Причина отмены This test method covers a field procedure for determining the transmissivity and storativity of geological formations having permeabilities lower than 10⁻³ μm² (1 millidarcy) using the pressure pulse technique.

Formerly under the jurisdiction of Committee D18 on Soil and Rock, this test method was withdrawn in January 2017 in accordance with section 10.6.3 of the Regulations Governing ASTM Technical Committees, which requires that standards shall be updated by the end of the eighth year since the last approval date.

Значение и использование

Test Method—The pulse test method is used to determine the transmissivity and storativity of low-permeability formations surrounding the packed-off intervals. This test method is considerably shorter in duration than the pump and slug tests used in more permeable rocks. To obtain results to the desired accuracy, pump and slug tests in low-permeability formations are too time consuming, as indicated in Fig. 1 (from Bredehoeft and Papadopulos (1)).

Analysis—The transient pressure data obtained using the suggested method are evaluated by the curve-matching technique described by Bredehoeft and Papadopulos (1), or by an analytical technique proposed by Wang et al (2). The latter is particularly useful for interpreting pulse tests when only the early-time transient pressure decay data are available.

Units:

Conversions—The permeability of a formation is often expressed in terms of the unit darcy. A porous medium has a permeability of 1 darcy when a fluid of viscosity 1 cP (1 mPa·s) flows through it at a rate of 1 cm³/s (10⁻⁶ m ³/s)/1 cm² (10⁻⁴ m²) cross-sectional area at a pressure differential of 1 atm (101.4 kPa)/1 cm (10 mm) of length. One darcy corresponds to 0.987 μm². For water as the flowing fluid at 20°C, a hydraulic conductivity of 9.66 μm/s corresponds to a permeability of 1 darcy.

Viscosity of Water—Table 1 shows the viscosity of water as a function of temperature.

TABLE 1 Viscosity of Water as a Function of Temperature

Temperature, °CAbsolute Viscosity, mPa·s 01.79 21.67 41.57 61.47 81.39 10 1.31 12 1.24 14 1.17 16 1.11 18 1.06 20 1.00 22 0.96 24 0.91 26 0.87 28 0.84 30 0.80 32 0.77 34 0.74 36 0.71 38 0.68 40 0.66 Область применения

1.1 This test method covers a field procedure for determining the transmissivity and storativity of geological formations having permeabilities lower than 10⁻³ μm² (1 millidarcy) using the pressure pulse technique.

1.2 The transmissivity and storativity values determined by this test method provide a good approximation of the capacity of the zone of interest to transmit water, if the test intervals are representative of the entire zone and the surrounding rock is fully water saturated.

1.3 The values stated in SI units are to be regarded as the standard. The values in parentheses are for information only.

1.4 This standard does not purport to address all of the safety concerns, if any, associated with its use. It is the responsibility of the user of this standard to establish appropriate safety and health practices and determine the applicability of regulatory limitations prior to use.