• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Rocks, Soil AP Env Sci Class 14 Dr. Mike Sowa
Rocks, Soil AP Env Sci Class 14 Dr. Mike Sowa

... • A Horizon: Mineral matter mixed with some humus • E Horizon: Light colored mineral particles. Zone of eluviation and leaching • B Horizon: Accumulation of clay transported from above • C Horizon: Partially altered parent material • Solum: O, A, E, and B layers. The “true soil” where soil formation ...
Abstract - UvA/FNWI
Abstract - UvA/FNWI

... of the 14C concentration. The specific mean- and half-life rates for 14C make it possible to determine the time of death of an organism. Many materials found in soils can be used for radiocarbon dating, as long as they were once part of the biosphere. Charcoal is an often used material. Charcoal is ...
Soils As A Resource Weathering Mechanical Weathering Frost
Soils As A Resource Weathering Mechanical Weathering Frost

... CO2 +H2O >>>> H2CO3 >>> H+ + HCO3CACO3 + H+ >>>>> Ca2+ + HCO3- ...
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? ...
Soils and Global Warming: A Positive or Negative Feedback?
Soils and Global Warming: A Positive or Negative Feedback?

... A Simple Analysis of How Soils May Respond to Global Warming Based on Changes in k a one time 0.5C increase in temperature:results based on Sierran soils ...
Soil Study Guide
Soil Study Guide

... Moist slippery earth usually red in color. Clay is often found in Georgia. Plants do not generally grow well in clay. ...
Parent materials
Parent materials

... How do living organisms affect the development of soil?  Organisms that live in soil—like plants, insects, and microbes—actively affect soil formation.  The greatest affect on the development of soil is from plants that once grew in it. This is referred to as native vegetation.  It determines th ...
Indicadores Biológicos Associados ao Ciclo do Fósforo em Solos de
Indicadores Biológicos Associados ao Ciclo do Fósforo em Solos de

... conventional tillage and cover crops on some biological indicators associated to the P cycle. The work was carried out on three adjacent areas on a Red-Yellow Oxisol: area I, a two-year experiment comparing the two management systems; area II a six-year experiment and area III, native Cerrado vegeta ...
Healthy Soils are: Full of Life - National Resources Conservation
Healthy Soils are: Full of Life - National Resources Conservation

... You can fit 40 million of them on the end of one pin. In fact, there are more soil microorganisms (microbes for short) in a teaspoonful of soil than there are people on the earth. These microbes, which make up only one-half of one percent of the total soil mass, are the yeasts, algae, protozoa, bact ...
The Group of Plant Nutrition and the Laboratory of
The Group of Plant Nutrition and the Laboratory of

... Zürich invite applications for a PhD position in soil organic matter/phosphorus biogeochemistry Soil organic matter is one of the most important components regulating the transfer of nutrients in terrestrial ecosystems. An innate constituent of soil organic matter is that it contains carbon, nitroge ...
Soils Part One: What`s in soil
Soils Part One: What`s in soil

... between soil components and moisture content? (There should be-the higher the soil’s organic matter, the higher its moisture)  Have students divide into pairs again to investigate soil air content  Provide each pair with 1 cup of dry soil in a 2 cup measuring cup.  Have each group slowly pour 1 c ...
Group assignments
Group assignments

... 2. (a) A substantial area of land in Zimbabwe is low land (dambo). Discuss the advantages and disadvantages associated with bottom land farming in these regions [15marks] (b) How could problems associated with bottom land farming be ameliorated? [10 marks] Individual Assignment Assignment I 1) Defin ...
Organic Matter
Organic Matter

... a crop grown for its organic matter green manure crops are generally plowed under while they are still green Examples = sweet clover, rye ...
Introduction Definition Factors Affecting Soil Formation How can we
Introduction Definition Factors Affecting Soil Formation How can we

... Soil is the base of the terrestrial life supporting system  It is a fragile resource which can be easily damaged by human activity  It must be conserved and treated with care ...
Soil Formation Worksheet
Soil Formation Worksheet

... produces layers known as soil horizons. The topsoil or A horizon is usually rich in darkcolored organic remains called humus (labeled O horizon below). The subsoil or B horizon contains minerals that have been transported deeper by groundwater. Most of the clay in soil has also been washed down to t ...
Chapter 10
Chapter 10

... Bokashi (Japanese for "fermented organic matter") is a method of intensive composting Commonly made with only molasses, water, EM, and wheat bran. Can be made by inoculating any organic matter with a variety of hosts of beneficial ...
Document
Document

... Students test the amount of water retained by different types of soil. Equal amounts of soil were added to four funnels with filters, then the same volume of water was poured through each soil sample. ...
Weathering and Erosion Study Guide
Weathering and Erosion Study Guide

... ____________________  When chemical reactions dissolve or alter the minerals in rocks or change them into different minerals ____________________  When rocks are broken apart by physical processes ____________________  Process in which surface materials are worn away and transported from one plac ...
Soil Formation Worksheet
Soil Formation Worksheet

... soil produces layers known as soil horizons. The topsoil or A horizon is usually rich in dark-colored organic remains called humus (labeled O horizon below). The subsoil or B horizon contains minerals that have been transported deeper by groundwater. Most of the clay in soil has also been washed dow ...
Study on carbon in Midwest Soil
Study on carbon in Midwest Soil

... more of it and store it (via photosynthesis) in their root systems — a net gain of carbon to the soil. However, as temperatures simultaneously increase, the microbes in soil become increasingly active, eating up more soil matter and releasing more carbon. Whatever small benefit higher atmospheric CO ...
Arid Zone Times - Arid Zone Trees
Arid Zone Times - Arid Zone Trees

... where the soils are less porous yet drain relatively quickly. Others, like the mesquites and Desert Willows are stream-side or riparian trees that can survive periods of water saturated soil conditions. Desert soils run the spectrum from sandy (in some cases dune sand) to heavy clay. The feature com ...
Agriculture and water
Agriculture and water

... then lead to the whole field becoming infertile and then having to wait hundreds of years for the field to produce new soil leading to it become fertile again. There is no problem in Germany, Scotland and Estonia because there are no droughts or very high temperatures. But it can be caused by fertil ...
Climate/Soil
Climate/Soil

... - soil types of different biomes differ - filtration rates, rate of water flow through the soil, of the different soils can be studied ...
Why is Soil Important? - Soil Science Society of America
Why is Soil Important? - Soil Science Society of America

... Getting the Dirt on Soils or ...
Getting the Dirt on Soils or Why is Soil Important
Getting the Dirt on Soils or Why is Soil Important

... Getting the Dirt on Soils or ...
< 1 ... 47 48 49 50 51 52 53 54 55 ... 58 >

Terra preta

Terra preta (Portuguese pronunciation: [ˈtɛʁɐ ˈpɾetɐ], locally [ˈtɛhɐ ˈpɾetɐ], literally ""black earth"" or ""black land"" in Portuguese) is a type of very dark, fertile anthropogenic soil found in the Amazon Basin. Terra preta owes its name to its very high charcoal content, and was made by adding a mixture of charcoal, bone, and manure to the otherwise relatively infertile Amazonian soil. It is very stable and remains in the soil for thousands of years. It is also known as ""Amazonian dark earth"" or ""Indian black earth"". In Portuguese its full name is terra preta do índio or terra preta de índio (""black earth of the Indian"", ""Indians' black earth""). Terra mulata (""mulatto earth"") is lighter or brownish in colour.Terra preta is characterized by the presence of low-temperature charcoal in high concentrations; of high quantities of pottery sherds; of organic matter such as plant residues, animal feces, fish and animal bones and other material; and of nutrients such as nitrogen (N), phosphorus (P), calcium (Ca), zinc (Zn), manganese (Mn). It also shows high levels of microorganic activities and other specific characteristics within its particular ecosystem. It is less prone to nutrient leaching, which is a major problem in most rain forests. Terra preta zones are generally surrounded by terra comum ([ˈtɛhɐ koˈmũ] or [ˈtɛhɐ kuˈmũ]), or ""common soil""; these are infertile soils, mainly acrisols, but also ferralsols and arenosols.Terra preta soils are of pre-Columbian nature and were created by humans between 450 BC and AD 950. The soil's depth can reach 2 meters (6.6 ft). Thousands of years after its creation it has been reported to regenerate itself at the rate of 1 centimeter (0.39 in) per year by the local farmers and caboclos in Brazil's Amazonian basin, who seek it for use and for sale as valuable potting soil.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report