A Review of Methods to Improve Nitrogen Use Efficiency in Agriculture
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Basic Soil Science W
Basic Soil Science W. Lee Daniels See http://pubs.ext.vt.edu/430/430-350/430-350_pdf.pdf for more information on basic soils! [email protected]; 540-231-7175 http://www.cses.vt.edu/revegetation/ Well weathered A Horizon -- Topsoil (red, clayey) soil from the Piedmont of Virginia. This soil has formed from B Horizon - Subsoil long term weathering of granite into soil like materials. C Horizon (deeper) Native Forest Soil Leaf litter and roots (> 5 T/Ac/year are “bio- processed” to form humus, which is the dark black material seen in this topsoil layer. In the process, nutrients and energy are released to plant uptake and the higher food chain. These are the “natural soil cycles” that we attempt to manage today. Soil Profiles Soil profiles are two-dimensional slices or exposures of soils like we can view from a road cut or a soil pit. Soil profiles reveal soil horizons, which are fundamental genetic layers, weathered into underlying parent materials, in response to leaching and organic matter decomposition. Fig. 1.12 -- Soils develop horizons due to the combined process of (1) organic matter deposition and decomposition and (2) illuviation of clays, oxides and other mobile compounds downward with the wetting front. In moist environments (e.g. Virginia) free salts (Cl and SO4 ) are leached completely out of the profile, but they accumulate in desert soils. Master Horizons O A • O horizon E • A horizon • E horizon B • B horizon • C horizon C • R horizon R Master Horizons • O horizon o predominantly organic matter (litter and humus) • A horizon o organic carbon accumulation, some removal of clay • E horizon o zone of maximum removal (loss of OC, Fe, Mn, Al, clay…) • B horizon o forms below O, A, and E horizons o zone of maximum accumulation (clay, Fe, Al, CaC03, salts…) o most developed part of subsoil (structure, texture, color) o < 50% rock structure or thin bedding from water deposition Master Horizons • C horizon o little or no pedogenic alteration o unconsolidated parent material or soft bedrock o < 50% soil structure • R horizon o hard, continuous bedrock A vs. -
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 -
Nutrient Management and Imbalances David H
98 Nutrient Management and Imbalances David H. Gent, J Robert Sirrine, and Heather M. Darby Hop plants produce abundant biomass in the form of bines, leaves, and cones. High- yielding plants such as hop require adequate nutrition. Many of the various nutrients required by hop may be deficient or in excess of the crop’s needs. It can be difficult to pinpoint the cause of abnormal plant symptoms, especially if multiple production factors lead to the same symptom. General symptoms associated with nutrient imbalances are described in this section, as well as known nutrient interactions with diseases and arthropod pests. Fertilization recommendations are beyond the scope of this pest management guide and are not provided. Recommendations vary widely in published literature, differing among production regions, varieties, irrigation methods, soil types, and production goals. Readers should seek input from local experts for guidance appropriate to their region and situation. Boron Iron Boron deficiency can result in delayed Iron deficiency is first observed on emergence of shoots; stunting, distortion, young leaves as yellowing between veins, and crinkling of young leaves (Fig. 257); while veins remain green (Fig. 260, right- and yellowing and death of shoot tips (Fig. hand image, and Fig. 261). Iron deficiency 258). Leaves of affected plants may be small is most common in alkaline soils, although and brittle, and may develop a fluffy-tipped it can be induced in highly acidic soils appearance due to impaired development (approximately pH 5.7 or less) because of lobes (Fig. 259). Deficiencies are most of enhanced solubility and uptake of common in acid and/or sandy textured soils. -
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. -
Fixed Nitrogen in Agriculture and Its Role in Agrocenoses
Agronomy Research 19(2), 601–611, 2021 https://doi.org/10.15159/AR.21.086 Fixed nitrogen in agriculture and its role in agrocenoses S. Tanchyk1, D. Litvinov1, A. Butenko2,*, O. Litvinova3, O. Pavlov1, A. Babenko1, N. Shpyrka1, V.Onychko4, I. Masyk5 and T. Onychko4 1National University of Life and Environmental Sciences of Ukraine, Agrobiological faculty, Department of Agriculture and herbology, Heroyiv Oborony 12, UA03041 Кyiv, Ukraine 2Sumy National Agrarian University, Faculty of agricultural technologies and environmental, Plant growing Department, H. Kondratieva 160, UA40021 Sumy, Ukraine 3National University of Life and Environmental Sciences of Ukraine, Agrobiological faculty, Department of Agricultural chemistry and quality of plant products, Heroyiv Oborony 12, UA03041 Кyiv, Ukraine 4Sumy National Agrarian University, Faculty of agricultural technologies and environmental, Department of Selection and seeds named after M.D. Honcharov, H. Kondratieva 160, UA40021 Sumy, Ukraine 5Sumy National Agrarian University, Faculty of agricultural technologies and environmental, Department of Agriculture, soil and agrochemistry, H. Kondratieva 160, UA40021 Sumy, Ukraine *Correspondence: [email protected] Received: February 23rd, 2021; Accepted: May 12th, 2021; Published: May 19th, 2021 Abstract. On typical low-humus black soils in short crop rotations with legumes (25–33%) and without them, it was found that depending on the set of crops in crop rotation and application of fertilizer rates, nitrogen yield per crop is from 355 kg ha-1 to 682 kg ha-1. The recommended fertilization system provided nitrogen compensation for crop yields by only 31–76%. Hence, in the plant-fertilizer system nitrogen deficiency varies from 161 to 370 kg ha-1. The greatest nitrogen deficiency in the soil is observed in crop rotation without the use of fertilizers with the following crop rotation: peas-winter wheat-grain maize-spring barley. -
Improving Soil Nitrogen Availability and Rice Growth Performance on a Tropical Acid Soil Via Mixture of Rice Husk and Rice Straw Biochars
applied sciences Article Improving Soil Nitrogen Availability and Rice Growth Performance on a Tropical Acid Soil via Mixture of Rice Husk and Rice Straw Biochars Gunavathy Selvarajh , Huck Ywih Ch’ng * , Norhafizah Md Zain, Palsan Sannasi and Siti Nuurul Huda Mohammad Azmin Faculty of Agro-Based Industry, Campus Jeli, University Malaysia Kelantan, Kelantan 17600, Malaysia; [email protected] (G.S.); norhafi[email protected] (N.M.Z.); [email protected] (P.S.); [email protected] (S.N.H.M.A.) * Correspondence: [email protected]; Tel.: +60-17-853-7510 Featured Application: This research focuses on using an environmentally friendly technology (mixture of rice straw and rice husk biochars) to sustainably minimize ammonia volatilization, increase soil nutrient retention, and improve rice plant nutrient uptake and use efficiency. The mixture of rice straw and rice husk biochars has a larger surface area and numerous pores to chelate ammonium and nitrate ions. This process will fundamentally reduce the loss of ammo- nia via volatilization from urea fertilizer being applied, thus reducing the excessive use of urea fertilizer in agricultural sector. The biochar at 5 and 10 t ha−1 significantly minimized ammo- nia volatilization by 33.5–40.7%. It resulted in an increase of nutrient uptake, use efficiency, and dry matter production of rice plant. This work may not only contribute to the reduction of urea fertilizer import bill of Malaysia, but also pave the way for better means of adding value to the agricultural waste to avoid environmental pollution. It also contributes to increasing rice produc- tion by solving the problem of ammonia loss from urea fertilizer in tropical acid soil. -
Advanced Crop and Soil Science. a Blacksburg. Agricultural
DOCUMENT RESUME ED 098 289 CB 002 33$ AUTHOR Miller, Larry E. TITLE What Is Soil? Advanced Crop and Soil Science. A Course of Study. INSTITUTION Virginia Polytechnic Inst. and State Univ., Blacksburg. Agricultural Education Program.; Virginia State Dept. of Education, Richmond. Agricultural Education Service. PUB DATE 74 NOTE 42p.; For related courses of study, see CE 002 333-337 and CE 003 222 EDRS PRICE MF-$0.75 HC-$1.85 PLUS POSTAGE DESCRIPTORS *Agricultural Education; *Agronomy; Behavioral Objectives; Conservation (Environment); Course Content; Course Descriptions; *Curriculum Guides; Ecological Factors; Environmental Education; *Instructional Materials; Lesson Plans; Natural Resources; Post Sc-tondary Education; Secondary Education; *Soil Science IDENTIFIERS Virginia ABSTRACT The course of study represents the first of six modules in advanced crop and soil science and introduces the griculture student to the topic of soil management. Upon completing the two day lesson, the student vill be able to define "soil", list the soil forming agencies, define and use soil terminology, and discuss soil formation and what makes up the soil complex. Information and directions necessary to make soil profiles are included for the instructor's use. The course outline suggests teaching procedures, behavioral objectives, teaching aids and references, problems, a summary, and evaluation. Following the lesson plans, pages are coded for use as handouts and overhead transparencies. A materials source list for the complete soil module is included. (MW) Agdex 506 BEST COPY AVAILABLE LJ US DEPARTMENT OFmrAITM E nufAT ION t WE 1. F ARE MAT IONAI. ItiST ifuf I OF EDuCATiCiN :),t; tnArh, t 1.t PI-1, t+ h 4t t wt 44t F.,.."11 4. -
Characterization of Nutrient Disorders and Impacts on Chlorophyll and Anthocyanin Concentration of Brassica Rapa Var
agriculture Article Characterization of Nutrient Disorders and Impacts on Chlorophyll and Anthocyanin Concentration of Brassica rapa var. Chinensis 1 1 1, 2 Patrick Veazie , Paul Cockson , Josh Henry y, Penelope Perkins-Veazie and Brian Whipker 1,* 1 Department of Horticultural Sciences, North Carolina State University, Raleigh, NC 27695, USA; [email protected] (P.V.); [email protected] (P.C.); [email protected] (J.H.) 2 Plants for Human Health Institute, North Carolina State University, Kannapolis, NC 28081, USA; [email protected] * Correspondence: [email protected] Current address is: The Scotts Miracle-Gro Company, Marysville, OH 43040, USA. y Received: 3 September 2020; Accepted: 5 October 2020; Published: 8 October 2020 Abstract: Essential plant nutrients are needed at crop-specific concentrations to obtain optimal growth and yield. Foliar tissue analysis is the standard method for assessing nutrient levels in plants. Symptoms of nutrient deficiency or toxicity occur when the foliar tissue values become too low or high. Diagnostic nutrient deficiency criteria for Brassica rapa var. Chinensis (bok choy) is lacking in the current literature. In this study, green (‘Black Summer’) and purple (‘Red Pac’) bok choy plants were grown in silica sand culture, with control plants receiving a complete modified Hoagland’s all-nitrate solution, and nutrient-deficient plants induced by using a complete nutrient formula withholding a single nutrient. Tissue samples were collected at the first sign of visual disorder symptoms and analyzed for dry weight and nutrient concentrations of all plant essential elements. Six weeks into the experiment, the newest matured leaves were sampled for chlorophyll a, b, and total carotenoids concentrations for both cultivars, and total anthocyanin concentration in ‘Red Pac’. -
Progressive and Regressive Soil Evolution Phases in the Anthropocene
Progressive and regressive soil evolution phases in the Anthropocene Manon Bajard, Jérôme Poulenard, Pierre Sabatier, Anne-Lise Develle, Charline Giguet- Covex, Jeremy Jacob, Christian Crouzet, Fernand David, Cécile Pignol, Fabien Arnaud Highlights • Lake sediment archives are used to reconstruct past soil evolution. • Erosion is quantified and the sediment geochemistry is compared to current soils. • We observed phases of greater erosion rates than soil formation rates. • These negative soil balance phases are defined as regressive pedogenesis phases. • During the Middle Ages, the erosion of increasingly deep horizons rejuvenated pedogenesis. Abstract Soils have a substantial role in the environment because they provide several ecosystem services such as food supply or carbon storage. Agricultural practices can modify soil properties and soil evolution processes, hence threatening these services. These modifications are poorly studied, and the resilience/adaptation times of soils to disruptions are unknown. Here, we study the evolution of pedogenetic processes and soil evolution phases (progressive or regressive) in response to human-induced erosion from a 4000-year lake sediment sequence (Lake La Thuile, French Alps). Erosion in this small lake catchment in the montane area is quantified from the terrigenous sediments that were trapped in the lake and compared to the soil formation rate. To access this quantification, soil processes evolution are deciphered from soil and sediment geochemistry comparison. Over the last 4000 years, first impacts on soils are recorded at approximately 1600 yr cal. BP, with the erosion of surface horizons exceeding 10 t·km− 2·yr− 1. Increasingly deep horizons were eroded with erosion accentuation during the Higher Middle Ages (1400–850 yr cal. -
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. -
Improving Garden Soils with Organic Matter, EC 1561
EC 1561 • May 2003 $2.50 Improving Garden Soils with Organic Matter N. Bell, D.M. Sullivan, L.J. Brewer, and J. Hart This publication will help you understand the • Tomatoes and peppers get blossom-end rot, importance of soil organic matter levels to good even if fertilized with calcium. plant performance. It also contains suggestions • Water tends to pool on the soil surface and to for suitable soil amendments. Any soil, no drain slowly, or it runs off the surface. matter how compacted, can be improved by the addition of organic matter. The result will be a nnnn better environment for almost any kind of plant. What makes a productive soil? nnnn A productive soil provides physical support, water, air, and nutrients to plants and soil- What gardening problems are dwelling organisms (see “What is soil?” caused by poor soil quality? page 2). Like humans, roots and soil organisms Many problems with home vegetable gar- breathe and require sufficient air and water to dens, fruit trees, shrubs, and flower gardens are live. As a result, a good soil is not “solid”; caused not by pests, diseases, or a lack of rather, between 40 and 60 percent of the soil nutrients, but by poor soil physical conditions. volume is pores. The pores may be filled with Symptoms of poor soil quality include the water or air, making both available to plants following. (see illustration on page 3). • The soil is dried and cracked in summer. The largest pores control aeration and move- • Digging holes in the soil is difficult, whether ment of water through the soil and are largely it is wet or dry.