Net logger iso 3.875 download

It supports programming, communication, and data retrieval between data loggers and a PC. LoggerNet consists of a server application and several client applications integrated into a single product.

It can support connection to a single data logger, but it is especially adept in applications that require telecommunications or scheduled data retrieval used in large data logger networks.

Download the Trial. A copy of the current software license agreement end-user license agreement for LoggerNet is available in the LoggerNet Instruction Manual. The standard LoggerNet software package is recommended for those who have data logger networks that do not require the more advanced features offered in LoggerNet Admin.

It includes the LoggerNet server and client applications. Note: The following shows notable compatibility information. It is not a comprehensive list of all compatible or incompatible products. LoggerNet runs on a PC, using serial ports, telephony drivers, and Ethernet hardware to communicate with data loggers via phone modems, RF devices, and other peripherals. LoggerNet is a collection of bit programs designed to run on Intel-based computers running Microsoft Windows operating systems.

The recommended minimum computer configuration for running LoggerNet is Windows 7. LoggerNet also runs on Windows 8 and Windows LoggerNet runs on both bit and bit versions of these operating systems. A version of LoggerNet 4. A change was made in the way the LoggerNet 4. A corresponding change was made in the Connect Screen 4. This application requires the Microsoft. Net 4. If it is not already installed on your computer, it can be obtained from the Microsoft Download Center.

Supported Operating Systems: 32 and 64 bit Windows 10, 8. LoggerNet 4. This tutorial demonstrates some of the new features and enhancements. Two new applications, View Pro and the Network Planner, are introduced. Current LoggerNet users: It is recommended that you install the trial on a computer other than the one running your existing LoggerNet.

If that is not practical, we strongly recommend you back up the LoggerNet working directory to prevent backward compatibility issues if you revert to a previous version. To revert you must re-install LoggerNet using the original disk and software key.

Note: This application requires the Microsoft. Premium Packages. Standard Packages. Console Mounting Packages.

Mounting Bases. Tunnel Mounts. Tunnel Mounts Wide. Tunnel Mount Accessories. Passenger Side Mounts. Complete C-M Series. Components C-B Series. Accessory Pockets. Equipment Brackets. Filler Plates. Overhead Consoles. Vehicle-Specific VS Series.

Vehicle-Specific with Internal Printer Mount. Universal Consoles. Stout Mount SM. Angled Consoles. Work Truck. Printer Armrests. Stand Alone Armrests. Storage Box Armrests. Cup Holders. Equipment Bracket Chart. Abbreviations Legend. Able 2. Carson Sirens. CV Electronics. Federal Signal. Feniex MFG. General Electric GE. Icom America. Premier Hazard. SoundOff Signal. SpeedTech Lights.

Map Lights. All Accessories. Motion Devices. Swing Arm Mounts. Tilt-Swivel Devices. Slide Out Trays. Trunk Mount Accessories. Trunk Fold Down. Trunk Side Mount. Storage Box. Fold Up Equipment Trays. Pallet Jack.

Bar Clamp Mounts. Connectivity Solutions. Getac K Laptop. Universal Rugged Laptop Cradles. Apple Device Mounts. Dell Tablet Mounts.

Getac Tablet Mounts. Microsoft Surface Cradles. Panasonic Tablet Mounts. Samsung Device Mounts. Havis Tablet Accessories. This Logger Downloads Logger32 Upgrade v4. Logger32 Full v4. Purpose This chart is used similarly to Chart REm to determine the borehole correction applied by the surface acquisition system. Description The six bed thickness correction charts on this page are paired for phase-shift and attenuation resistivity at different values of true Rt and shoulder bed Rs resistivity.

Only uncorrected resistivity values are entered on the chart, not the resistivity shown on the log. Enter the chart on the x-axis at 6 ft and move upward to intersect the in. Spacing Dielectric CorrectionOpen Hole. Purpose This chart is used to estimate the true resistivity Rt and dielectric correction r.

Rt is used in water saturation calculation. The intersection point of the two values is used to determine Rt and the dielectric correction. Rt is interpolated from the subvertical lines described by the dots originating at the The r is interpolated from the radial lines originating from the r values listed on the left-hand side of the chart. Rt and r. Purpose The charts in this chapter are used to determine the correction for invasion effects on the following parameters:.

Description The invasion correction charts, also referred to as tornado or buttery charts, assume a step-contact prole of invasion and that all resistivity measurements have already been corrected as necessary for borehole effect and bed thickness by using the appropriate chart from the Resistivity Laterolog chapter.

To use any of these charts, enter the y-axis and x-axis with the required resistivity ratios. The rst of two approaches is the S w -Archie SwA , which is found using the Archie saturation formula or Chart SatOH-3 with the derived Rt value and known values of the formation resistivity factor FR and the resistivity of the water Rw. If SwA and SwR are equal, the assumption of a step-contact invasion prole is indicated to be correct, and all values determined Sw, Rt, Rxo, and di are considered good.

For more information, see Reference 9. Description The conditions for which this chart is used are listed at the top. Rt and diameter of invasion. Ring, Deep, and Medium Button Resistivity 6. Charts Rt through Rt are similar to Chart Rt for different tool sizes, congurations, and resistivity terms. Rt, di, and Rxo. Deep, Medium, and Shallow Button Resistivity 6. Bit, Ring, and Deep Button Resistivity 6. Ring, Deep, and Medium Button Resistivity in. Deep, Medium, and Shallow Button Resistivity in.

Bit, Ring, and Deep Button Resistivity in. Purpose This chart illustrates the resistivity response, as affected by sand and shale layers, of the arcVISION tool in horizontal wellbores.

The chart is used to determine the values of Rh and Rv. These corrections are already applied to the log presentation. That is, both the layers of shale and the tool are horizontal to the vertical. Other requirements for use of this chart are that the shale resistivity Rsh is 1 ohm-m and the sand resistivity is 5 or 20 ohm-m.

Select the appropriate chart for the attenuation Rad or phaseshift Rps resistivity and values of resistivity of the shale Rsh and sand Rsand. Enter the chart with the volume of shale Vsh on the x-axis and the resistivity on the y-axis. At the intersection point of these two values move straight downward to the dashed blue curve to read the value of Rh.

Move upward to the solid green curve to read the value of Rv. Description Enter the appropriate chart with the value of relative dip angle and move to intersect the known resistivity spacing.

Relative dip angle 34 in. Description Enter the appropriate chart with the value of the phase-shift or attenuation resistivity on the y-axis.

Move horizontally to intersect the resistivity spacing curve. Purpose This log-log chart is used to determine the correction applied to the log presentation of the in.

These data are used to evaluate a formation for hydrocarbons. Description Enter the chart with the ratio of the in. Rad on the y-axis and in. Rad on the x-axis. The intersection point denes the following:. Chart Rt is used for 2-MHz resistivity values. The corresponding charts for resistive invasion are Charts Rt and Rt Example Given: Find: Answer: in. Rxo, di, and correction factor for in. At the intersection point of 0. The value of the in. Rad is reduced by the correction factor: in.

Rad 0. The corrections are already applied to the log presentation. Rad for resistive invasion. The value of Rt is used to calculate water saturation. Description There are two sets of charts for differing conditions:. Bed proximity effect. The top set of charts is appropriate for these resistivity values. Enter the y-axis of the left-hand chart at 1.

The corresponding value on the x-axis is 1 ft, which is the distance of the surrounding bed from the tool. At 2 ft from the bed boundary, the value of in. Distance to bed boundary ft 34 in.

The correction is already applied to the log presentation. Purpose This chart is a method for identifying the type of clay in the wellbore. Description Enter the upper chart with the values of Pe and K to determine the point of intersection. The intersection points are not unique but are in general areas dened by a range of values. Mineral concentration of the logged clay. Purpose This chart is used to determine the type of minerals in a shale formation from concentrations measured by the NGS Natural Gamma Ray Spectrometry tool.

Description Entering the chart with the values of thorium and potassium locates the intersection point used to determine the type of radioactive minerals that compose the majority of the clay in the formation. Purpose This chart is used to determine the lithology and porosity of a formation. The porosity is used for the water saturation determination and the lithology helps to determine the makeup of the logged formation.

At the point of intersection, porosity and lithology values can be determined. Porosity and lithology. This chart is used similarly to Chart Lith-3 for lithology and porosity determination with values of photoelectric factor Pe and. Purpose This chart is used to determine the apparent matrix volumetric photoelectric factor Umaa for the Chart Lith-6 percent lithology determination.

Description This chart is entered with the values of bulk density b and Pe from a density log. The value of the apparent total porosity ta must also be known. The appropriate solid lines on the right-hand side of the chart that indicate a freshwater borehole uid or dotted lines that represent saltwater borehole uid are used depending on the salinity of the borehole uid.

Uf is the uid photoelectric factor. Apparent matrix volumetric photoelectric factor Umaa. Enter the chart with the Pe value 4. Purpose This chart is used to identify the rock mineralogy through comparison of the apparent matrix grain density maa and apparent matrix volumetric photoelectric factor Umaa.

Description The values of maa and Umaa are entered on the y- and x-axis, respectively. The rock mineralogy is identied by the proximity of the point of intersection of the two values to the labeled points on the plot. The effect of gas, salt, etc. Matrix composition of the formation. Purpose This chart is used to help identify mineral mixtures from sonic, density, and neutron logs.

Description Because M and N slope values are practically independent of porosity except in gas zones, the porosity values they indicate can be correlated with the mineralogy. See Appendix E for the formulas to calculate M and N from sonic, density, and neutron logs. Enter the chart with M on the y-axis and N on the x-axis. The intersection point indicates the makeup of the formation. Points for binary mixtures plot along a line connecting the two mineral points. Ternary mixtures plot within the triangle dened by the three constituent minerals.

The effect of gas, shaliness, secondary porosity, etc. The lines on the chart are divided into numbered groups by porosity range as follows: 1. Mineral composition of the formation. The intersection of the M and N values indicates dolomite in group 2, which has a porosity between 0 to 12 p. Description Because M and N values are practically independent of porosity except in gas zones, the porosity values they indicate can be correlated with the mineralogy.

Because the dolomite spread is negligible, a single dolomite point is plotted for each mud. Purpose Charts Lith-9 customary units and Lith metric units provide values of the apparent matrix internal transit time t maa and apparent matrix grain density maa for the matrix identication MID Charts Lith and Lith With these parameters the identication of rock mineralogy or lithology through a comparison of neutron, density, and sonic measurements is possible.

First, apparent crossplot porosity is determined using the appropriate neutron-density and neutron-sonic crossplot charts in the Porosity section of this book. For data that plot above the sandstone curve on the charts, the apparent crossplot porosity is dened by a vertical projection to the sandstone curve. Second, enter Chart Lith-9 or Lith with the interval transit time t to intersect the previously determined apparent crossplot porosity.

This point denes t maa. Third, enter Chart Lith-9 or Lith with the bulk density b to again intersect the apparent crossplot porosity and dene maa. The values determined from Charts Lith-9 and Lith for tmaa and maa are cross plotted on the appropriate MID plot Charts Lith and Lith to identify the rock mineralogy by its proximity to the labeled points on the plot. Purpose Charts Lith and Lith are used to establish the type of mineral predominant in the formation.

Description Enter the appropriate customary or metric units chart with the values established from Charts Lith-9 or Lith to identify the predominant mineral in the formation.

The presence of secondary porosity in the form of vugs or fractures displaces the data points parallel to the apparent matrix internal transit time tmaa axis. The presence of gas displaces points to the right on the chart.

Plotting some shale points to establish the shale trend lines helps in the identication of shaliness. For uid density f other than 1. The predominant mineral. The formation consists of both dolomite and calcite, which indicates a dolomitized limestone.

The formation used in this example is from northwest Florida in the Jay eld. The vugs secondary porosity created by the dolomitization process displace the data point parallel to the dolomite and calcite points. Purpose Chart Lith is used similarly to Chart Lith to establish the mineral type of the formation. Purpose This chart is used to convert sonic log slowness time t values into those for porosity. Description There are two sets of curves on the chart.

The blue set for matrix velocity vma employs a weighted-average transform. The red set is based on the empirical observation of lithology see Reference Enter the chart with the slowness time from the sonic log on the x-axis. Move vertically to intersect the appropriate matrix velocity or lithology curve and read the porosity value on the y-axis. For rock mixtures such as limy sandstones or cherty dolomites, intermediate matrix lines may be interpolated.

To use the weighted-average transform for an unconsolidated sand, a lack-of-compaction correction Bcp must be made. Enter the chart with the slowness time and intersect the appropriate compaction correction line to read the porosity on the y-axis. If the compaction correction is not known, it can be determined by working backward from a nearby clean water sand for which the porosity is known.

Find: Porosity and the formation lithology sandstone, dolomite, or limestone. This intersection point indicates the correction factor curve of 1. Use the 1. Porosity, p. Description Values of log-derived bulk density b corrected for borehole size, matrix density of the formation ma , and uid density f are used to determine the density porosity D of the logged formation.

The f is the density of the uid saturating the rock immediately surrounding the boreholeusually mud ltrate. Enter the borehole-corrected value of b on the x-axis and move vertically to intersect the appropriate matrix density curve.

From the intersection point move horizontally to the uid density line. Follow the porosity trend line to the porosity scale to read the formation. Density porosity. Purpose This chart is used for the apparent limestone porosity recorded by the APS Accelerator Porosity Sonde or sidewall neutron porosity SNP tool to provide the equivalent porosity in sandstone or dolomite formations.

It can also be used to obtain the apparent limestone porosity used for the various crossplot porosity charts for a log recorded in sandstone or dolomite porosity units.

Description Enter the x-axis with the corrected near-to-array apparent limestone porosity APLC or near-to-far apparent limestone porosity FPLC and move vertically to the appropriate lithology curve. Then read the equivalent porosity on the y-axis.

For APS porosity recorded in sandstone or dolomite porosity units enter that value on the y-axis and move horizontally to the recorded lithology curve. Then read the apparent limestone neutron porosity for that point on the x-axis. The APLC is the epithermal short-spacing apparent limestone neutron porosity from the near-to-array detectors. The log is automatically corrected for standoff during acquisition. Because it is epithermal this measurement does not need environmental corrections for temperature or chlorine effect.

However, corrections for mud weight and actual borehole size should be applied see Chart Neu The short spacing means that the effect of density and therefore the lithology on this curve is minimal.

The FPLC is the epithermal long-spacing apparent limestone neutron porosity acquired from the near-to-far detectors. The long spacing means that the density and therefore lithology effect on this curve is pronounced, as seen on Charts Por and Por The same corrections apply.

Resolution Normal Enhanced Not. Find: Porosity for sandstone and for dolomite. Find: Apparent limestone neutron porosity. Answer: Enter the y-axis at 20 p. Move vertically from the points of intersection to the x-axis and read the apparent limestone neutron porosity values.

Apparent limestone neutron porosity, APScor p. It can also be used to obtain the apparent limestone porosity used for the various crossplot porosity charts from a log recorded in sandstone or dolomite porosity units. Move vertically to intersect the appropriate curve and read the porosity for quartz sandstone or dolomite on the y-axis. The chart has a built-in salinity correction for TNPH values. Thermal neutron porosity ratio method Neutron porosity environmentally corrected and enhanced vertical resolution processed Thermal neutron porosity environmentally corrected.

Porosity in sandstone. From the TNPH porosity reading of 18 p. From the y-axis, the porosity of the sandstone is 24 p. Purpose This chart is used similarly to Chart Por-5 to convert in. Fresh formation water is assumed. Purpose This chart is used to determine the porosity of sandstone, limestone, or dolomite from the corrected apparent limestone porosity measured with the adnVISION 4. Description Enter the chart on the x-axis with the corrected apparent limestone porosity from Chart Neu to intersect the curve for the appropriate formation material.

Read the porosity on the y-axis. Description Enter the chart with the environmentally corrected apparent neutron limestone porosity on the x-axis and bulk density on the y-axis. The intersection of the two values describes the crossplot porosity and lithology.

If the point is on a lithology curve, that indicates that the formation is primarily that lithology.

If the point is between the lithology curves, then the formation is a mixture of those lithologies. The position of the point in relation to the two lithology curves as composition endpoints indicates the mineral percentages of the formation.

The porosity for a point between lithology curves is determined by scaling the crossplot porosity by connecting similar numbers on the two lithology curves e. The scale line closest to the point represents the crossplot porosity. Chart Por is used for the same purpose as this chart for saltwater-invaded zones. Crossplot porosity and lithology. This chart applies to boreholes lled with freshwater drilling uid; Chart Por is used for saltwater uids. Anhydrite plots on separate curves.

The gas correction direction is indicated for formations containing gas. Approximate quartz sandstone porosity. Enter at 8 p. Because the APLC porosity value was used, move parallel to the blue gas correction line until the blue quartz sandstone curve is intersected at approximately 19 p.

Find: Approximate quartz sandstone porosity. Answer: Enter 8 p. Because the APLC porosity value was used, move parallel to the blue gas correction line until the blue quartz sandstone curve is intersected at approximately 20 p. Corrected apparent limestone neutron porosity, ADNcor p.

The intersection of the two values is the crossplot porosity. The position of the point of intersection between the matrix curves represents the relative percentage of each matrix material. Crossplot porosity and matrix material. Azimuthal Density Neutron tool to determine the lithology of the logged formation and the crossplot porosity.

Description This chart is applicable for logs obtained in freshwater drilling uid. Enter the corrected apparent limestone porosity and the bulk density on the x- and y-axis, respectively. Their intersection point determines the lithology and crossplot porosity.

Porosity and lithology type. Entering the chart at 20 p. Azimuthal Density Neutron values. Purpose This chart is used to determine crossplot porosity and an approximation of lithology for sonic and thermal neutron logs in freshwater drilling uid. Description Enter the corrected neutron porosity apparent limestone porosity on the x-axis and the sonic slowness time t on the y-axis to nd their intersection point, which describes the crossplot porosity and lithology composition of the formation.

Two sets of curves are drawn on the chart. The blue set of curves represents the crossplot porosity values using the sonic time-average algorithm.

The red set of curves represents the eld observation algorithm. Enter the neutron porosity on the x-axis and the sonic slowness time on the y-axis. The intersection point is at about 25 p. The matrix is quartz sandstone. Purpose This chart is used to determine porosity and lithology for sonic and density logs in freshwater-invaded zones. Description Enter the chart with the bulk density on the y-axis and sonic slowness time on the x-axis. The point of intersection indicates the type of formation and its porosity.

Purpose This chart is used to determine the porosity and average water saturation in the ushed zone Sxo for freshwater invasion and gas composition of C1. Description Enter the chart with the neutron- and density-derived porosity values N and D, respectively. On the basis of the table, use the blue curves for shallow reservoirs and the red curves for deep reservoirs.

Porosity and Sxo. Enter the chart at 25 p. Purpose This chart is used to determine the porosity and average water saturation in the ushed zone Sxo for freshwater invasion and gas composition of CH4 methane. Porosity and S xo. Purpose This nomograph is used to estimate porosity in hydrocarbon-bearing formations by using density, neutron, and resistivity in the ushed zone Rxo logs.

The density and neutron logs must be corrected for environmental effects and lithology before entry to the nomograph. Hydrocarbon-corrected porosity. Enter the p. A line from this value to 38 p. Hydrocarbon-corrected porosity: The intersection point on the 1 scale indicates the value of 1. Draw a line from the 1 value to the origin lower right corner of the chart for versus Shr. This correction factor algebraically added to the porosity 1 gives the corrected porosity.

Purpose This chart is used to estimate the hydrocarbon density h within a formation from corrected neutron and density porosity values. The intersection point of the two values denes the density of the hydrocarbon. Hydrocarbon density. Purpose This chart is used for a variety of conversions of the formation resistivity factor FR to porosity. Description The most appropriate conversion is best determined by laboratory measurement or experience in the area.

In the absence of this knowledge, recommended relationships are the following:. Purpose This chart is used to identify how much of the measured porosity is isolated vugs or moldic or fractured porosity. SatOH Description This chart is based on a simplied model that assumes no contribution to formation conductivity from vugs and moldic porosity and the cementation exponent m of fractures is 1.

When the pores of a porous formation have an aspect ratio close to 1 vugs or moldic porosity , the value of m of the formation is usually greater than 2. Fractured formations typically have a cementation exponent less than 2. Enter the chart with the porosity on the x-axis and m on the y-axis. The intersection point gives an estimate of either the amount of isolated porosity iso or the amount of porosity resulting from fractures fr. Intergranular matrix porosity. Entering the chart with 10 p.

Description If Ro is known, a straight line from the known Ro value through the measured Rt value indicates the value of Sw. If Ro is unknown, it may be determined by connecting Rw with FR or porosity. Water saturation. Draw a straight line from 0. It should be used in clean nonshaly formations only. Purpose This chart is used to determine water saturation Sw in shaly or clean formations when knowledge of the porosity is unavailable.

It may also be used to verify the water saturation determination from another interpretation method. The small chart provides an Sxo correction when Sxo is known.