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12.1 Soil - Union High School
12.1 Soil - Union High School

... 1. Mineral matter and organic matter together make up about 50 percent of soil. What two substances make up the other 50 percent? ...
SOILS Soils are Crucial for Life on Earth
SOILS Soils are Crucial for Life on Earth

... • Soils function as nature’s recycling system. Within the soil, waste products and dead bodies of plants, animals, and people are assimilated into elements made available for reuse by the next generation of life. • Soils provide habitats for many living organisms from small mammals and reptiles to t ...
soil intro - Ms Kim`s Biology Class
soil intro - Ms Kim`s Biology Class

... has major significance on the development of soil. • Microorganisms help develop soils by decomposing organic matter and forming weak acids that dissolve minerals faster than would pure water. • Fibrous root systems of grasses have a distinctly different effect on soils than do the coarser roots of ...
Soil Problems
Soil Problems

... My garden starts out well but constantly needs watering and fertilization ...
Cation Exchange Capacity: Its Context as an Integral Component of
Cation Exchange Capacity: Its Context as an Integral Component of

... system. The soil system is a complex ensemble of solid, aqueous and gaseous fluxes that are in dynamic equilibrium. The total amount of cations that can be retained electrostatically on soil surfaces is termed the cation exchange capacity (CEC). A measurement of CEC is one of the few techniques used ...
small intestine
small intestine

... of plant material, connects where the small and large ...
Tabela 5.2 Course specification Methods of soil Analysis OK
Tabela 5.2 Course specification Methods of soil Analysis OK

... The subject is the basis for understanding soil fertility, agricultural practices and fertilization in crop production 3. Course content Theoretical instruction Chemical methods of soil testing: The absorption method (colorimetry, spectrophotometry, atomic absorption spectrophotometry) Emission meth ...
Soil Vocabulary
Soil Vocabulary

... Humus: the broken down remains of plants and animals found in soil. Humus can hold large amounts of water and nutrients. Particle: a very small portion of matter; a small piece of something. Sand: the largest grain size, or sediment piece, that makes up soil. It feels gritty. Sediment: the pieces of ...
Classification - rosedale11universitybiology
Classification - rosedale11universitybiology

... their body with a shell for protection.  Reproduce sexually or asexually ...
“You Are What You Eat” The Digestion System
“You Are What You Eat” The Digestion System

... of alimentary canal Duodenum: 1st 25 cm, acid chyme mixes with digestive juices from the liver, gallbladder, and pancreas, and glass cells of wall Liver creates bile that has digestive enzymes and bile salts that aid digestion and absorption of fats As peristalsis moves the chime and digestive juice ...
INSECT INTERNAL ANATOMY
INSECT INTERNAL ANATOMY

... Foregut – mostly used for temporary storage, mixing and grinding. ...
soil matrix - School of Earth and Environment
soil matrix - School of Earth and Environment

... carbon and iron oxides with depth in a soil profile. ...
Teachers Guid 10 - Nature Conservation Lewisham
Teachers Guid 10 - Nature Conservation Lewisham

... by nature. Rocks change from one type to another during this process. ...
MAINTENANCE INTRODUCTION OBJECTIVES ALIMENTARY
MAINTENANCE INTRODUCTION OBJECTIVES ALIMENTARY

... which in turn branch into tinier tracheoles. This branching gets the tracheoles within a few cell diameters of each cell. This is important because each cell needs to have oxygen available on demand. When cells need more oxygen, the spiracles open and air rushes in. ...
LECTURE 10 - Rhodes University
LECTURE 10 - Rhodes University

... Definition: “The sum total of exchangeable cations that a soil can adsorb. This soil property is due to the negative electrical charge of the colloidal (both organic and inorganic) fraction of most soils. The negative charge is balanced by adsorbed cations so that the soil system as a whole is elect ...
Soils - Nmsu
Soils - Nmsu

... • What are some of the physical characteristics of soil? • What are some of the chemical characteristics of soil? • Are there different types of soil? – What are they? ...
Zoology - Cardinal Newman
Zoology - Cardinal Newman

... then to bilaterally symmetrical animals. ...
Computation of Evapotranspiration by Soil moisture Depletion Studies
Computation of Evapotranspiration by Soil moisture Depletion Studies

... irrigated field crops. ...
The Soil Profile
The Soil Profile

... • Parent Material: the original “Mom & Pop” soil transported from elsewhere, usually by wind or water, at different speeds • Climate: the amount, intensity, timing, and kind of precipitation that breaks down parts of ecosystem (i.e. rocks, trees) into soil • Topography: Slope and Aspect affect the a ...
Ch. 12 Part 1
Ch. 12 Part 1

... also helps purify water. IB considers soil to be nonrenewable resource because it takes hundreds to thousands of years to replace a few inches. ...
Abstract
Abstract

... In the course of their growth, cassava (Manihot spp.) roots exert pressure on the soil through which they pass and the influence of such pressure on soil structure is expected to be most pronounced at maturity, when the roots also have high content of polysaccharide which is known to play important ...
SOIL SAMMY
SOIL SAMMY

... the hose is the head of Soil Sammy, and the grass looks like hair when it grows. 2. Pack a handful of soil in the end of the hose on top of the seeds. Make sure the ball of soil is slightly larger than the opening of the baby food jar. 3. Tie a knot in the hose under the ball of soil. 4. Completely ...
FERTILITY CAPABILITY CLASSIFICATION Problem soils have been
FERTILITY CAPABILITY CLASSIFICATION Problem soils have been

... degradation hazards are more severe and adequate soil management measures are more difficult or costly to apply. Such soils, if improperly used or inadequately managed will degrade rapidly, sometimes irreversibly. As a result the land itself might go out of production (Dent, 1990). The process of gr ...
THE ROLES OF VARIOUS FUNCTIONAL GROUPS OF
THE ROLES OF VARIOUS FUNCTIONAL GROUPS OF

... season, i.e. on one level of scale beyond. If the objective would have been to explain the decomposition or mineralization process on the scale of the individual plant, we should have sampled the microsites below the plant scale with a frequency accounting for the speed at which processes occur in t ...
BIOL 202 LAB 11 Arthropoda
BIOL 202 LAB 11 Arthropoda

... unsurpassed success is due to the fact that they were the first animals to inhabit land. Between 440 and 410 million years ago, arthropods gradually moved into a previously unexploited habitat that simultaneously was being populated by vascular plants. They were also the first animal group to evolve ...
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Earthworm



An earthworm is a tube-shaped, segmented worm found in the phylum Annelida. They are commonly found living in soil, feeding on live and dead organic matter. Its digestive system runs through the length of its body. It conducts respiration through its skin. An earthworm has a double transport system composed of coelomic fluid that moves within the fluid-filled coelom and a simple, closed blood circulatory system. It has a central and a peripheral nervous system. The central nervous system consists of two ganglia above the mouth, one on either side, connected to a nerve cord running back along its length to motor neurons and sensory cells in each segment. Large numbers of chemoreceptors are concentrated near its mouth. Circumferential and longitudinal muscles on the periphery of each segment enable the worm to move. Similar sets of muscles line the gut, and their actions move the digesting food toward the worm's anus.Earthworms are hermaphrodites—each individual carries both male and female sex organs. They lack either an internal skeleton or exoskeleton, but maintain their structure with fluid-filled coelom chambers that function as a hydrostatic skeleton.""Earthworm"" is the common name for the largest members of Oligochaeta (which is either a class or a subclass depending on the author). In classical systems, they were placed in the order Opisthopora, on the basis of the male pores opening posterior to the female pores, though the internal male segments are anterior to the female. Theoretical cladistic studies have placed them, instead, in the suborder Lumbricina of the order Haplotaxida, but this may again soon change. Folk names for the earthworm include ""dew-worm"", ""rainworm"", ""night crawler"", and ""angleworm"" (due to its use as fishing bait).Larger terrestrial earthworms are also called megadriles (or big worms), as opposed to the microdriles (or small worms) in the semiaquatic families Tubificidae, Lumbriculidae, and Enchytraeidae, among others. The megadriles are characterized by having a distinct clitellum (which is more extensive than that of microdriles) and a vascular system with true capillaries.Earthworms are far less abundant in disturbed environments and are typically active only if water is present.
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