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Soil Science: An Overview of Non-Crystalline Minerals and Clay Minerals, Quizzes of Plant Taxonomy and Evolution

Definitions and properties of various non-crystalline minerals, including allophane and imogolite, and iron and aluminum oxide clays such as geothite, hematite, and gibbsite. Additionally, it covers organic soil colloids and cation exchange capacity. The document also discusses the importance of cation exchange capacity and the factors influencing cation competition.

Typology: Quizzes

2013/2014

Uploaded on 11/06/2014

jmm1418
jmm1418 🇺🇸

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Download Soil Science: An Overview of Non-Crystalline Minerals and Clay Minerals and more Quizzes Plant Taxonomy and Evolution in PDF only on Docsity! TERM 1 Non- Crystalline Minerals DEFINITION 1 Allophane and Imogolite -colloid silicatesPoorly crystallizedMoste predominant in volcanic ash (andisols & spodosolsProperties charge varies with pH, adsorb OM, H20, PO4 TERM 2 Allophane and Imogolite DEFINITION 2 Colloide silicats TERM 3 Iron & Aluminum Oxide clays DEFINITION 3 Greater occurrence in highly weathered, utisols & oxisolsGeothiteHematitegibbsitecharge varies with pHlow stickyness and platicityStrong soil structure TERM 4 Geothite DEFINITION 4 FeOOH (yellowish brown) TERM 5 Hematite DEFINITION 5 Fe TERM 6 Gibbsite DEFINITION 6 Gibbsite, A3, is one of the mineral forms of aluminium hydroxide. It is often designated as -Al(OH)3 (but sometimes as -Al(OH)3.). TERM 7 Organic Soil Colloids DEFINITION 7 Functional group supply chargeMajority of charge from SOM quantitiy of charge depends on pH.Carboxy- R -COOH R- COOH + OH- = R-COO- + H2OPhenolic- sorry could not get it symbol to postEnolic-R-OH TERM 8 Cation Exchange Capacity DEFINITION 8 SumIn soil science, cation-exchange capacity or CEC is the number of exchangeable cations per dry weight that a soil is capable of holding, at a given pH value, and available for exchange with the soil water solution. TERM 9 Cation DEFINITION 9 Basic - Ca2+, Mg2+, Na+, K+Acidic- Al3+, H+ TERM 10 Importance of CEC DEFINITION 10 Nutrient retentionBuffering capacityAdsorption of heavy metals TERM 21 Mineralogical definition of clay mineral DEFINITION 21 Clay mineral is a layer silicate composed of Si- tetrahedral sheets and gibbsite [Al(OH30] or brucite [Mg3(OH6)] octehedral TERM 22 Kaolinite DEFINITION 22 Kaolinite is a clay mineral, part of the group of industrial minerals, with the chemical composition Al2Si2O5(OH)4. It is a layered silicate mineral, with one tetrahedral sheet linked through oxygen atoms to one octahedral sheet of alumina octahedra. TERM 23 Properties of Kaolinite 1:1 DEFINITION 23 No interlayer spacesurface area 5-30 m2/g Hexogonal crystalsplasticity = lowshrink-swell =noneCEC=1- 15cmolc/kgdiameter .1-5um coarse clay - fine silt TERM 24 Pyrophyllite DEFINITION 24 No isormorphic subs Si8Al4O20(OH)4Pyrophyllite is a phyllosilicate mineral composed of aluminium silicate hydroxide: Al2Si4O12. It occurs in two more or less distinct varieties, namely, as crystalline folia and as compact masses; distinct crystals are not known. TERM 25 Smectites - montomorillonite DEFINITION 25 Most substitution is in octahedral layer(Si7.8Al.2) (Al3.4Mg.6)O20(OH)4 TERM 26 Properties of Smectite DEFINITION 26 Internal Surface = very highSurface area = ext. 80-150, int. 550-650 m^2/gPlasticity = highShrink-swell = highCEC =80 to 150 cmolc/kgDiameter .01- 1 um TERM 27 Properties of vermiculite DEFINITION 27 Internal surfave = highsurface area = ext. 70=120, int. 600- 700 m^2/gPlasticity = MeduimShrink-swell = mediumCEC =100-200 cmolc/ kgDiameter = .1 to 5 um TERM 28 Illite DEFINITION 28 Hydrous mica or fine grained micaK1.4(si6.4Al1.6)Al4O20(OH)4 TERM 29 Properties of Illite DEFINITION 29 Internal surface = noneSurface area=70-175 m^2/gPlasticity = medium "slightly"shrink - swell = non-expanding (minimal swelling)CEC = 10-40 cmolc/kgDiameter .2 um -2.0 um TERM 30 Clay Mineral Formation DEFINITION 30 Clay minerals formed by physical and chemical weathering or alteration of certain primary minerals.Ex. feldspar, micas, muscovite, biotite TERM 31 2:1 Vermicolite DEFINITION 31 Tritahedral (Si6Al2)(Mg5.4Fe^3 0.6) O20(OH)4Dioctahedral (Si7.2Al.8)(Al3.4Mg.6)O20(OH)4Substitutions in tetrahedral and OctahedralDioctahedral is more resistant to weatheringDioct>trioct TERM 32 Biotite DEFINITION 32 Biotite is a common phyllosilicate mineral within the mica group, with the approximate chemical formula . K2(Si6Al2) (Mg,Fe)6O20(OH)4 TERM 33 Muscovite DEFINITION 33 Muscovite is a phyllosilicate mineral of aluminium and potassium with formula KAl2(AlSi3O10)(F,OH)2, or (KF)2(Al2O3)3(SiO2)6(H2O).
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