Beginning in the early 1970s he became a prolific illustrator for many anarchist, radical, alternative and mainstream publications, organisations, groups and individuals including Freedom Press, Undercurrents, Respect for Animals, BIT Newsletter, Arts Lab Newsletter, Idiot International, 1977 Firemans Strike, Libertarian Education, The Idler, Radical Community Medicine, Anarchy Magazine, Black Flag, Anarchy Comix, Common Ground, Industrial Worker, Aberlour Distillery, Country Life, Graphical Paper and Media Union, The Times Saturday Review, Tolpuddle Martyrs Festival, New Scientist, Oxford University Press, Penguin Books, Times Educational Supplement, London Anarchist Bookfair, Public and Commercial Services Union, The Sunday Times Magazine, Catholic Worker, Soil Association, The Bodleian Library, New Statesman, Cienfeugos Anarchist Review, Headline Books, The Financial Times, Resurgence, Scotland on Sunday, Town and Country Planning Association, Movement Against A Monarchy, Nursing Times, John Hegarty, The Listener, Zero, McCallan Whisky, Solidarity, New Society, News from Neasden, House & Garden, The Tablet, Radical Science Journal, Royal Mail, The Co-ops Fairs, Picador Books, Pluto Press, Working Press, Anarchismo, Insurrection, Our Generation, Ogilvy & Mather, Vogue, Radio Times, National Union of Teachers, Faber & Faber, Pimlico, Trades Union Congress, Transport and General Workers Union, Serpents Tale, Compendium Books, Poison Girls, Yale University Press, The Daily Telegraph, The Independent, Elephant Editions, Intelligent Life, Landworker, Zounds, Honey, New Musical Express, Knockabout Comics, Trickett and Webb, The Times, See Sharp Press, Countryside Commission, Industrial Common Ownership Movement, BBC Worldwide, Stop the War Coalition, The Folio Society, Unison, Anarchist Studies, Country Standard, Fitzrovia News, Anarchist Black Cross and many others.

The notable acts repealed were the Town and Country Planning Act, the Water and Soil Conservation Act, the Soil Conservation and Rivers Control Act, and the Minerals Act.

Soil redeposition is evaluated by washing clean swatches with the dirty ones.

Soil with a pH value higher than 7. 3 is normally referred to as alkaline.

Clay identification is determined by a process of refiring the ceramic, and assigning a color to it using Munsell Soil Color notation.

Soil erosion ( especially from agricultural activity ) is considered to be the leading global cause of diffuse water pollution, due to the effects of the excess sediments flowing into the world's waterways.

The most commonly used model for predicting soil loss from water erosion is the Universal Soil Loss Equation ( USLE ), which estimates the average annual soil loss as:

Soil is contaminated through particulate accumulation from lead in pipes, lead paint and residual emissions from leaded gasoline that was used before the Environment Protection Agency issue the regulation around 1980.

Environment-current issues: Soil salinity is rising.

According to the Soil Association, the total copper that can be applied to organic land is 6 kg / ha / year.

Soil erosion due to improper land and plough utilization is possible.

Its label states it is approved by the Soil Association and the Vegetarian Society.

Soil is a natural body consisting of layers ( soil horizons ) that are primarily composed of minerals which differ from their parent materials in their texture, structure, consistency, colour, chemical, biological and other characteristics.

Soil is the end product of the influence of the climate ( temperature, precipitation ), relief ( slope ), organisms ( flora and fauna ), parent materials ( original minerals ), temperature, and time.

Soil is composed of particles of broken rock ( parent materials ) which have been altered by chemical and mechanical processes that include weathering ( disintegration ) with associated erosion ( movement ).

Soil is altered from its parent material by the interactions between the lithosphere, hydrosphere, atmosphere, and biosphere.

Soil is commonly referred to as " earth " or " dirt "; technically, the term " dirt " should be restricted to displaced soil.

Soil pH, a measure of the hydrogen ion ( acid-forming ) soil reactivity, is a function of the soil materials, precipitation level, and plant root behavior.

Soil formation, or pedogenesis, is the combined effect of physical, chemical, biological, and anthropogenic processes on soil parent material.

Soil is said to be formed when organic matter has accumulated, and colloids washed downward, leaving deposits of clay, humus, iron oxide, carbonate, and gypsum.

Soil is said to be formed when detectable layers of clays, organic colloids, carbonates, or soluble salts have been moved downward.

Soil is always changing.

Soil texture is determined by the relative proportion of the three kinds of soil particles, called soil " separates ": sand, silt, and clay.

Soil density, particularly bulk density, is a measure of soil compaction.

** Soil erosion – process by which soil is removed from the Earth's surface by natural processes such as wind or water flow, and then transported and deposited in other locations.

Soil is not only a support for vegetation, but it is also the zone beneath our feet ( the pedosphere ) of numerous interactions between climate ( water, air, temperature ), soil life ( micro-organisms, plants, animals ) and its residues, the mineral material of the original and added rock, and its position in the landscape.

Soil conditions for farming are generally good, especially downwind of volcanoes.

The surface is generally rolling ; Soil mostly second rate except on some of the Birch and Maple ridges it is first rate.

The Surface of this Township is generally level the dry land is but very little elevated above the Swamps the Soil is poor 3rd rate bearing but little vegetation but is generally covered with a thick heavy moss.

The Surface of the Township is generally broken the Soil is very poor 3rd rate producing very little vegetation but the Surface of the land is generally covered with a thick heavy moss.

The Surface of This Township is generally Broken Soil (?

The Surface of this Township is generally Broken Soil 3rd rate producing but little vegetation the Surface of the land being generally covered with a thick heavy moss (?).

Soil generally consists of visually and texturally distinct layers, which can be summarized as follows from top to bottom:

Soil moisture is generally described as water content,, or saturation,.

The municipality's land soil is generally classified into five ( 5 ) types, namely: Cataingan Soil, 91. 93 %; Farm-on Soil, 4. 25 %; Panganiban Soil, 2. 55 %; Hydrosol, 0. 70 %; and Batuan Soil, 0. 57 %.

The fiercely abolitionist Free Soil Party was a huge spoiler in this election, earning 9 seats in districts that generally supported Whig politicians.

Soil colloidal particles ( clay and humus ) behave as a repository of nutrients and moisture, and buffer the variations of soil solution ions.

Soil type s by clay, silt and sand composition as used by the United States Department of Agriculture | USDAIron-rich soil near Paint Pots in Kootenay National Park, Canada The mineral components of soil, sand, silt, and clay determine a soil's texture.

Soil composition is primarily sand and clay rather than limestone, so very few sinkholes develop ; however deep, large diameter sinkholes do occur.

Soil composition ranges from sandy to clay base.

Soil containing the common clay mineral montmorillonite ( Mte ) and kaolinite ( Kte ) binds more effectively with the prions than soil containing quartz.

* a Unified Soil Classification System symbol for organic silt and / or clay

Soil structure decline under irrigation is usually related to the breakdown of aggregates and dispersion of clay material as a result of rapid wetting.

* OH, in the Unified Soil Classification System, the designation for organic-rich clay or silt of high plasticity

Soil is made up in part of finely ground rock particles, grouped according to size as sand and silt in addition to clay and humus, organic material such as decomposed plant matter.

* Soil, a mixture of clay, sand and organic matter present on the surface of the Earth and serving as substrate for plant growth and micro-organisms development

Soil and especially clay is good thermal mass ; it is very good at keeping temperatures at a constant level.

Soil: derno-podzolic, moderate coal clay, clay sand, and sand.

Soil characteristics strongly influence the architecture of taproots ; for example, deep rich soils favor the development of vertical taproots in many oak species such as Quercus kelloggii, while clay soils promote the growth of multiple taproots.

* Soil and microclimate: The Tokaj terrain consists of clay or loess soil on volcanic subsoil.

* Soil and microclimate: The Tokaj terroir consists of clay or loess soil on volcanic subsoil.

Soil composition developed from recent alluvial deposits which are silty-loam to clay loam and landforms consist of limestone and sedimentary rocks.

According to the Unified Soil Classification System, a # 4 sieve ( 4 openings per inch ) having 4. 75mm opening size separates sand from gravel and a # 200 sieve with an 0. 075 mm opening separates sand from silt and clay.

Soil in good tilth is loamy, nutrient-rich soil that can also be said to be friable because optimal soil has a mixture of sand, clay and organic matter that prevents severe compaction.

Soil Status varies from alluvial to clay loam.