Please note that there was an error in the initial proposal: samples should be nominally 1 inch in diameter (see below).

Similar documents
FPG8601 Force Balanced Piston Gauge

Gerald D. Anderson. Education Technical Specialist

BULK SPECIFIC GRAVITY AND UNIT WEIGHT OF COMPACTED HOT MIX ASPHALT (HMA) (Kansas Test Method KT-15)

ASSIGNMENT 2 CHE 3473

ASSIGNMENT 2 CHE 3473

INTRODUCTION Porosity, permeability, and pore size distribution are three closely related concepts important to filter design and filter performance.

PMI Advanced Automated. Pulse Decay Permeameter APDP-10K-HP-101. Not just products... Solutions!

PETROLEUM ENGINEERING 310 SECOND EXAM. October 23, 2002

CORESTA RECOMMENDED METHOD N 6

AN EXPERIMENTAL STUDY OF IRREDUCIBLE WATER SATURATION ESTABILISHMENT

SPECIFICATION FOR REPEATED LOAD TRIAXIAL (RLT) TESTING FOR PAVEMENT MATERIALS

Permeability. Darcy's Law

7250 Sys. Ruska Multi-Range Pressure Calibration System. GE Sensing & Inspection Technologies. Features. Applications

Predicted Dispense Volume vs. Gravimetric Measurement for the MICROLAB 600. November 2010

Succeeding with Production Air Leak Testing Methods. Paul Chamberlain President, CEO

LOW PRESSURE EFFUSION OF GASES revised by Igor Bolotin 03/05/12

SIMULATION OF CORE LIFTING PROCESS FOR LOST GAS CALCULATION IN SHALE RESERVOIRS

OHD L-44 METHOD OF TEST FOR MEASUREMENT OF WATER PERMEABILITY OF COMPACTED PAVING MIXTURES

OHD L-44 METHOD OF TEST FOR MEASUREMENT OF WATER PERMEABILITY OF COMPACTED PAVING MIXTURES

Evaluation of CO2 storage actuarial risk: defining an evidence base

LOW PRESSURE EFFUSION OF GASES adapted by Luke Hanley and Mike Trenary

P Oskarshamn site investigation. Borehole: KAV01 Results of tilt testing. Panayiotis Chryssanthakis Norwegian Geotechnical Institute, Oslo

Series 7250 Ruska High-Speed Digital Pressure Controller. GE Sensing. Features

Technical Information Conducal CLY421

ASPHALT PLANT LEVEL 1

Pressure Measurement

Flow in Porous Media. Module 1.c Fundamental Properties of Porous Media Shahab Gerami

THREE-PHASE UNSTEADY-STATE RELATIVE PERMEABILITY MEASUREMENTS IN CONSOLIDATED CORES USING THREE IMMISCIBLE LIQUIDS

Air Pycnometer. Operating Manual. Umwelt-Geräte-Technik GmbH

Chapter Pipette service & maintenance. Pipette specifications according to ISO Repair in the lab or return for service?

Hardware Triaxial and Consolidation Testing Systems Pressure Measurement and Control

Application Worksheet

(a) Deflection to the left, slower velocity means greater deflection, greatest deflection at the south pole

Department of Civil & Geological Engineering GEOE Engineering Geology

Lab #1 Pressure: Bubblers and Water Balloons CEE 331 Fall 2003

S.A. Klein and G.F. Nellis Cambridge University Press, 2011

Application Note AN-107

Gas injection in a water saturated porous medium: effect of capillarity, buoyancy, and viscosity ratio

Unsaturated Testing of Soil (UNSAT)

Florida Method of Test for MEASUREMENT OF WATER PERMEABILITY OF COMPACTED ASPHALT PAVING MIXTURES

OP CHECKLIST FOR 1D CONSOLIDATION LABORATORY TEST

Lab 1: Pressure and surface tension. Bubblers, gravity and the mighty paper clip.

IN-PLACE DENSITY WAQTC FOP AASHTO T 209 (16)

Petroleum Reservoir Rock and Fluid Properties

Determination of Capillary pressure & relative permeability curves

Gas flow calibrations performed at the National Metrology Institute of South Africa (NMISA)

Soil water retention determination using the Wetlab facility at CSIRO, Davies Laboratory

Specific Accreditation Criteria Calibration ISO IEC Annex. Mass and related quantities

CHAPTER 2. Initial Experimental Testing Program

Analysis of dilatometer test in calibration chamber

INTERACTION BETWEEN WIND-DRIVEN AND BUOYANCY-DRIVEN NATURAL VENTILATION Bo Wang, Foster and Partners, London, UK

GP1 & GP2. Electropneumatic Regulators FOR PRESSURE CONTROL TO 1,000 PSI

Test Method of Trap Performance for Induced Siphonage

Guideline for RMO Key comparison for Air kerma rate in 60 Co gamma radiation

Aug 17, 2001 LAB MANUAL MAXIMUM SPECIFIC GRAVITY (RICE VOIDS TEST) OF PAVING MIXTURES AASHTO Designation T 209 (Mn/DOT Modified))

Design, Static Structural & Model Analysis of Water Ring Vacuum Pump Impeller

Certification of AMS acc. EN 15267, Part 3 - Overview and First Experience -

VITLAB Volumetric instruments

MODELLING OF FUME EXTRACTORS C. R.

Integrity Testing LifeASSURE BNA045 and BNA065 Series Filter Cartridges

Accurate Measurement of Steam Flow Properties

ASPHALT WAQTC FOP AASHTO T 209 (12)

Integrity Testing LifeASSURE BDA020, BGA020 and BNA020 Series Filter Cartridges

Paper 2.2. Operation of Ultrasonic Flow Meters at Conditions Different Than Their Calibration

CASE STUDY. Elvington To Brayton Barff Air valve replacement Program

Modern Perforating Techniques: Key to Unlocking Reservoir Potential

U S F O S B u o y a n c y And Hydrodynamic M a s s

Brent Sleep, Magdalena Krol, University of Toronto Kevin Mumford, Queen s University Richard Johnson, Oregon Health and Science University

Soil Water Characteristic Curve (SWCC) Using the WP4C

Digiquartz Water-Balanced Pressure Sensors for AUV, ROV, and other Moving Underwater Applications

Theory of a vertically loaded Suction Pile in CLAY

Development of a Shock Loading Simulation Facility

Lab 3 Introduction to Quantitative Analysis: Pumps and Measurements of Flow

Offshore platforms survivability to underwater explosions: part I

Analogue and Digital Mass Flow Meters and Controllers for Gases MASS-STREAM

COMPUTATIONAL FLOW MODEL OF WESTFALL'S LEADING TAB FLOW CONDITIONER AGM-09-R-08 Rev. B. By Kimbal A. Hall, PE

Level MEASUREMENT 1/2016

Flow in a shock tube

NMISA NEW GAS FLOW CALIBRATION FACILITY. Deona Jonker 7 October 2013

Cover Page for Lab Report Group Portion. Head Losses in Pipes

Cover Page for Lab Report Group Portion. Pump Performance

Appendix A Preliminary SEMs

Pressure Measurements

P-04 Stainless Steel Corrugated Hoses and Metal Bellows Expansion Joints

Organisation Internationale de Métrologie Légale

Technical Report. Comparison of Ventilation Standard Calibration Methods

POROMETER 3G POROMETER. through-pore size analyzer. Membranes. Filters. Non-Woven. Textiles. Papers. Ceramics. Sintered Metals SERIES

EVALUATION OF WATER SATURATION FROM RESISTIVITY IN A CARBONATE FIELD. FROM LABORATORY TO LOGS.

SPIRIT III Radiometer Saturation Effect

Prof. B V S Viswanadham, Department of Civil Engineering, IIT Bombay

Method of Determining the Threshold Pressure Gradient

Tips for Proper Pipette handling and Maintenance. D. Muruganand, Ph.D ILQA - Bangalore, Feb 2014

NMISA New Gas Flow Calibration Facility

Validation of Custody Transfer Metering Skid at Site After Laboratory Proving

PERFORMANCE SPECIFICATION SHEET MICROPHONE ASSEMBLY, M-169A/AIC

Gas Flow Calibration Basics

Technical Datasheet ZHA Series Gear Flow Meters Aluminum Version with ball bearing for lubricating media

Commercial Practice Test Method Internal Vapor Analysis of Hermetic Devices

Low Profile Load Cells

COPYRIGHT. Reservoir Fluid Core. Single Phase, Single Component Systems. By the end of this lesson, you will be able to:

Transcription:

Test schedule for Inter-lab testing Perm/Strength/Vel... October 9, 2008 from David Lockner <dlockner@usgs.gov> Dear colleagues, Here is the revised protocol for Inter-lab testing of Strength/Permeability/Wave Speed/Resistivity/Conductivity. Thank you all for your input in preparing this test procedure. Unless any new questions arise, we should conduct our first round of test in accordance with the following descriptions. Please note that there was an error in the initial proposal: samples should be nominally 1 inch in diameter (see below). Also, for thermal conductivity tests, we will only measure water-saturated samples (no dry tests). Please contact me if you have further questions. regards, David page 1

1) General comments for all tests 1.1) Please provide a brief description of how calibrations of pressures, displacements, etc. are carried out and how these can be traceable, for example, to NIST (in USA) or some equivalent agency. 1.2) If appropriate, a description of corrections should be provided. For example, in our high temperature friction test, Cu jackets have measurable shear strength that must be corrected for. Seal friction, when using an external load cell, is another example. 1.3) Estimates of uncertainties should be provided for all measurements. This will be useful when we compare results from different labs and different techniques. 1.4) Time history of stresses, displacements and related parameters should be recorded as appropriate for the types of measurement performed. We will decide at a later time how these will be included in final results. 1.5) Basic information should be recorded for all samples including: dimensions mass dry bulk density Basic determination of connected porosity should be performed on some portion of the samples (e.g., submerged, saturated weight test). 1.6) Samples should be preserved in case follow-up tests (i.e., thin section work) are wanted. 1.7) Note. Sample types can be identified as follows: Crab Orchard sandstone fine-grained, banded, 5% nominal porosity Berea sandstone lightly banded, 20% nominal porosity Wilkeson sandstone (to be delivered) medium grain size, 10% nominal porosity Carrera marble marble Sierra white granite medium-grained granite (to be delivered) page 2

2) Strength Tests Eight samples of each rock type should be prepared (cored parallel to up/down direction). Nominal sample dimensions: right cylinders, 2.5 inches long x 1.0 inch diameter. [This is our standard dimension. Other sample diameters are acceptable, i.e., 30 mm or 40 mm. An aspect ratio of 2.5:1 is preferred. Aspect ratio should be greater than 2.0:1.] 2.1) Crab Orchard sandstone: (DRY tests) Vacuum dry samples for 24 hr at 60 C (or 48 hr at room temperature). Run all tests room-dry that is, equilibrated with relative humidity in laboratory. Perform constant strain rate tests at 10-5 sec -1 axial shortening rate. (For example, this would be 0.635 micron/sec for a sample length of 2.5 inches.) Determine peak strength and (if possible) residual friction. One test each at constant confining pressures of: 0, 10, 20, 50, 150 MPa 3 repeat tests at constant confining pressure of 100 MPa 2.2) Carrera marble: (DRY tests) Same sequence as Crab Orchard 2.3) Sierra granite: (DRY tests) Vacuum dry samples for 24 hr at 60 C (or 48 hr at room temperature). Run all tests room-dry. Perform constant strain rate tests at 10-5 sec -1 axial shortening rate. (For example, this would be 0.635 micron/sec for a sample length of 2.5 inches.) Determine peak strength and(if possible) residual friction. One test each at constant confining pressures of: 0, 20, 60 MPa 5 repeat tests at constant confining pressure of 40 MPa 2.4) Berea sandstone: (WET tests) Vacuum dry samples for 24 hr at 60 C (or 48 hr at room temperature). Saturate with distilled water Perform constant strain rate tests at 10-5 sec -1 axial shortening rate. (For example, this would be 0.635 micron/sec for a sample length of 2.5 inches.) Determine peak strength and possibly residual friction. Record volume change during deformation (if possible). Run all tests at constant pore pressure of 2 MPa. One test each at constant confining pressures of: 12, 22, 52, 152 MP 3 repeat tests at constant confining pressure of 102 MPa 2.5) Wilkeson sandstone: (WET tests) Same sequence as Berea page 3

3) Permeability Tests propose testing of only 1 or 2 samples for each rock type. Nominal sample dimensions: right cylinders, 1.969 inches long x 1.0 inch diameter. [Use different diameter samples if necessary; i.e. 30 mm or 40 mm]. Please prepare standardized sample lengths of 50 mm (1.969 inch) for all tests, regardless of sample diameter. 3.1) Note: Particularly for oscillating flow measurements, there is an optimum range of permeability/sample length/reservoir volume/oscillation frequency. Those of you who have performed these measurements are, no doubt, aware of these constraints. In the Fisher and Paterson (1992) notation, γ represents the ratio: (down-stream reservoir storage capacity)/(sample storage capacity). For best results, design the down-stream reservoir for γ between 1 and 100. Then, for optimum sensitivity in the inversion, oscillation period should be chosen to provide ψ in the range between 1 and 3 again, see Fisher and Paterson (1992). Pore pressure drop across the sample should be limited to a maximum of ±5 MPa. 3.2) Crab Orchard, Berea, Wilkeson, Sierra granite: (use distilled water) Fully saturate samples in the following manner: (i) Vacuum dry for 24 hr at 60 C(or 48 hr at room temperature). (ii) Introduce water into sample while still in vacuum chamber. [There are different ways to do this. The point is to avoid trapping air in the sample; especially in low-porosity samples.] Evacuate to remove stray air bubbles and fill pore pressure system with water. Tests should be run at nominal pore pressure of 10 MPa. For steady flow tests, high-side and low-side pore pressure should be chosen to provide average pore pressure of 10 MPa. (If this is not practical, then downstream side of sample can be vented to atmosphere.) Care should be taken to avoid over-pressuring sample prior to permeability test to avoid complications from hysteresis of permeability. Measure permeability in the following sequence of effective confining pressure: 10, 30, 60, 100, 30, 60, 100, 30, 60, 100 MPa page 4

4) Ultrasonic Velocity Tests Note: This should be about the same procedure as will be used in permeability tests. propose testing of only 1 or 2 samples for each rock type. Nominal sample dimensions: right cylinders, 1.969 inches long x 1.0 inch diameter. [This is our standard dimension. If this presents problems for you, go ahead and use your own sample configurations. Use the 1.969 inch (50 mm) length if at all possible.] Keep track of NS and EW orientations. 4.1) Crab Orchard, Sierra granite, Carrera marble: DRY tests Vacuum dry for 24 hr at 60 C (48 hr at room temperature). Conduct tests on room-dry samples (that is, samples equilibrated with relative humidity of laboratory). Confining pressure only; no differential stress. Measure shear wave speed polarized in NS direction. Measure P and S in the following sequence of confining pressure: 5, 10, 30, 60, 100, 30, 60, 100, 30, 60, 100 MPa 4.2) Berea: WET tests (use distilled water) Fully saturate samples: Vacuum dry for 24 hr at 60 C (48 hr at room temperature). Introduce water into sample while still in vacuum chamber. [There are different ways to do this. The point is to avoid trapping air in the sample; especially in low-porosity samples.] Evacuate to remove stray air bubbles and fill pore pressure system with water. Pore pressure can be vented to atmosphere. Care should be taken to avoid over-pressuring sample prior to each velocity test to avoid complications from hysteresis. Measure shear wave speed in NS orientation Measure velocities in the following sequence of effective confining pressure: 5, 10, 30, 60, 100, 30, 60, 100, 30, 60, 100 MPa page 5

5) Electrical Conductivity Tests propose testing of only 1 sample for each rock type. Nominal sample dimensions: right cylinders, 1.969 inches long x1.0 inch diameter. [This is our standard dimension. If this presents problems for you, go ahead and use your own sample dimensions.] 5.1) Crab Orchard, Berea, Wilkeson, Sierra granite: (use 0.1 molar KCl aqeous ) Fully saturate samples: Vacuum dry for 24 hr at 60 C (48 hr at room temperature). Introduce brine into sample while still in vacuum chamber. [There are different ways to do this. The point is to avoid trapping air in the sample; especially in low-porosity samples.] Evacuate to remove stray air bubbles and fill pore pressure system with brine. Flush equivalent of 1 pore volume of brine through sample. Pore pressure lines can be vented to atmosphere during tests. Care should be taken to avoid over-pressuring sample prior to test at each confining pressure to avoid complications from hysteresis. Run test at 100 Hz to avoid electrode polarization. RECORD SAMPLE TEMPERATURE FOR EACH TEST Report results as conductivity and formation factor Measure conductivity in the following sequence of effective confining pressure: 5, 10, 30, 60, 100, 30, 60, 100, 30, 60, 100 MPa page 6

6) Thermal Conductivity Tests propose testing of only 1 sample for each rock type. Nominal sample dimensions: right cylinders, 1.0 inch long x 1.0 inch diameter. [You should use sample dimensions that are appropriate to your test configuration.] 6.1) Crab Orchard, Berea, Wilkeson, Sierra granite: WET tests (use distilled water) Fully saturate samples as described: Vacuum dry for 24 hr at 60 C (48 hr at room temperature). Introduce water into sample while still in vacuum chamber. [There are different ways to do this. The point is to avoid trapping air in the sample; especially in low-porosity samples.] Perform bench-top test if appropriate Evacuate if needed to remove stray air bubbles and fill pore pressure system with water. Pore pressure lines can be vented to atmosphere during tests. Care should be taken to avoid over-pressuring sample prior to test at each confining pressure to avoid complications from hysteresis. Measure conductivity in the following sequence of effective confining pressure: 10, 40, 100, 10, 40, 100 MPa page 7