul Hudak, Committee Member and Chair of the Department of Geography Sandra L. Terrell, Dean of the Robert B. Toulouse School of Graduate Studies Maxey, George F. Geology as a Georegional Influence on Quercus Fagaceae Distribution in Denton and Coke Counties of Central and North Central Texas and Choctaw County of Southeastern Oklahoma, Using GIS as an Analytical Tool. Doctor of Philosophy (Environmental Science), December 2007, 198 pp., 30 figures, 24 tables, references, 57 titles. This study elucidates the underlying relationships for the distribution of oak landcover on bedrock and soil orders in two counties in Texas and one in Oklahoma. ESRI’s ArcGis and ArcMap was used to create surface maps for Denton and Coke Counties, Texas and Choctaw County, Oklahoma. Attribute tables generated in GIS were exported into a spreadsheet software program and frequency tables were created for every formation and soil order in the tri-county research area. The results were both a visual and numeric distribution of oaks in the transition area between the eastern hardwood forests and the Great Plains. Oak distributions are changing on this transition area of the South Central Plains. -
Perennial Grain Crop Roots and Nitrogen Management Shape Soil Food Webs T and Soil Carbon Dynamics ∗ Christine D
Soil Biology and Biochemistry 137 (2019) 107573 Contents lists available at ScienceDirect Soil Biology and Biochemistry journal homepage: www.elsevier.com/locate/soilbio Perennial grain crop roots and nitrogen management shape soil food webs T and soil carbon dynamics ∗ Christine D. Sprungera, , Steven W. Culmana, Ariane L. Peraltab, S. Tianna DuPontc, Jay T. Lennond, Sieglinde S. Snappe a School of Environment and Natural Resources, The Ohio State University, Wooster, OH, 44691, USA b Department of Biology, East Carolina University, Greenville, NC, 27858, USA c Tree Fruit Research and Extension, Washington State University, Wenatchee, WA, 98801, USA d Department of Biology, Indiana University, Bloomington, IN, 47405, USA e Department of Plant, Soil, and Microbial Sciences, Michigan State University, East Lansing, MI, 48824, USA ARTICLE INFO ABSTRACT Keywords: Perennial grain crops may confer greater ecosystem services relative to annual row crop systems due to their Organic matter extensive roots systems and year-round ground cover. However, less is known about the extent to which per- Root biomass ennial grain crops affect food web dynamics and soil carbon (C) cycling over time. Furthermore, manyme- Nematodes chanistic questions remain regarding the influence of root quantity and quality on soil biological communities Bacteria and C cycling function. In this study, we quantified root biomass and quality, bacterial and nematode community Soil food webs structure, and labile soil C pools of perennial intermediate wheatgrass [Thinopyrum intermedium (Host) Buckworth and Dewey] and annual winter wheat (Triticum aes L.) across three nitrogen (N) management systems (Organic, Low inorganic N, High inorganic N). After 4 years, the perennial grain crop had significantly greater root quantity and permanganate oxidizable carbon (POXC) relative to annual wheat. -
The Soil Orders of Texas
The Soil Orders of Texas The system for classifying soils, Soil Taxonomy, is used worldwide. The highest level of Soil Taxonomy is the Soil Order. There are 12 recognized soil orders in the world. Of these, the state of Texas has 9. There are more than 1,300 soil series in Texas, and each series is classified in one of these 9 soil orders. The Dominant Soil Orders map represents the general distribution of 7 of the 9 soil orders in Texas. The 7 soil orders, Alfisols, Aridisols, Entisols, Inceptisols, Mollisols, Ultisols, and Vertisols, are mapped extensively in the state. The other 2 soil orders, Histosols and Spodosols, which are mapped in the southeastern part of the state, are not shown on the map because they cover relatively small areas. The soil orders not found in Texas are Andisols (volcanic soils), Gelisols (frozen soils), and Oxisols (highly weathered tropical soils). Alfisols Inceptisols The Duval series is an example of an Alfisol. Alfisols have a subsurface The Weswood series is an example of an Inceptisol. Inceptisols are soils with accumulation of clay and have greater than or equal to 35 percent base weakly developed subsurface horizons. These soils may be shallow to saturation. Duval soils occur in the Northern and Western Rio Grande Plain on bedrock, occur on steeply sloping land, or they may be very deep soils in nearly level to gently sloping uplands. areas subject to intermittent flooding. Weswood soils occur along the flood plains of the Brazos and Colorado Rivers in central Texas. Aridisols Mollisols The Upton series is an example of an Aridisol. -
Harnessing the Benefits of Soil Biology in Conservation Agriculture Vadakattu Gupta, Margaret Roper and John Thompson
Chapter 15 Harnessing the benefits of soil biology in conservation agriculture Vadakattu Gupta, Margaret Roper and John Thompson Soil biology and ecology in conservation agriculture “Soil, the 1 m skin of the earth, sustains all life forms in the terrestrial ecosystem and is vital to the very existence and substance of human life” (Dick 2018). Soils function as biological entities due to the microbial communities that exist within them. It is estimated that in 1 kg of soil, there are more than 1 billion bacteria and >2 km of fungal hyphae. More than 95% of soil microbial species are non- culturable, but metagenomic analysis of nucleic acids is transforming our ability to understand the breadth and diversity of soil microbial communities and their functional capabilities. Soil microbial communities are dependent for the most part on food sources, water and oxygen. In Australian soils, which are low in soil organic matter, spatial heterogeneity results in more concentrated communities associated with microsites such as plant roots (rhizosphere) and decomposing residues (detritusphere) which support approximately 60% of all microbial life in surface soils. In the rhizosphere, carbon (C) and other nutrients and water are supplied by rhizodeposition with above- and below-ground crop residues being major sources of C inputs in agricultural soils. Microbial communities in the rhizosphere generally originate from the general soil but spatial isolation and minimal food sources in the soil limit their proliferation and activities. In the rhizosphere, interactions among microorganisms and plants are generally mutualistic. Apart from food and nutrients supplied by plants, microorganisms benefit from interactions with each other and provide benefits to the plant by transforming nutrients to available forms or by competing with or suppressing plant pathogens.