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TAMU Kingsville - EVEN - 6318
Interphase Mass-transfer-Equilibrium Partitioning81+D=FJAH'INTERPHASE MASS-TRANSFER EQUILIBRIUM PARTITIONINGChapter Goals The concept of thermodynamic equilibrium Common equilibrium partitioning relationshipsINTRODUCTIONIn the last ch
TAMU Kingsville - EVEN - 6318
Chapter Goals+D=FJAHMASS-BALANCE EQUATIONS OTHER SALIENT CONCEPTS Learn about steady-state and transient models Simplifications of mass-balance expressions Understanding the importance of various processes using dimensionless groupsINTROD
TAMU Kingsville - EVEN - 6318
2)46*MATHEMATICAL AND NUMERICAL TECHNIQUESCOMPUTING TOOLS FOR MODEL DEVELOPMENTChapter Goals+D=FJAH Learn about various computing tools for building environmental models Evaluate the use of spreadsheets for model development Explore bas
TAMU Kingsville - EVEN - 6318
162 Applied Environmental Systems Modeling"MATRICESAND+D=FJAHEQUATIONSLINEAR SYSTEMOFChapter Goals How to perform matrix operations in MS-EXCEL Solving system of linear equations in MS-EXCELINTRODUCTIONIn the last chapter we saw ho
TAMU Kingsville - EVEN - 6318
218 Applied Environmental Systems Modeling%NUMERICAL METHODS FOR SOLVING FIRST-ORDER ODESChapter Goals Explore certain numerical methods for solving first-order ODEs Implement Euler and Runge-Kutta methods using MS-EXCEL+D=FJAHINTRODUCTION
TAMU Kingsville - EVEN - 6318
70 Applied Environmental Systems Modeling+D=FJAH&INTERPHASE MASS-TRANSFER KINETIC THEORIESChapter Goals Learn about interphase mass-transfer Single-resistance and two-film theories of mass-transferINTRODUCTIONMany contaminants can exist
TAMU Kingsville - G - 4425
Lecture Outline Geographic Information SystemLecture 1Introduction to GISDefinition of GIS Four component of system Three view of GIS Major characteristics Software packages GIS applicationsWhat is GIS?GIS: a particular form of information syst
TAMU Kingsville - G - 3450
Grid Cell/Square based Raster ModelRowsField Mapping, Cartography and Global PositioningLecture 6. Terrain ModelingGrid extentGrid cellResolutionRaster resolution Measured by cell size Storage space increases dramatically with precisio
TAMU Kingsville - G - 4425
Tessellation of Geographical SpaceGeographic Information System Lecture 6GIS Data Model: Raster Data StructuresGeographical space can be tessellated into sets of connected discrete units, which completely cover a flat surface. The units can be i
TAMU Kingsville - L - 5312
Tessellation of Geographical SpaceGeographic Information System Lecture 6GIS Data Model: Raster Data StructuresGeographical space can be tessellated into sets of connected discrete units, which completely cover a flat surface. The units can be i
TAMU Kingsville - L - 1302
Glaciers: a part of two basic cycles in the Earth systemEarth Science, 11eGlaciers, Deserts, and Wind Chapter 6Glaciers are a part of both the hydrologic cycle and rock cycle Glacier - a thick mass of ice that forms over land from the compaction
TAMU Kingsville - L - 1301
Volcanic eruptionsEarth Science, 11eVolcanoes and Other Igneous Activity Chapter 9Factors that determine the violence of an eruption Composition of the magma Temperature of the magma Dissolved gases in the magmaViscosity of magma Viscosity
TAMU Kingsville - L - 1301
Earth Science, 11eMinerals: Building Blocks of Rocks Chapter 2QuartzOlivineFluoriteBeryl (variety aquamarine) Realgar1Bornite and ChalcopyriteNative copperGold nuggetCut diamondMinerals: the building blocks of rocksDefinition of
TAMU Kingsville - L - 1302
The geologic time scaleEarth Science, 11eEarths History: A Brief Summary Chapter 12Precambrian era4.5 billion to 540 million years ago 88% of Earth's history Only sketchy knowledge Most Precambrian rocks are devoid of fossilsPrecambrian eraP
TAMU Kingsville - L - 1302
Early history of astronomyEarth Science, 11eOrigin of Modern Astronomy Chapter 21Ancient Greeks Used philosophical arguments to explain natural phenomena Also used some observational data Most ancient Greeks held a geocentric (Earth-centered)
TAMU Kingsville - L - 1302
Earth as a system: the hydrologic cycleEarth Science, 11eIllustrates the circulation of Earth's water supply Processes involved in the cycle Precipitation Evaporation Infiltration: water soaks into the ground Runoff: Surplus water flows over t
TAMU Kingsville - L - 5312
Find pathGeographic Information SystemsLecture 11. Network Analysis1Best way to school (Barrier)Distance2BarrierFind path with stopsAdvanced Path3Finding transportation network errorFinding loops Water network4Find connect
TAMU Kingsville - L - 1301
Composition of seawaterEarth Science, 11eOcean Water and Ocean Life Chapter 14Seawater consists of about 3.5% (by weight) dissolved minerals Salinity Total amount of solid material dissolved in water Typically expressed in parts-per-thousand (
TAMU Kingsville - L - 5312
Scanned ImageNew map in GIS database Define ProjectionGCP acquisition GPS, Aerial photo Accuracy Checking RMS errorProjection of GCP points Link table Geometric transformation ResamplingVector digitizationGeoreferenced Image!12#& '
TAMU Kingsville - L - 1301
EarthquakesEarth Science, 11eEarthquakes and Earths Interior Chapter 7General features Vibration of Earth produced by the rapid release of energy Associated with movements along faults Explained by the plate tectonics theory Mechanism for ea
TAMU Kingsville - G - 3450
Why DGPS? Field Mapping, Cartography and Global PositioningLecture 9. Differential GPSReference from Trimble WebsiteWhy Differential GPS? For many applications Basic GPS is plenty accurate. Some crafty engineers came up with "Differential GPS,"
TAMU Kingsville - L - 1301
Continental drift: an idea before its timeEarth Science, 11ePlate Tectonics: A Scientific Theory Unfolds Chapter 8Alfred Wegener First proposed hypothesis, 1915 Published The Origin of Continents and OceansContinental drift hypothesis Super
TAMU Kingsville - L - 5312
! " # $ % & ! 'Scanned ImageNew map in GIS database Define ProjectionGCP acquisition GPS, Aerial photo Accuracy Checking RMS errorProjection of GCP points Link table Geometric transformation Resampling! " ! " # #Vector digitizationGeoref
TAMU Kingsville - L - 1302
Earth's external processesEarth Science, 11eWeathering, Soil, and Mass Wasting Chapter 4Weathering the disintegration and decomposition of material at or near the surface Mass wasting the transfer of rock material downslope under the influence
TAMU Kingsville - L - 5312
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TAMU Kingsville - G - 3450
Why GPS? Field Mapping, Cartography and Global PositioningLecture 7. Global Positioning System Part IReference from Trimble Website Figure out where you are and where you're going Navigation and positioning are crucial to so many activities The
TAMU Kingsville - L - 1301
Rock cycleEarth Science, 11eRocks: Materials of the Solid Earth Chapter 3Shows the interrelationships among the three rock types Earth as a system: the rock cycle Magma Crystallization Igneous rock Weathering, transportation, and deposition
TAMU Kingsville - L - 1302
Historical notesCatastrophism Landscape developed by catastrophes James Ussher, mid-1600s, concluded Earth was only a few thousand years old11. Geologic TimeModern geology Uniformitarianism Fundamental principle of geology "The present is t
TAMU Kingsville - L - 1301
DeformationEarth Science, 11eMountain Building Chapter 10Deformation is a general term that refers to all changes in the original form and/or size of a rock body Most crustal deformation occurs along plate margins Factors that influence the stre
TAMU Kingsville - L - 1301
Ocean water movementsEarth Science, 11eThe Dynamic Ocean Chapter 15Surface circulation Ocean currents are masses of water that flow from one place to another Surface currents develop from friction between the ocean and the wind that blows acro
TAMU Kingsville - G - 3450
GPS Menu Field Mapping, Cartography and Global PositioningLecture 8. GPS SettingReference from Trimble WebsiteCommunication Protocol NMEA 0183: The National Marine Electronics Association Protocol TSIP: Trimble Standard Interface Protocol Eart