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31. Clay Minerals - Vancouver Island University
USC Mineralogy Geol 215a (Anderson) Clay Minerals Clay minerals likely are the most utilized minerals … not just as the soils that grow plants for foods and garment, but a great range of applications, including oil absorbants, iron casting, animal …
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3 Groundwater geochemistry - Vancouver Island University
web.viu.ca3 Groundwater geochemistry In this section we will look at the general chemical characteristics of groundwaters, and at some of the geochemical processes that are important in the chemical evolution of water that flows through the ground – including
Surfactants, soaps, and detergents
web.viu.caCase Study # 3 – Surfactants, soaps and detergents 5 Switchable surfactants give on-demand emulsions Oil and water can now be mixed or separated simply by bubbling carbon dioxide or air
Naming Rules for Organic Compounds
web.viu.caAlkynes - compounds containing carbon-carbon triple bonds 1) Are named and numbered like alkenes. Add "yne" to root name. Aromatic Hydrocarbons - Compounds containing benzene-like rings 1) Benzene is the simplest aromatic compound containing cyclic structure of six carbons with a total of three double bonds. benzene NOT 1,3,5-cyclohexatriene ...
UNITS OF CONCENTRATION
web.viu.caConcentrations expressed as ppm and N are less familiar to most students at this stage. Parts per million: The number of milligrams of solute per kg of solution = one ppm, since 1 mg = 10-3 g and 1 kg = 103 g. Assuming the density of water is 1.00 g/mL, 1 liter of solution = 1 kg and hence, 1 mg/L = 1 ppm.
UNITS OF CONCENTRATION
web.viu.caNormality is a somewhat dated concentration unit that is still encountered in may texts and lab manuals. It has advantages when carrying out titration calculations, however it can be confusing for the uninitiated. Normality is defined as the number of equivalents of solute per liter, and as such, is similar to Molarity.
Principles of GW Flow - Vancouver Island University
web.viu.caPrinciples of groundwater flow Hydraulic head is the elevation to which water will naturally rise in a well (a.k.a. “static level). Any well that is not being pumped will do for this, but a well that is created especially for measuring hydraulic head is known as an observation well a monitoring well or a piezometer. For unconfined
Glacial Tills - Vancouver Island University
web.viu.caTypes of Glacial Till Sub-glacial tills •Lodgement till (“lodged” by the ice onto the substrate) •Sub-glacial meltout till (commonly forms within cavities) •Deformation till (deformation of soft non-glacial sediments) Supra-glacial tills •Supra-glacial meltout till …
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Basic Relationships of Well Log Interpretation
store-assets.aapg.orgLithology and Mineralogy In well-log analysis, the terms lithology and miner-alogy are used with some ambiguity. Lithology is often used to describe the solid (matrix) portion of the rock, generally in the context of a description of the primary mineralogy of the rock (e.g., a sandstone as a descrip-tion of a rock composed primarily of quartz ...
CHEMICAL ANALYSIS OF MINERALS
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11. Hydrothermal Alteration - USGS
pubs.usgs.govtion to begin to understand alteration mineralogy and chem-istry and the spatial arrangement of alteration types related to VMS systems: the Galapagos Rift stockwork zone, mafic systems at TAG, a siliciclastic mafic system at Middle Valley, and a bimodal felsic system in Manus Basin north of Papua New Guinea (fig. 11–1).
VOLCANIC-ASSOCIATED MASSIVE SULFIDE DEPOSITS …
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Acid Mine Drainage
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