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Business Communication Trends1

Course: BUSINESS XCOM/285, Spring 2011
School: University of Phoenix
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Word Count: 410

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head: Running BUSINESS COMMUNICATION TRENDS 1 BUSINESS COMMUNICATION TRENDS JAMES WHITE XCOM/285 MAY 22, 2011 UNIVERSITY of PHOENIX (Axia) BUSINESS COMMUNICATION TRENDS 2 BUSINESS COMMUNICATION TRENDS Being a soldier in the United States Army, business communication plays a vital role in my day to day activities. As an organization we relied heavily on business communications. The role of business communication...

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head: Running BUSINESS COMMUNICATION TRENDS 1 BUSINESS COMMUNICATION TRENDS JAMES WHITE XCOM/285 MAY 22, 2011 UNIVERSITY of PHOENIX (Axia) BUSINESS COMMUNICATION TRENDS 2 BUSINESS COMMUNICATION TRENDS Being a soldier in the United States Army, business communication plays a vital role in my day to day activities. As an organization we relied heavily on business communications. The role of business communication in the Army is vital to our overall accomplishment of missions. We relies heavily on email, training and verbal communications not mention video-conferences. This allows us to arrange meetings with our unit's Commanders, regardless of the location. As an organization we tend to use more nonverbal communication such as e-mail. This allows for us to have a more effective and rapid way to receive and transport information. We as an organization relay information throughout our organization, several ways such as reports, email, power points, telephone and the biggest one videoconferencing. By using nonverbal communication it helps us to manage our daily activities without the hassle of traveling from place to place. This process helps us to track movement of our troops as well as keeping in contact no matter where our soldiers may be at. Some of the trends I see in our organization, bulk is and over kill in e-mails, nonverbal communications that is not being absorbed. With the emerged of e-mail communication our Commanders are relying heavily on nonverbal communications. This trend has the potential to create problems, such as the lost of e-mails, security breach and the possibility of having our systems hacked or being exposed to various viruses. These trends has the potential not only be good, but can be bad also. With the constant change in technology, business communication has gone to a new level. Management tends to get away from the face to face approach to the more easier e-mail option. This can cause employee's in my case soldier's to have low moral without the interactions from our leaders. Soldiers feel as though they are part of a big mixing bowl instead of individuals. Business communication depends on personal preference or professional requirement. Like the old saying there are two sides to every story, in business communication there going to be to side to every form of communication. One must be able to analyze their audience, and be able to determine which form of communication will be the most effective and efficient. Business communications is something one must know to be successful in today's world. BUSINESS COMMUNICATION TRENDS 3
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University of Phoenix - BUSINESS - XCOM/285
Business Writing
University of Phoenix - BUSINESS - XCOM/285
Running head: BUSINESS WRITING PORTFOLIO 1Business Writing Portfolio JAMES WHITE XCOM/285 July 17, 2011 University of Phoenix (Axia)BUSINESS WRITING PORTFOLIO 2Business Writing Portfolio Reflection As I reflect on my experience in Essentials of Manager
University of Phoenix - BUSINESS - XCOM/285
CARBOHYDRATE'SWHAT ARE CARBOHYDRATES?DIFFERENT TYPES OF CARBOHYDRATE'SSIMPLE CARBOHYDRATESCOMPLEX CARBOHYDRATESare sugars broken down and used in the body?HowWhat are the benefits that carbohydrates provide to the body?Healthy sources of carbohydr
Ashford University - BUS - 599
Assignment "Alan Mulally, CEO, Ford Motor Company"cfw_ WITH NEW ORIGINAL WORK- BUS520) -Read the case and write a 4-5 page report that answers the following: 1.Discuss the role of leadership and how it can impact organizational performance. 2.Discuss Mula
Ashford University - BUS - 599
Case: "Conflict Resolution at General Hospital" Read the case and write a 4-5 page report that answers the following: 1.Discuss the conflict that is occurring at General Hospital. 2.Discuss the conflict management styles that are evident in the case. 3.Di
Ashford University - BUS - 599
"ROWE Program at Best Buy"cfw_ WITH NEW ORIGINAL WORK- BUS 520)-Read the case and write a 4-5 page report that answers the following: 1.Describe the culture of Best Buy. 2.Discuss the approach to organizational change that the ROWE program illustrates. 3.
Ashford University - BUS - 599
FedEx Office and Print Service, Inc.," Respond to the following: o Identify the concepts of vertical design used in the case. o Explain why each is considered a vertical design element.[250 WORDS]
Ashford University - BUS - 599
"How Personal Can Ethics Get?" (Integrated cases - read the case and write a 4-5 page report that answers the following: 1.Discuss how personal differences and preference can impact organizational ethics. 2.Discuss how organizational policies and procedur
Ashford University - BUS - 599
Allstate Insurance Company" Read the case and write a 4-5 page report that answers the following: 1-Using the model for goal setting, evaluate Allstate's goal setting process to determine whether or not Allstate has an effective goal-setting program. 2- D
Ashford University - BUS - 599
Discussion: Costco Wholesale Please respond to the following: -Discuss and evaluate Costco's strategy in terms of pricing, product selection, and marketing and advertising strategy. -Determine whether or not Costco can achieve a sustained competitive adva
Ashford University - BUS - 599
Discuss: The possible challenges you may face as you progress in this class and then recommend how you may be able to overcome those challenges (250 words)
Ashford University - BUS - 599
Discuss:the elements of Starbuck's business strategy and how execution of the strategy lead to company growth and provided the organization a competitive advantage in the marketplace. [250 words]
Ashford University - BUS - 599
Discussion:Evaluate the company objectives for General Motors, The Home Depot, YUM! Brands, and Avon. Discuss whether or not the objectives are measurable and achievable 250 words.
Stony Brook University - PHYSICS - 384
Terrain correctionHammer correctionApplied Geophysics Corrections and analysisFree-air anomalyA gravity anomaly suggests the difference between atheoretical and observed value.Tie survey to base station where absolute gravity is knownThen the free-
Stony Brook University - PHYSICS - 384
Introduction to geophysical methods:Techniques and targetsReference:Sharma p1-10Reynolds p1-27Applied geophysics IntroductionWhat do we mean by applied geophysics?Applied geophysics Introduction1
Stony Brook University - PHYSICS - 384
ExamplesDelineating bedrockOver-interpretation?Look for additional data Local geology Other surveys BoreholesApplied Geophysics Seismic reflection IVExamplesGroundwaterObjective:Map subsurfacelocation of aquifer forthe purpose of drillinga w
Stony Brook University - PHYSICS - 384
ExamplesFaults and flat spotsFlat spots and bright spots:indicate oil or gasApplied Geophysics Seismic reflection IVExamplesDelineating bedrockWhy would we want to know this?Correlating seismic with well log data Drilling a well provides ground t
Stony Brook University - PHYSICS - 384
Velocity analysisDetermination of seismicvelocity is key to seismicmethodsVelocity is needed to convert thetime-sections into depth-sections i.e.geological cross-sectionsUnfortunately reflection surveysare not very sensitive to velocityOften comp
Stony Brook University - PHYSICS - 384
MultiplesDue to multiple bounce paths in the sectionLooks like repeated structureThese are also removed with deconvolution easily identified with an autocorrelation removed using cross-correlation of theautocorrelation with the waveformSea-bottom r
Stony Brook University - PHYSICS - 384
Induced magnetization (JI) andmagnetic susceptibility A magnetizable body acquires magnetization when Hfield is applied Disappears when field is removed Field induces magnetization in material The induced magnetization is parallel andproportional t
Stony Brook University - PHYSICS - 384
Analytic Signal Combination of derivatives: Shape is independent of inclination/declination of induced field.18
Stony Brook University - PHYSICS - 384
Variations in gLarge scale variations:global or regionsSmaller scale variations:localThis is what we want tomake use ofApplied Geophysics Gravity theory and measurementThe geoidMean sea level is anequipotential surfaceit is the geoidApplied Ge
Stony Brook University - PHYSICS - 384
Gravity surveyingDriftThe reading of a gravimeters at a point changes with time!Causes Instrument drift: due to environmental changes (P,T) and spring creep Earth tides: relative rotations of the earth, moon and sunApplied Geophysics Gravity theory
Stony Brook University - PHYSICS - 384
Reflectivity and convolutionThe seismic wave is sensitive tothe sequence of impedancecontrastsThe reflectivity series (R)We input a source wavelet (W) which isreflected at each impedance contrastThe seismogram recorded at the surface(S) is the con
Stony Brook University - PHYSICS - 384
Fresnel ZoneTells us about the horizontal resolutionon the surface of a reflectorFirst Fresnel ZoneThe area of a reflector that returns energy tothe receiver within half a cycle of the firstreflectionThe width of the first Fresnel zone, w:2 w2d
Stony Brook University - PHYSICS - 384
Gravity anomaly mapApplied Geophysics Corrections and analysisSimple shape anomaliesApplied Geophysics Corrections and analysis7
Stony Brook University - PHYSICS - 384
Profile Cusps Wenner Arrayi. Current lines converge towardboundary, decrease potentialgradient at potential electrodesii. C2 at boundaryiii. Current density increases adjacentto boundary in low resistivity unit,causes potential gradient betweenpot
Stony Brook University - PHYSICS - 384
Suppression Principle of suppression:Thin layers of smallresistivity contrast withrespect to background willbe missed. Thin layers of greaterresistivity contrast will bedetectable, but equivalencelimits resolution ofboundary depths, etc.Horizon
Stony Brook University - PHYSICS - 384
Equivalence: several models producethe same results Ambiguity in physics of 1D interpretation such thatdifferent layered models basically yield the sameresponse. Different Scenarios: Conductive layers between two resistors, wherelateral conductance
Stony Brook University - PHYSICS - 384
ConvolutionReflectivityseriesSourcewavelet1-Output10RecordedwaveformApplied Geophysics Seismic reflection IConvolutionReflectivityseriesSourcewaveletOutput1-101RecordedwaveformApplied Geophysics Seismic reflection I9
Stony Brook University - PHYSICS - 384
Reflectivity and convolutionThe seismic wave is sensitive tothe sequence of impedancecontrastsThe reflectivity series (R)We input a source wavelet (W) which isreflected at each impedance contrastThe seismogram recorded at the surface(S) is the con
Stony Brook University - PHYSICS - 384
ExamplesElectromagnetic surveyingApplied geophysics IntroductionExamplesElectromagnetic surveyingApplied geophysics Introduction14
Stony Brook University - PHYSICS - 384
Geometrical FactorsArray advantages and disadvantagesArrayAdvantagesDisadvantagesWenner1. Easy to calculate a in the 1. All electrodes moved eachsoundingfield2. Sensitive to local shallow2. Less demand onvariationsinstrument sensivity3. Long
Stony Brook University - PHYSICS - 384
Current density and equipotential linesfor a current dipoledfraction total current 2z 2i f = tan1 dif=0.5 atz=d2if=0.7 at z = dWider spacing Deeper currentsApparent ResistivityPrevious expression can berearranged in terms of resistivity:=
Stony Brook University - PHYSICS - 384
Two Current Electrodes: Source and Sink Why run an electrode to infinity when we can use it?sourcesinkrsourcePrsinkVsource =Total Voltage at P:i2rsourceVsin k =Vp = Vsource Vsin k =i2 rsinki 11r2 source rsink Measurement Practicalities
Stony Brook University - PHYSICS - 384
Generalized reciprocal methodProcedure:Velocity analysis function, TV Calculate TV as a function ofoffset AG for a variety of XYdistances The optimal XY is when E and Fconverge on H Optimal XY is identified by thesmoothest TV curveTV Refractor
Stony Brook University - PHYSICS - 384
Generalized reciprocal methodThe plus-minus methodassumes a planar interface andshallow dip between C and EThe generalized reciprocalapproach uses two geophones,X and Y, recording refractedarrivals originating from thesame point on the refractora
Stony Brook University - PHYSICS - 384
Alkali Vapor MagnetometerAdvantages Dont have to align bottle with field Very rapid, almost continuousDisadvantages Cant measure vector fieldMeasurement accuracy : 0.01 to 1nTMagnetic Gradiometer Takes differences between two measurements that ar
Stony Brook University - PHYSICS - 384
Alkali Vapor Magnetometer Basic Physics: Uses precession frequency of alkali vapor Quantum mechanics Magnetometer construction:Bottle filled with cesium or rubidium vaporPolarized light source of same elementCoil to generate radio frequency magneti
Stony Brook University - PHYSICS - 384
Suppression Principle of suppression:Thin layers of smallresistivity contrast withrespect to background willbe missed. Thin layers of greaterresistivity contrast will bedetectable, but equivalencelimits resolution ofboundary depths, etc.12
Stony Brook University - PHYSICS - 384
Equivalence: several models producethe same results Ambiguity in physics of 1D interpretation such thatdifferent layered models basically yield the sameresponse. Different Scenarios: Conductive layers between two resistors, wherelateral conductance
Stony Brook University - PHYSICS - 384
ExamplesSeismic reflectionApplied geophysics IntroductionExamplesSeismic reflectionApplied geophysics Introduction5
Stony Brook University - PHYSICS - 384
Reflection and transmissionSeismic rays obey Snells Law(just like in optics)The angle of incidence equals theangle of reflection, and the angle oftransmission is related to the angle ofincidence through the velocity ratio.But a conversion from P to
Stony Brook University - PHYSICS - 384
DeploymentImportant considerations Need good coupling to the ground spike Mini-arrays to reduce surface wave noiseOffset of geophonesSmall offsets Near-vertical incidence retains P-energy High resolution of subsurface reflectorsSeismic reflection
Stony Brook University - PHYSICS - 384
ExamplesGravityApplied geophysics IntroductionExamplesSeismic refractionApplied geophysics Introduction12
Stony Brook University - PHYSICS - 384
Definitions: Magnetic fieldstrength or intensity Biot-Savarts law definition:for a loop of wire of radius r that iscarrying a current I, H at center isgiven as:H=nI/2r [A/m]where n is a unit vector normal to theplane of the loop. The magnetic fie
Stony Brook University - PHYSICS - 384
Definitions: Magnetic fieldor flux density Definition: Vector quantity defining the magneticflux/unit area; i.e., the density of the magnetic field lines.Thus often called Flux Density Mathematical Definitions:o pp Wbr = c 2 r 2 = Tesla Air:4 r
Stony Brook University - PHYSICS - 384
Magnetization or magnetic polarization A measure of the pole strength/unit area along oneof the ends of magnetic material:J=(p/A) n [A/m]Magnetic moment Strength of a magnetic field generatorM=J V = p l [A m2]For a loop of current: M=(Ir2) n
Stony Brook University - PHYSICS - 384
Dipole nature of magnetic materialsBar MagnetN+ Although, no magnetic monopolesexist in nature, they are useful fortheory: magnetic monopoles of samesign repel, opposite signs attract.S Dipole created by two poles ofopposite sign and separated by
Stony Brook University - PHYSICS - 384
Definitions: Magnetic potential Remember that the potential is defined as thepotential to do work.o pp Wb =c W= Magnetic Potential:4 rrmwhere o=4 10-7 [H/m] is the magnetic permeability of free spaceand p [A/m] is magnetic pole strength Gravit
Stony Brook University - PHYSICS - 384
Applications Shallow (Engineering and Environmental):contaminants, toxic waste, pipes, cables and metalinclusions Military: location of UXOs Archeology: buried walls, old fire pits Mining: iron sulfide deposits Oil and groundwater: depth to magneti
Stony Brook University - PHYSICS - 384
Derivatives Emphasizing shorter wavelength features. First vertical derivative emphasizes near surface features. It canbe measured with gradiometer, or derived from corrected data Second vertical derivative emphasizes boundaries of targetzones.Reduc
Stony Brook University - PHYSICS - 384
Removal of Regional Use formula tosubtract off IGRFvalue. Filtering processes toget the regional formula(like gravity).General Guidelines16
Stony Brook University - PHYSICS - 384
Gravity Anomalies: 2D forward calculationfor rectangular parallelepipeds with greater vertical extent than horizontalSpreadsheet: Grav2Dcolumnsee Dobrin and Savit eq 12-34Gravity anom aly2.50Define density structureProfile 10.30.30.30.30.30.3
Stony Brook University - PHYSICS - 384
SpikingdeconvolutionRecordedwaveform1-1Deconvolutionoperator101-1Output0RecoveredreflectivityseriesApplied Geophysics Seismic reflection IISpikingdeconvolutionRecordedwaveform1-1Deconvolutionoperator11100Output0-Recovere
Stony Brook University - PHYSICS - 384
Spiking deconvolutionApplied Geophysics Seismic reflection IISpikingdeconvolutionRecordedwaveformDeconvolutionoperatorOutput11-10-11RecoveredreflectivityseriesApplied Geophysics Seismic reflection II3
Stony Brook University - PHYSICS - 384
Vertical Electric Sounding When trying to probe howresistivity changes withdepth, need multiplemeasurements that each givea different depth sensitivity. This is accomplished throughresistivity sounding wheregreater electrode separationgives great
Stony Brook University - PHYSICS - 384
Geometrical FactorsArray advantages and disadvantagesArrayAdvantagesDisadvantagesWenner1. Easy to calculate a in the 1. All electrodes moved eachsoundingfield2. Sensitive to local shallow2. Less demand onvariationsinstrument sensivity3. Long
Stony Brook University - PHYSICS - 384
Current density and equipotential linesfor a current dipoledfraction total current 2z 2i f = tan1 dif=0.5 atz=d2if=0.7 at z = dWider spacing Deeper currentsApparent ResistivityPrevious expression can berearranged in terms of resistivity:=
Stony Brook University - PHYSICS - 384
Horizontal interfaceTraveltime equationsDirect wave:T=HeadwavexV1Head wave:T = TSB + TDD ' + TBDT=2h1x 2h1 tan ic+V1 cos icV2T=22x 2h1 V2 V1+V2V2V1T = ax + bslope: 1/V2intercept: gives h1Applied Geophysics Refraction IHorizontal
Stony Brook University - PHYSICS - 384
Critical incidenceWhen rP = 90 iP = iC the critical anglesin iC =VP1VP 2The critically refracted energy travelsalong the velocity interface at V2continually refracting energy back intothe upper medium at an angle iCa head waveReflection and tran