Download PDF by George Henry Dunteman, Moon-Ho R. Ho: An Introduction to Generalized Linear Models (Quantitative
By George Henry Dunteman, Moon-Ho R. Ho
Do you've information that's not in most cases dispensed and do not know the way to research it utilizing generalized linear types (Glm)? starting with a dialogue of primary statistical modeling options in a a number of regression framework, the authors expand those innovations to Glm and show the similarity of varied regression types to Glm. every one approach is illustrated utilizing genuine lifestyles facts units. The e-book presents an available yet thorough advent to Glm, exponential kin distribution, and greatest probability estimation; contains dialogue on checking version adequacy and outline on the way to use Sas to slot Glm; and describes the relationship among survival research and Glm. it's an awesome textual content for social technology researchers who would not have a robust statistical historical past, yet want to study extra complicated options having taken an introductory path masking regression analysis.
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Additional info for An Introduction to Generalized Linear Models (Quantitative Applications in the Social Sciences)
The accumulation of detrital sediments depends on sediment transport (Allen, 1985). When the transport rate changes, erosion or deposition occur. Sediment transport is a periodic phenomenon; however, for all preserved sequences, Statistics for Petroleum Engineers and Geoscientists 9 deposition prevailed in the long term. , 1987). , and their rates of change. Secondary phenomena such as compaction and diagenesis can also modify the petrophysical properties. Nevertheless, the influence of primary depositional texture usually remains a strong determining factor in the petrophysical variability in clastic reservoirs.
For all five wells, Prob(EI) = 3/5, Prob(E2) = 4/5, and Prob(E1 n E2) = 2/5. 48 -:1- Prob(E1 n E2), E1 and E2 are dependent. Excluding Weill, Prob(E1) = 2/4, Prob(E2) = 1, and Prob(E1 n E2) =2/4. 5 = Prob(E1 n E2), so E1 and E2 are independent. Clearly, the data in Weill are important in assessing the independence of these two events. Statistical independence may or may not coincide with geological independence. There may be a good geological explanation why facies C should be lower in the sequence than either A orB.
The most common measurement is on plugs extracted from the subsurface; on certain types of media, larger pieces of the core may be used-the so-called whole-core measurements. All of these measurements are quite small-scale. Far larger volumes--of the order of several cubic meters--of a reservoir may be sampled through well testing. All techniques are fraught with difficulties. Consequently, we inevitably see correlations of permeability with other petrophysical quantities. The primary correlant here is porosity; the reader will see numerous references to log(k) vs.
An Introduction to Generalized Linear Models (Quantitative Applications in the Social Sciences) by George Henry Dunteman, Moon-Ho R. Ho