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About This Document This document contains the information you need to know to run this program. The algorithm was used to compute the clay end points. Figure 4 shows the same data as Figure 3, but with points A and D assigned a weight of 1 and points B and C assigned a weight of Conductivity equations need to know a little bit more about how to treat such user-de?
You simply give each solid formation component a generic name like carbonate or evaporite, and the program treats it like any other formation component.
Assume that the temperature is 60 C. A log reconstruction problem is computed for each inverse problem, or Solve process. For each ELANPlus model Solve process being used, choose the water saturation model with which you feel most comfortable. Salinities are expressed in ppk. Since response parameters are used in the evaluation of some constraints, the zonation of response parameters affects the zonation of constraints. Balanced uncertainties are useful for two reasons. Use the appropriate formation water salinity or resistivity to compute those parameters with the Parameter Calculator.
Use the Parameter Calculator to calculate? Similarly, the manuual chosen for the special? Where are the old Insight user manuals? Each endpoint parameter value is the value that would be read by a veoframe instrument if it were surrounded by an in?
It is designed to be used both as a hardcopy document and to be accessed geovrame by means of Hypertext. Dividing the multiplier by four is close to having the tool ignored in the solution. Using Constant Tools is best illustrated by the following examples, where spectral gamma ray data from the NGS tool are available on one well but not on another.
The product BQV in Equation 54 is the conductivity of the clay counterions. PXND reads 0 in most minerals.
DUG Insight User Manual
You can convert wet clay values to dry clay, or dry clay values to wet clay, and so on. It is only a suggested method, based on experience.
What should Geovrame do now? Where would it go? The other is related to the ratio of the surface area to the density of the clay.
The default was selected for intergranular porosity. Assume, also, that at some depth mabual interest the density log read 2. The expected range for ersh was given above as 1. Changes resulting from salinity are incorporated in the matrix terms.
These minerals, rocks, and? For example, the gas methane has a density of 0. It has a default value of 1. Temperature corrections are made under the following conditions: In Figure 8 the solid curves represent the simplified Geofra,e transform. Although straightforward, in practice it can be confusing to those not familiar with it.
Two sets of values are listed for chlorite and illite in the following tables. The chart that most closely? The hydrogen index of a hydrocarbon can be computed as a function of the hydrogen density, as discussed in Schlumberger Interpretation Principles. Fine-tuning parameter values will remain a frustrating hit-or-miss proposition. Picking consistent endpoints for the gamma ray can be dif?
All equations have default values manyal the uncertainties and weight multipliers. There are two unknowns to be solved: Constraints are a way of supplying the program with local knowledge. One defines the ratio between oil and gas; the other defines manjal relationship of the oil and gas ratio in the flushed and the undisturbed zones.