Changes for page Layer terminology
Last modified by Roelof Zwaan on 2021/12/07 11:08
<
>
edited by TerraIndex TerraIndex
on 2021/09/09 09:31
on 2021/09/09 09:31
edited by TerraIndex TerraIndex
on 2021/05/28 14:01
on 2021/05/28 14:01
Change comment:
There is no comment for this version
Summary
-
Page properties (1 modified, 0 added, 0 removed)
Details
- Page properties
-
- Content
-
... ... @@ -12,7 +12,7 @@ 12 12 13 13 = Primary = 14 14 15 -The primary fraction is the fraction which is more than 50% of the same material. If this primary faction is anthropogenic the layer gets the name of the anthropogenic substance. The quality of the sample of the primary fraction needs to be QM5 and with organic soil QM4. 15 +The primary fraction is the fraction which is more than 50% of the same material. If this primary faction is anthropogenic the layer gets the name of the anthropogenic substance. For the name of the primary fraction one can take a look at the category [[soil specification>>url:https://terrapedia.terraindex.com/index.php?title=Soil_specification&action=edit&redlink=1]]. The quality of the sample of the primary fraction needs to be QM5 and with organic soil QM4. 16 16 17 17 == M50 == 18 18 ... ... @@ -22,9 +22,9 @@ 22 22 23 23 The secondary fraction lies between 5 and 50 % of the same material. At 5% > 20% of the same material one can speak of a weak presence of the material. At 20%>50% of the same material one can speak of a strong presence of the material. There is a possibility to add a second secondary component, but that is also the maximum of secondary components that can be present. 24 24 25 -== [[Gradation>> doc:Characteristics.Soil boundaries.WebHome]] ==25 +== [[Gradation>>url:https://terrapedia.terraindex.com/index.php?title=Gradation&action=edit&redlink=1]] == 26 26 27 -When the material has abrupt transition into the primary or tertiary fraction the gradation is called weak. With a strong gradation the border between materials is less clear and the clast size changes gradually. 27 +When the material has abrupt transition into the primary or tertiary fraction the [[gradation>>url:https://terrapedia.terraindex.com/index.php?title=Gradation&action=edit&redlink=1]] is called weak. With a strong [[gradation>>url:https://terrapedia.terraindex.com/index.php?title=Gradation&action=edit&redlink=1]] the border between materials is less clear and the clast size changes gradually. 28 28 29 29 == Grain shape == 30 30 ... ... @@ -34,18 +34,14 @@ 34 34 35 35 = Tertiary = 36 36 37 -This category is used for the indication of a strange or [[special component>>d oc:Soil.Specials.WebHome]] present in the layer. In this category many residual materials are present, for example calcium and wood. The fraction present can range from 5 to 50%. At 5% > 25% of the same material one can speak of a weak presence of the material. At 25%>50% of the same material one can speak of a strong presence of the material. Organic components are not accounted in the tertiary category. For other materials present the samples need to be of at least class QM4. Further below some components are explained.37 +This category is used for the indication of a strange or [[special component>>url:https://terrapedia.terraindex.com/index.php/Special_component]] present in the layer. In this category many residual materials are present, for example calcium and wood. The fraction present can range from 5 to 50%. At 5% > 25% of the same material one can speak of a weak presence of the material. At 25%>50% of the same material one can speak of a strong presence of the material. Organic components are not accounted in the tertiary category. For other materials present the samples need to be of at least class QM4. Further below some components are explained. 38 38 39 39 == AC 16 base/ AC 16-22 base == 40 40 41 41 Reinforcement layers for asphalt. 42 42 43 -== Catclay ==43 +== Acid clay == 44 44 45 -Katteklei, also cat clay is the common name for mostly clay (but sometimes venomous) deposits in which, in addition to sulphuric acid, large amounts of iron, aluminum and heavy metals also occur. As a result, the soil is poorly suited for agriculture. These soils are especially recognizable by the yellow jarosite spots, in addition, iron stains are common. The acidity of the soil is high (pH 9). 46 - 47 -Katteklei forms in soils that naturally contain many iron sulphides, especially pyrite. These usually arise in coastal areas, especially in quiet environments such as lagoons or quiet parts of estuaries and often on the edge of peatlands that emit a lot of iron-containing water. When these soils are exposed to air, for example during drainage, sulfuric acid forms. This used to happen frequently in the Western Netherlands when the drying plants were pumped out, leaving some farmers stuck with very bad plots of land. [3] 48 - 49 49 == Ammunitions == 50 50 51 51 Remnant of fired gun and can cause lead poisoning of the soil. ... ... @@ -56,7 +56,7 @@ 56 56 57 57 == Asbestos == 58 58 59 -Asbestos is a term used to refer to six naturally occurring silicate minerals. All are composed of long and thin fibrous crystals, each fiber being composed of many microscopic 'fibrils' that can be released into the atmosphere by abrasion and other processes. Asbestos is used to strengthen ceramic creations and in walls or roofs of houses. When one suspect the presence of asbestos in a decayed wall or roof one needs to select the 'Asbestos suspect material'-field. More on asbestos-sampling and other specification can be found on the following [[page>> doc:Characteristics.Samples.Asbestos.WebHome]].55 +Asbestos is a term used to refer to six naturally occurring silicate minerals. All are composed of long and thin fibrous crystals, each fiber being composed of many microscopic 'fibrils' that can be released into the atmosphere by abrasion and other processes. Asbestos is used to strengthen ceramic creations and in walls or roofs of houses. When one suspect the presence of asbestos in a decayed wall or roof one needs to select the 'Asbestos suspect material'-field. More on asbestos-sampling and other specification can be found on the following [[page>>url:https://terrapedia.terraindex.com/index.php/Asbestos]]. 60 60 61 61 == Asphalt or bitumen == 62 62 ... ... @@ -110,7 +110,7 @@ 110 110 111 111 A porous black solid, consisting of an amorphous form of carbon, obtained as a residue when wood, bone, or other organic matter is heated in the absence of air. 112 112 113 -== [[Clay>> doc:Rocktypes.Sedimenten.Clay.WebHome]] ==109 +== [[Clay>>url:https://terrapedia.terraindex.com/index.php/Clay]] == 114 114 115 115 A stiff, sticky fine-grained earth that can be moulded when wet, and is dried and baked to make bricks, pottery, and ceramics. 116 116 ... ... @@ -173,15 +173,15 @@ 173 173 174 174 Any rock-forming mineral that has a specific gravity greater than 2.8 and that is generally dark in color. 175 175 176 -== [[Detritus>> doc:Organic depositions.Detritus.WebHome]] ==172 +== [[Detritus>>url:https://terrapedia.terraindex.com/index.php/Detritus]] == 177 177 178 178 Detritus is particles of rock derived from pre-existing rock through processes of weathering and erosion. Detritus can also be dead organic material. 179 179 180 -== [[Dolerite>> doc:Rocktypes.Igneousrocks.Extrusivegneous rocks.Dolerite.WebHome]] ==176 +== [[Dolerite>>url:https://terrapedia.terraindex.com/index.php/Dolerite]] == 181 181 182 182 Dolerite is an igneous rock with a silica amount of 48 till 52%. The minerals present in dolerite are: olivine, plagioclase, biotite, amphiboles and pyroxenes. 183 183 184 -== [[Dy>> doc:Organic depositions.Dy.WebHome]] ==180 +== [[Dy>>url:https://terrapedia.terraindex.com/index.php/Dy]] == 185 185 186 186 Type of soil formed in nutrient low waters which mainly consist of very fine sunken organic components. 187 187 ... ... @@ -207,7 +207,7 @@ 207 207 208 208 Gravel is a loose aggregation of rock fragments. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. ISO 14688 grades gravels as fine, medium, and coarse with ranges 2 mm to 6.3 mm to 20 mm to 63 mm. 209 209 210 -== [[Gypsum>> doc:Rocktypes.Salts.Gypsum.WebHome]] ==206 +== [[Gypsum>>url:https://terrapedia.terraindex.com/index.php/Gypsum]] == 211 211 212 212 Gypsum is the common name for CaSO,,4,,·2 H,,2,,O and is present at places where the sea water is partly or totally dried up. These dried up areas form loose layers in between the other rocks. This type of rock is soluble in water and is formed close to halite and anhydrite. Gypsum breaks into rhombus shaped pieces. 213 213 ... ... @@ -235,7 +235,7 @@ 235 235 236 236 Limestone is a sedimentary rock composed from remnants of small sea organisms. One can say a rock is limestone upon discovering a fossil. Limestone is made up from calcium carbonate and therefor a very soft rock type. It can be distinguished from other rock types with the help of HCl, because it sizzles when HCl touches its surface. 237 237 238 -== Loam == 234 +== [[Loam>>url:https://terrapedia.terraindex.com/index.php/Loam]] == 239 239 240 240 Loam is a soil type which mostly consist of sand and silt particles. A smaller amount of clay particles is present too. By weight, its mineral composition is about 40-40-20% concentration of sand-silt-clay respectively. If this proportions vary it is classified as the main type plus the name loam. For example: sandy loam, clay loam, etc. 241 241 ... ... @@ -361,9 +361,9 @@ 361 361 362 362 Unwanted or unusable material, substances, or by-products. 363 363 364 -== [[Wood>> doc:Organic depositions.Wood.WebHome]] ==360 +== [[Wood>>url:https://terrapedia.terraindex.com/index.php/Wood]] == 365 365 366 -Wood is the hard fibrous material that forms the main substance of the trunk or branches of a tree or shrub, used for fuel or timber. 362 +Wood is the hard fibrous material that forms the main substance of the trunk or branches of a tree or shrub, used for fuel or timber. 367 367 368 368 == ZOAB == 369 369