Measuring and testing – Borehole or drilling – Fluid flow measuring or fluid analysis
Reexamination Certificate
2000-11-27
2002-08-20
Williams, Hezron (Department: 2856)
Measuring and testing
Borehole or drilling
Fluid flow measuring or fluid analysis
Reexamination Certificate
active
06435021
ABSTRACT:
The present invention relates to a process for verifying the effectiveness of drilling fluids in stabilizing oil well walls, by measuring the ultrasonic wave transmission velocity on clay cuttings subjected to aging in drilling fluids.
During drilling of an oil well, there is often the problem of instability of the well in shale formations. To prevent this instability, drilling fluids are prepared with additives suitable for inhibiting shale swelling.
The effectiveness of these additives is evaluated by tests which are specified in API procedures, for example, dispersion tests of clay cuttings in mud (hot-rolling test) or laboratory procedures (for example measuring the swelling of clay samples).
None of these techniques used in the prior art takes into account the mechanical characterization of the shale, one of the main factors in determining the effect of the drilling fluid on the stability of the well walls.
On the other hand, techniques for evaluating the mechanical characteristics (for example uniaxial, triaxial, indentation tests) have the great disadvantage of being destructive, costly and time-consuming.
It is also known that the related mechanical properties can be discovered from measuring the velocity of sound waves through rock samples. Although these acoustic techniques are not destructive, they have the drawback of being used at present only for the acoustic characterization of formations that gives the mechanical properties of the rock. They neglect, on the other hand, the effect due to rock-drilling fluid interaction.
A process has now been found which overcomes the above disadvantages as it allows the mechanical properties of shales to be evaluated in the presence of drilling fluids. The process of the present invention also has the advantage of not being destructive.
In accordance with this, the present invention relates to a process for measuring the effects on the mechanical properties of shales due to interaction with drilling fluids, which comprises:
(a) preparation of a shale sample having at least two flat, parallel opposite surfaces;
(b) measurement of the transmission velocity of ultrasonic waves through the sample of step (a),
(c) preparation of a mixture of water-or oil-based drilling fluid and the shale sample (a);
(d) removal, after a pre-established time, of the shale sample (a) from the mixture (c) and measurement of the ultrasonic wave transmission velocity through the sample thus removed;
(e) comparison between the measurements of step (d) and those of step (b).
The process of the present invention can be applied to cuttings produced during drilling, or to samples prepared from outcrop shale or cores.
Alternatively, it is possible to operate on reconstituted shale samples.
When cuttings produced during drilling are used, owing to their irregular geometry, they must be subjected to smoothing or grinding until two flat, parallel surfaces are obtained. This can be achieved by smoothing each cutting by means of diamond sandpaper disks lubricated with oil or demineralized water, until two flat, parallel surfaces are obtained.
Step (a) of the process of the present invention consists in the preparation of shale. This is done preparing suitably-sized (at least 2 mm thick) test-samples. When cuttings are used, these can either derive from wells or be prepared from cores (well or quarry). The sample preparation is normally carried out with an automatic slitter in demineralized water or oil to obtain the desired test-samples, which must have at least two flat, parallel surfaces. Samples that have cracks are discharged. It is essential for them not to be exposed to the air as the response of the sample greatly depends on the degree of saturation.
Step (b) consists in measuring the sound wave transmission velocity through the shale sample. The test consists in generating an ultrasonic pulse by means of an emitter transducer (connected to a function generator) onto a surface of the sample and recording, by means of an oscilloscope (connected to a receiver transducer), the transit time t of said pulse through the sample. If the thickness of the sample L is known, the sound disturbance velocity is given by the ratio V=L/t.
The fact of generating compressional or shear waves is related to the particular type of transducers used; in particular a pair of transducers (emitter and receiver) is used for compressional waves and a pair of transducers (emitter and receiver) for shear waves. The ultrasonic wave passes through the sample and is converted to an electric signal by the receiver transducer; the electric signal received is then visualized by means of a digital oscilloscope which, taking into account the delay due to the transducers and circuit, enables the transit time of the ultrasonic pulse through the cutting to be determined.
If the thickness of the cutting is known, it is thus possible to determine the transmission velocity of the compressional or shear ultrasonic waves.
The water-or oil-based drilling fluids used in step (c) are well-known to experts in the field (see for example Gray G. R. and Darley H. C. H.: “Composition and properties of oil well drilling fluids”; Gulf Publishing Company, fourth edition, Houston Tex. U.S.A., 1980).
Step (c) consists in the preparation of the mixture of shale (a) and drilling fluid. This mixture, preferably prepared by pouring the shale (a) into the drilling fluid, is brought at the desired temperature, indicatively from 10° C. to 200° C., preferably from 20° C. to 150° C. The mixture thus prepared is left to age either under static conditions or under stirring.
After a pre-established time, shale samples are removed from the shale/drilling fluid mixture (step d). Measurements of the compressional and shear wave velocity through the cutting are then taken, care being taken not to let it dry. The procedure is identical to that of step (b). In order to allow acoustic coupling, however, a particular coupling fluid is inserted between transducers and sample. These fluids preferably have viscosity values ranging from 200 to 800 poises measured with a shear velocity gradient of 3.1 s
−1
(Standard American Petroleum Institute 13 B-1).
The above technique, also known as “pulse velocity” can be used on cores (for example cylindrical rock samples having a diameter of 2.5 cm and double the height), but also on rock fragments with dimensions of less than a centimeter which reach the surface during drilling.
The experimental apparatus generally consists of (a) a pulse generator with a duration time varying from 1 &mgr;s to 20 &mgr;s; (b) a pair of piezoelectric transducers capable of generating compressional ultrasonic waves, highly damped and with a 100% band width or, alternatively, a pair of piezoelectric transducers capable of generating shear ultrasonic waves, highly damped and with a 100% band width; (c) a digital oscilloscope with a minimum resolution of 10
−2
&mgr;s.
In particular, it is known that the compressional wave velocity V
p
through a material is directly proportional to the Lamè &lgr; constant and shear modulus G and inversely proportional to the density of the material &rgr;, according to the equation: V
p
=(80+2G)/&rgr;.
Analogously, it is known that the shear wave velocity V
s
is directly proportional to the shear modulus G and inversely proportional to the density of the material &rgr;, according to the equation: V
s
=G/&rgr;.
In addition, it is known that the Lame &lgr; constant is in relation to the bulk modulus of elasticity K of a material by means of the equation &lgr;=K−2·G/3.
The bulk modulus K is also intended as the inverse of the compressibility, as a result of which an analysis of the ultrasonic wave transmission velocity through a shale sample makes it possible to determine the effects due to interaction with a fluid on the mechanical properties (compressibility, shear modulus) and on the density of the material. These properties are in fact key parameters which indicate the capacity of a shale formation of not generating instability phen
Carminati Stefano
Gaudio Lucilla Del
Marsala Alberto
ENI S.p.A.
Oblon & Spivak, McClelland, Maier & Neustadt P.C.
Politzer Jay L
Williams Hezron
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