Nematode Community-Based Soil Food Web Analysis of Ferralsol, Lithosol and Nitosol Soil Groups in Ghana, Kenya and Malawi Reveals Distinct Soil Health Degradations
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Measuring Soil Ph
Measuring soil pH Viti-note Summary: Soil pH refers to the acidity or alkalinity Equipment of the soil. It is a measure of the • Equipment Colorimetric test kit available from concentration of free hydrogen ions nurseries (includes mixing stick, plate, • Timing (H+) that are in the soil. Soil pH can dye, barium sulphate, pH colour chart, be measured in water (pH ) or a weak • Method w instructions), teaspoon, recording sheet calcium chloride solution (pH ). The pH CaCl and pen. • Timing range is from 0-14, with value of 7 being neutral. Soil pH values (as measured in a OR water and soil solution) indicate: Hand held pH meter, clear plastic jar with • Strong acidity if less than 5.0. screw-on lid, distilled water, recording sheet and pen. • Moderate acidity at 5.0 to 6.0. • Neutral between 6.5 and 7.5. Timing • Moderate alkalinity at 7.5 to 8.5. This measurement is best undertaken • Strong alkalinity for values of 8.5 when soil sampling is conducted and and above. would normally be done at the same time The limited data available suggests that as assessments for electrical conductivity. soil pHCaCl should be in the range 5.5-7.5 Soil pH should be measured in the fibrous for best vine performance. root zone (ie. 0-20cm depth) as well as Soil pH outside the neutral range can the deeper root zone (>20cm depth). influence the availability of specific Make sure the soil samples are taken nutrients to plants, as well as the inside the irrigation wetting pattern. -
Backyard Food
Suggested Grades: 2nd - 5th BACKYARD FOOD WEB Wildlife Champions at Home Science Experiment 2-LS4-1: Make observations of plants and animals to compare the diversity of life in different habitats. What is a food web? All living things on earth are either producers, consumers or decomposers. Producers are organisms that create their own food through the process of photosynthesis. Photosynthesis is when a living thing uses sunlight, water and nutrients from the soil to create its food. Most plants are producers. Consumers get their energy by eating other living things. Consumers can be either herbivores (eat only plants – like deer), carnivores (eat only meat – like wolves) or omnivores (eat both plants and meat - like humans!) Decomposers are organisms that get their energy by eating dead plants or animals. After a living thing dies, decomposers will break down the body and turn it into nutritious soil for plants to use. Mushrooms, worms and bacteria are all examples of decomposers. A food web is a picture that shows how energy (food) passes through an ecosystem. The easiest way to build a food web is by starting with the producers. Every ecosystem has plants that make their own food through photosynthesis. These plants are eaten by herbivorous consumers. These herbivores are then hunted by carnivorous consumers. Eventually, these carnivores die of illness or old age and become food for decomposers. As decomposers break down the carnivore’s body, they create delicious nutrients in the soil which plants will use to live and grow! When drawing a food web, it is important to show the flow of energy (food) using arrows. -
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. -
The Soil Survey
The Soil Survey The soil survey delineates the basal soil pattern of an area and characterises each kind of soil so that the response to changes can be assessed and used as a basis for prediction. Although in an economic climate it is necessarily made for some practical purpose, it is not subordinated to the parti cular need of the moment, but is conducted in a scientific way that provides basal information of general application and eliminates the necessity for a resurvey whenever a new problem arises. It supplies information that can be combined, analysed, or amplified for many practical purposes, but the purpose should not be allowed to modify the method of survey in any fundamental way. According to the degree of detail required, soil surveys in New Zealand are classed as general, . district, or detailed. General surveys produce sufficient detail for a final map on the scale of 4 miles to an inch (1 :253440); they show the main sets of soils and their general relation to land forms; they are an aid to investigations and planning on the regional or national scale. District surveys, for maps, on the scale of 2 miles to an inch (1: 126720), show soil types or, where the pattern is detailed, combinations of types; they are designed to show the soil pattern in sufficient detail to allow the study of local soil problems and to provide a basis for assembling and distributing information in many fields such as agriculture, forestry, and engineering. Detailed surveys, mostiy for maps on the scale of 40 chains to an inch (1 :31680), delineate soil types and land-use phases, and show the soil pattern in relation to farm boundaries and subdivisional fences. -
Soil Ph Ranges Neutral Acidity Alkalinity
Sound Farm Idea #04 Lime For Pastures and Crops When it comes to managing soil health in the Northwest, it’s easy to focus on the big three nutrients (nitrogen, phosphorus, and potassium) in the soil, and overlook a fourth key aspect - soil pH. Soil pH refers to how acidic (sour) or alkaline (sweet) soil is on a scale between 0 and 14, with 7.0 being neutral. Most plants and crops prefer soil pH levels in the 6.0 – 7.0 range. Soil pH Ranges Neutral Acidity Alkalinity 10,000x 1,000x 100x 10x o 10x 100x 1,000x 10,000x 3 4 5 6 7 8 9 10 11 Here in Western Washington, our soils are typically mildly to strongly acidic (5.0 – 6.5). Soil pH is important for a number of reasons. First of all, it controls the rate of chemical reactions and the activity of soil microorganisms. As you move towards the ends of the scale, different nutrients will either become more or less available for plants. For example, phosphorus is readily available when soil pH is 6.5; decreasing the pH to 5.5 reduces its availability by half. Also, as soil pH decreases, the activity of beneficial nitrogen-fixing bacteria slows down and many detrimental disease-causing fungi become more active. It’s important to factor pH levels into your fertilizer applications to ensure that nutrients will be available to plants. Often, after a lime application, a lawn or pasture may quickly ‘green-up’. This is due to nutrients already in the soil becoming available during the pH adjustment. -
Review Article on Paleopedology And
PRELIMINARY STUDY OF SOIL SAMPLES FROM IRON AGE NECROPOLES AT CAMPO Christophe MBIDA MINDZIE, Antoine MVONDO ZE, Conny MEISTER & Manfred K.H. EGGERT ABSTRACT This work was undertaken on soil samples of six prospective graves and four ”rubbish pits” from Campo and Akonetye sites. The studied soil samples could be divided into two distinguishing groups. The first was characterized by relatively high values of pH, very high content of calcium, phosphorus and potassium compared to values commonly found in surrounding forest soils. This group was found to correspond to the dump pits, while the second group of samples with low pH, lower content of calcium, phosphorus came from the hypothesised burial places. Key words: soil features, soil analyses, calcium and phosphorus content, dump pits, necropolis, burial. INTRODUCTION The most common features encountered in iron age sites of Southern Cameroon are the so called “rubbish pits”, which seem to be most obviously, a final use of those pits, when the original purposes for which they were dug were over. One of the studied sites located in the vicinity of the Catholic Church at Campo, a small town of south Cameroon revealed specific structures different in their nature from the dump pits. There were dump pits alongside with alignments of overturned clay potteries. The first surveys (ZANA, 2000; OSLISLY et al, 2006) confirmed the latter features were different and their specificity shown by the disposition and types of the artefacts recovered. It was hypothesized they were graves. The preliminary chemical study of soil samples from few pits and those new features was performed to determine the nature of the deposits and how they were deposited, as well as to analyse the context of conservation of artefact in the equatorial soils. -
Seventh Grade
Name: _____________________ Maui Ocean Center Learning Worksheet Seventh Grade Our mission is to foster understanding, wonder and respect for Hawai‘i’s Marine Life. Based on benchmarks SC.6.3.1, SC. 7.3.1, SC. 7.3.2, SC. 7.5.4 Maui Ocean Center SEVENTH GRADE 1 Interdependent Relationships Relationships A food web (or chain) shows how each living thing gets its food. Some animals eat plants and some animals eat other animals. For example, a simple food chain links plants, cows (that eat plants), and humans (that eat cows). Each link in this chain is food for the next link. A food chain always starts with plant life and ends with an animal. Plants are called producers (they are also autotrophs) because they are able to use light energy from the sun to produce food (sugar) from carbon dioxide and water. Animals cannot make their own food so they must eat plants and/or other animals. They are called consumers (they are also heterotrophs). There are three groups of consumers. Animals that eat only plants are called herbivores. Animals that eat other animals are called carnivores. Animals and people who eat both animals and plants are called omnivores. Decomposers (bacteria and fungi) feed on decaying matter. These decomposers speed up the decaying process that releases minerals back into the food chain for absorption by plants as nutrients. Do you know why there are more herbivores than carnivores? In a food chain, energy is passed from one link to another. When a herbivore eats, only a fraction of the energy (that it gets from the plant food) becomes new body mass; the rest of the energy is lost as waste or used up (by the herbivore as it moves). -
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. -
Soil Acidification
viti-notes [grapevine nutrition] Soil acidifi cation Viti-note Summary: Characteristics of acidic soils • Soil pH Calcium and magnesium are displaced • Soil acidifi cation in by aluminium (Al3+) and hydrogen (H+) vineyards and are leached out of the soil. Acidic soils below pH 6 often have reduced • Characteristics of acidic populations of micro-organisms. As soils microbial activity decreases, nitrogen • Acidifying fertilisers availability to plants also decreases. • Effect of soil pH on Sulfur availability to plants also depends rate of breakdown of on microbial activity so in acidic soils, ammonium to nitrate where microbial activity is reduced, Figure 1. Effect of soil pH on availability of minerals sulfur can become unavailable. (Sulfur • Management of defi ciency is not usually a problem for acidifi cation Soil pH vineyards as adequate sulfur can usually • Correction of soil pH All plants and soil micro-organisms have be accessed from sulfur applied as foliar with lime preferences for soil within certain pH fungicides). ranges, usually neutral to moderately • Strategies for mature • Phosphorus availability is reduced at acid or alkaline. Soil pH most suitable vines low pH because it forms insoluble for grapevines is between 5.5 and 8.5. phosphate compounds with In this range, roots can acquire nutrients aluminium, iron and manganese. from the soil and grow to their potential. As soils become more acid or alkaline, • Molybdenum is seldom defi cient in grapevines become less productive. It is neutral to alkaline soils but can form important to understand the impacts of insoluble compounds in acid soils. soil pH in managing grapevine nutrition, • In strongly acidic soil (pH <5), because the mobility and availability of aluminium may become freely nutrients is infl uenced by pH (Figure 1). -
A Systemic Approach for Modeling Soil Functions
SOIL, 4, 83–92, 2018 https://doi.org/10.5194/soil-4-83-2018 © Author(s) 2018. This work is distributed under SOIL the Creative Commons Attribution 4.0 License. A systemic approach for modeling soil functions Hans-Jörg Vogel1,5, Stephan Bartke1, Katrin Daedlow2, Katharina Helming2, Ingrid Kögel-Knabner3, Birgit Lang4, Eva Rabot1, David Russell4, Bastian Stößel1, Ulrich Weller1, Martin Wiesmeier3, and Ute Wollschläger1 1Helmholtz Centre for Environmental Research – UFZ, Permoserstr. 15, 04318 Leipzig, Germany 2Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, Germany 3TUM School of Life Sciences Weihenstephan, Technical University of Munich, Emil-Ramann-Straße 2, 85354 Freising, Germany 4Senckenberg Museum of Natural History, Sonnenplan 7, 02826 Görlitz, Germany 5Martin-Luther-University Halle-Wittenberg, Institute of Soil Science and Plant Nutrition, Von-Seckendorff-Platz 3, 06120 Halle (Saale), Germany Correspondence: Hans-Jörg Vogel ([email protected]) Received: 13 September 2017 – Discussion started: 4 October 2017 Revised: 2 February 2018 – Accepted: 14 February 2018 – Published: 15 March 2018 Abstract. The central importance of soil for the functioning of terrestrial systems is increasingly recognized. Critically relevant for water quality, climate control, nutrient cycling and biodiversity, soil provides more func- tions than just the basis for agricultural production. Nowadays, soil is increasingly under pressure as a limited resource for the production of food, energy and raw materials. This has led to an increasing demand for concepts assessing soil functions so that they can be adequately considered in decision-making aimed at sustainable soil management. The various soil science disciplines have progressively developed highly sophisticated methods to explore the multitude of physical, chemical and biological processes in soil. -
Age and Pedogenic Reconstruction of a Paleo–Relict Chernozem Soil from Central Transylvanian Basin
AGE AND PEDOGENIC RECONSTRUCTION OF A PALEO–RELICT CHERNOZEM SOIL FROM CENTRAL TRANSYLVANIAN BASIN F. PENDEA1, Z. SZÁNTÓ2, A. S. BADARAU1 and S. DEZSI1 1Babes–Bolyai University, Faculty of Geography, Cluj–Napoca Clinicilor street no 5–7, 3400 Cluj–Napoca, Romania 2Institute of Nuclear Research, Laboratory of Environmental Studies, H 4001 Debrecen P.O Box 51, Hungary Abstract: The “chernozem” area of Transylvanian Lowland has been of much debate in the last two centuries. The paper presents pedological and geochronological evidence that the chernozem soils of the Central Transylvania have relict Late Glacial–Early Holocene features and at least partially must be clasiffied as paleo–relict in the sense of Reuter (2000). Key words: radiocarbon dating, pedogenic carbonates, paleo–relict features, Central Transylvania During the last century a much debated issue for Romanian pedological and botanical scientific communities was the age and origin of the Central Transylvanian Mollisol cover in conjunction with the associated forest–steppe vegetation. In this study we have found at least partial evidence that the chernozem soil cover in Central Transylvanian was a stable feature long before the ascent of human activities and that, in the Late Holocene, they have suffered a degradation process to the present state of Haplic and Luvic chernozem. The process is somewhat similar with that inferred for Central and Southern Germany, where chernozems formed in the dry steppe or forest–steppe conditions were degraded to brown earths, the resulting polygenetic cover being named Braunerde (Parabraunerde)–Tschernozem (Catt 1989). Because the nature and properties of different soil horizons can hold information with respect to the time pedogenic factor an investigation was undertaken to determine if the typical chernozem features were indeed Late Holocene (Post–Neolithic) as it has been accepted before. -
Plants Are Producers! Draw the Different Producers Below
Name: ______________________________ The Unique Producer Every food chain begins with a producer. Plants are producers. They make their own food, which creates energy for them to grow, reproduce and survive. Being able to make their own food makes them unique; they are the only living things on Earth that can make their own source of food energy. Of course, they require sun, water and air to thrive. Given these three essential ingredients, you will have a healthy plant to begin the food chain. All plants are producers! Draw the different producers below. Apple Tree Rose Bushes Watermelon Grasses Plant Blueberry Flower Fern Daisy Bush List the three essential needs that every producer must have in order to live. © 2009 by Heather Motley Name: ______________________________ Producers can make their own food and energy, but consumers are different. Living things that have to hunt, gather and eat their food are called consumers. Consumers have to eat to gain energy or they will die. There are four types of consumers: omnivores, carnivores, herbivores and decomposers. Herbivores are living things that only eat plants to get the food and energy they need. Animals like whales, elephants, cows, pigs, rabbits, and horses are herbivores. Carnivores are living things that only eat meat. Animals like owls, tigers, sharks and cougars are carnivores. You would not catch a plant in these animals’ mouths. Then, we have the omnivores. Omnivores will eat both plants and animals to get energy. Whichever food source is abundant or available is what they will eat. Animals like the brown bear, dogs, turtles, raccoons and even some people are omnivores.