This assignment is related to Geochemistry. It looks simple, but be careful not to make mistakes. EPS131_2014_Lecture9.pdf Download Attachment This is an unformatted preview. Please download the attached document for the original format. Today’s road map: 1.? Thermodynamics of solu4ons and mixtures 1.? par4al molar proper4es 2.? chemical poten4al 3.? ideal mixing; mechanical mixtures 4.? ideal solu4ons 5.? non-?ideal solu4ons 2.? Phase diagrams (con$nued): a.? two components b.? solid solu4on c.? binary eutec4c d.? P-?X diagrams of gases To 1.? 2.? 3.? 4.? 5.? 6.? 1 Thermodynamics of solu4ons and mixtures: Most geologic materials are solu4ons of variable composi4on. For example, the minerals is igneous petrology contain more than one component; they are solid solu4ons. A solu$on is formed by dissolving one or more substance (solid, liquid or gas), in another substance (solid, liquid or gas). If a homogeneous solu4on, it can be treated in thermodynamics as a phase. The solu4on itself can be either solid (e.g., plagioclase feldspar is a solu4on of albite (NaAlSi3O8) and anorthite (CaAl2Si2O6), liquid (e.g., NaCl or CO2 dissolved in water) or gas (e.g., our atmosphere). A solu4on may be ideal or non-?ideal; with thermodynamic proper4es depending on this ideality. Almost all major igneous minerals (olivine, pyroxenes, amphiboles, feldspars, micas) are solid solu4ons of two or more components. Quartz is the notable excep4on. 2 Thermodynamics of solu4ons and mixtures: Non-?ideal behavior of a gas mixture is to modify the ideal gas law to ?t available P-?V-?T data. Non-?ideality in liquid and solid solu$ons can be described as devia4on from ideality à? using “excess func$ons” To de?ne the composi4on of a solu4on, we need: 1.? to know what substances are present : components or (less restric4vely) cons$tuents = any combina4on of elements in the system in any