This invention relates to the determination of ion concentrations in downhole water from hydrocarbon wells, aquifers etc. This is useful in a wide range of applications, including predicting the formation of scale and fingerprinting waters from different sources.
The prediction of the location and type of mineral scale that may form around or within the production or surface facilities of an oil well is an important factor both in the design of the well and the formulation of strategies to cope with the mineral scale.
Current methods for predicting mineral scale formation involve the retrieval of samples from downhole, which are then either analyzed at the surface or else sent off to laboratories for analysis. Errors and delays can arise from this ex situ analysis.
Electrochemical methods have previously been developed for the measurement of the concentration of a number of different metal ions, and some have been deployed in shallow boreholes, lakes and ocean waters. However, the application of these methods to oilfield operations has been limited, as the high temperatures (up to 175 Celsius) and pressures (up to 1500 bar) common to most reservoirs, make their use impractical. Furthermore, many electrochemical methods are not able to distinguish between the principal metal ions (Ca2+, Ba2+ and Sr2+} responsible for scale formation. This problem is compounded by the low concentrations of these ions (about 10 s mg/L) in formation water which is often highly saline.
The ability to rapidly and conveniently distinguish scaling ions may also find application, for example, in fingerprinting waters flowing into a hydrocarbon well from different producing zones. This information, which is indicative of connectivity between different zones of a producing well, may allow the optimization of production strategies for recovering the oil in place.
An object of the invention is to provide improved methods for the measurement of the scaling ions, which are suitable for use in situ i.e. in a continuous connection to a flow of fluid.
Accordingly, a first aspect of the invention provides an apparatus for determining the concentration of scaling ions in downhole water; the apparatus comprising a ligand which binds scaling ions from a flowing fluid, which could be downhole water, said ligand having an electronic configuration which is altered on binding of a scaling ion, and a detector for determining alterations in said electronic configuration, the amount of said alterations being indicative of the concentration of the scaling ion in the sample.
Preferably the ligand is contained within an electrochemical cell and changes in the electroactivity of the ligand are determined, for example amperometrically or voltammetrically. In other embodiments, the binding of a scaling ion may alter the fluorescent properties of the ligand. Changes in the fluorescence of the ligand upon binding of the ligand may be determined using any of a range of conventional techniques.
The apparatus may comprise a single ligand which binds specifically to a single scaling ion, such that changes in the electronic configuration of the ligand are directly related to the concentration of the scaling ion in the sample water.
More preferably, the apparatus may contain two or more different ligands, for example three, four, or five or more. Alterations in the electronic configuration of each ligand may be determined independently, either simultaneously or sequentially.
In some embodiments, each ligand may bind specifically to a different scaling ion. Changes in the electronic configuration of each ligand are directly related to the concentration of the corresponding scaling ion in the sample water.
In other embodiments, each ligand may bind to two or more different scaling ions. Changes in the properties (i.e. the electronic configuration) of each ligand are directly related to the concentration in the sample water of the two or more scaling ions to which that ligand binds. The different electronic response of the ligand to different ions can be translated into a respective concentration measurements, for example by locating the peaks in a voltagram.
Alternatively, each ligand may bind to a different combination of scaling ions such that the concentration of each individual scaling ion in the sample water may be calculated from the measurements determined for two or more different ligands.
An advantage of the apparatus is that it allows in situ analysis to be performed, thereby avoiding the problems associated with transporting samples to the surface for ex situ analysis. The present invention is partly based on the realisation that electrochemical techniques can be adapted for performance downhole, i.e. in relatively demanding and hostile conditions.
Preferably the detector is operably connected to a processor for determining the concentration of scaling ions from the current or potential in the cell. In some embodiments, the apparatus is adapted for use downhole (i.e. in a hydrocarbon well or aquifer). The processor may also be adapted for use downhole, or alternatively it may be intended for remote installation e.g. at the surface. For example, the processor may be a suitably programmed computer.
A further aspect of the invention provides for the use of apparatus as described herein for in situ measurement of scaling ion concentration.
In another aspect the invention provides a method of monitoring the concentrations of scaling ions in downhole water comprising;
contacting a sample of downhole water with a ligand which selectively binds scaling ions, wherein the binding of scaling ions in said sample to the ligand alters the electronic configuration of the ligand;
measuring changes in the electronic configuration of the ligand; and,
determining the concentration of said scaling ion from said changes in electronic configuration.
Specific embodiments of the invention will now be described with reference to the following drawings, in which:
In general terms, the present invention relates to the measurement of concentration of ions in downhole water, in particular ions responsible for scale formation by means of changes in the electronic configuration of a ligand which binds scaling ions. A preferred approach involves the use of an electrochemical cell containing a ligand whose electroactivity changes on binding a scaling ion. Changes in ligand electroactivity upon ion binding alter the electrochemical properties of the cell and may be measured using a detector. Other approaches may comprise the use of a ligand whose fluorescent properties change on binding of a scaling ion.
Downhole water may be comprised within a production fluid from a hydrocarbon well or reservoir, which may comprise hydrocarbons, drilling mud etc. The downhole water may, for example, be connate water.
Scaling ions are ions which are responsible for the formation of scale. The principal scaling ions in downhole water are Ca2+, Ba2+ and Sr2+. A suitable ligand may bind selectively to one or more of these scaling ions e.g. a ligand may bind to Ca2+, Ba2+ and Sr2+. Preferably, a ligand shows substantially no binding to other ions.
In some embodiments, the ligand may have a different binding affinity for each of the three principal scaling ions (Ca2+, Ba2+ and Sr2+), allowing the levels of each individual ion in the downhole water to be determined. Discrimination between different ligands may be achieved, for example, by determining the characteristic redox properties of each ligand at different potentials.
The ligand may be present in the cell in an aqueous solution at a concentration of 0.1 to 10 mM, preferably 1 to 10 mM, or may be dispersed within a porous polymer membrane.
Ligands suitable for use in accordance with the invention are stable and able to bind scaling ions under downhole conditions, for example at high temperature (e.g. up to 175° C.) and pressure (e.g. up to 1500 bar).
One class of suitable ligands have the formula (I):
where R1 is a C1-5 alkyl (including, e.g. unsubstituted C1-5alkyl and substituted C1-5 alkyl) or C1-8 aryl (including, e.g. unsubstituted C1-8 aryl and substituted C1-8 aryl); and,
R2 to R9 may independently be H, halogen (F, Cl, Br, I); C1-5 alkyl group; O—C1-5 alkyl group; COOH; NH2; —CONH2; CO—C1-5 alkyl group; or a fluorophore group such as carboxy-X-rhodamine (ROX), tetramethylrhodamine (TAMRA) and fluorescein (FAM).
“C1-5 alkyl” pertains to a monovalent moiety obtained by removing a hydrogen atom from a C1-5 hydrocarbon compound having from 1 to 5 carbon atoms, which may be aliphatic or alicyclic, or a combination thereof, and which may be saturated, partially unsaturated, or fully unsaturated.
Examples of suitable ligands according to formula I are shown in
In some embodiments, the aromatic rings of suitable ligands may comprise substitutions in the ortho, meta or para positions (i.e. at one or more of positions R2 to R9), in order to shift the redox features of a ligand to allow scanning for the different ions in well-separated spectral windows, in order to prevent interference.
For the purpose of this invention the above class of ligands are referred to as O,O′-Bis(2-aminophenyl)ethyleneglycol-N,N,N′,N′-tetraacetic acid or BAPTA derivatives.
Other suitable ligands may include cryptands (Lehn & Sauvage (1975) J. Am. Chem. Soc. 97 23 6700), for example a ligand shown in
A further ligand of the cryptand family is shown in
For the purpose of this invention, ligands of the type of
The apparatus may further comprise a porous membrane or porous electrode block which allows ions within the downhole water to pass into the cell to contact the ligand. A suitable porous membrane may be made of zeolite or a ceramic material. A block may be made of epoxy material as base material.
The membrane may be contacted with discrete samples or batches of downhole water or the membrane may be contacted with a continuous flow of downhole water.
The apparatus may comprise one or more liquid guidance channels to direct downhole water to the membrane and to remove downhole water after contact with the membrane.
The detector may comprise one or more electrodes which contact the ligand. Various arrangements of electrodes may be used as is conventional in electrochemistry.
Conveniently a three-electrode arrangement consisting of a working electrode, a reference electrode and a counter electrode may be used. Preferably, the working electrode is composed of a material resistant to fouling, such as boron-doped diamond or glassy carbon, the counter electrode is platinum and the reference electrode is Ag/AgCl. Other suitable electrode materials, such as AgI, are known to those skilled in the art.
The electrodes may be used to detect changes in the electroactivity of the one or more ligands. For example, electroactivity changes caused by the presence of scaling ions may alter the current flow or voltage between electrodes. Current or voltage may be detected or measured by the detector. For example, the potential of the electrodes may be varied and the current measured or vice versa. The current or potential difference associated with the electroactivity of each of the one or more ligands may be measured by the detector and correlated with the concentration of scaling ions in the downhole water sample. In the presence of the target ions, the peak current(s) should increase, proportional to the concentration of the target species. A power source may be connected to the electrodes to drive the current between the electrodes. The power source may be an integral part of the apparatus, and, for example, may be comprised within the detector. In other embodiments, the power source may be separate from the apparatus and connectable thereto. The apparatus may comprise appropriate circuitry for connection to the power source.
The ligand may be contained within the apparatus in any of a number of ways. In some embodiments, the ligand may be dispersed in an aqueous solution within a chamber of the apparatus. In other embodiments, the ligand may be dispersed within a porous polymer membrane. Binding of the scaling ions by the ligand occurs within the pores of the membrane and resultant changes in current or potential are detected by circuitry connected directly to the membrane via the working, counter and reference electrodes. The use of a porous membrane is convenient in allowing the miniaturisation of the voltammetric or amperometric sensor, thus leading to faster response times, lower consumption of reagents and lower unit costs.
In other embodiments, the ligands may be attached to conducting solid particles, such as carbon or a metal (e.g., gold), which are incorporated into the surface of one or more of the electrodes, preferably, the working electrode. The accumulation of particles with attached ligand forms a conducting porous electrode with ligand attached to the walls of the pores. Suitable techniques for fixing the particles to the electrode surface include epoxy resin adhesion or abrasive immobilisation. A porous electrode for hydrogen sulfide determination, for example, is described in co-pending published United Kingdom application GB-A-2391314.
For example, the ligand (I) above may be designed such that group R8 is an amine (—NH2), which can be reacted with nitrous acid to form the diazonium ion —N+≡N and subsequently coupled to carbon particles by reduction of the diazonium group by hypophosphorous acid. The ligand is thus chemically bonded to the carbon particles and these can be incorporated into the working electrode 4 as described above. In other embodiments, the ligand (I) above may be coupled to gold particles with one of the groups R2 to R9 being either an amine (—NH2) or a thiol (—SH).
As described above, the detector may be operably connected to a processor that determines the concentration of scaling ions in the sample from the current or potential difference measured by the detector. The processor may be separate from or part of the detector. The processor may also be adapted for use under downhole conditions (i.e. high temperature, high pressure and high salinity). Alternatively, it may be intended for remote installation e.g. at the surface. For example, the processor may be a suitably programmed computer.
The measurement of scaling ion concentrations as described herein may be useful in downhole sampling, production logging to characterize flow into the well, and thereby aid remediation or production strategies, and in permanent monitoring applications, where the build up of scale or water breakthrough/flooding of the reservoir might be gauged.
In the variant of
In an example according to an embodiment of the invention, the four ligands (2A-2D) shown in
These ligands have different binding properties; ligand 2A binds Ca2+, Sr2+ and Ba2+; ligand 2B binds Ca2+ and Sr2+, ligand 2C binds Sr2+ and Ba2+ and ligand 2D binds Ba2+.
The level of Sr2+ in the sample water may be determined, for example, by measuring the alterations of the electroactivities of ligands 2C and 2D in the cell and then subtracting the value obtained for ligand 2D from value obtained for ligand 2C, to provide a value which represents the concentration of Sr2+. (i.e. 2C−2D=[Sr2+]). As above the figure label is taken as a representative of the respective ligand and/or the concentration measurement associated with it.
The level of Ca2+ in the sample water may be determined by measuring the alterations of the electroactivities of ligands 2B, 2C and 2D in the cell. The values for ligands 2B and 2D are added together and the value obtained for ligand 2C is subtracted from this combined figure, to provide a value which represents the concentration of Ca2+. (i.e. 2B+2D−2C=[Ca++]).
The level of Ba2+ in the sample water is determined by measuring the alterations of the electroactivities of ligands 2A and 2B in the cell and then subtracting the value obtained for ligand 2B from the value obtained for ligand 2A, to provide a value which represents the concentration of Ba2+. (i.e. 2A−2B=[Ba2+] or ligand 2D).
The chemical structure of further examples of ligands are shown in
In
The flowchart of
An application of the sensor is illustrated in
The flowmeter consists essentially of a constriction or throat 814 and two pressure taps 818, 819 located conventionally at the entrance and the position of maximum constriction, respectively. Usually the Venturi flowmeter is combined with a densiometer 815 located further up- or downstream.
The novel scale sensor 816 is preferably located downstream from the Venturi to take advantage of the mixing effect the Venturi has on the flow. A recess 817 protected by a metal mesh provides an inlet to the unit.
During production wellbore fluid enters the recess 817 and is subsequently analyzed using sensor unit 816. The results are transmitted from the data acquisition unit to the surface via wires 813.
While the invention has been described in conjunction with the exemplary embodiments described above, many equivalent modifications and variations will be apparent to those skilled in the art when given this disclosure. Accordingly, the exemplary embodiments of the invention set forth above are considered to be illustrative and not limiting. Various changes to the described embodiments may be made without departing from the spirit and scope of the invention.
Number | Date | Country | Kind |
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0317260.8 | Jul 2003 | GB | national |
This application is a continuation of U.S. application Ser. No. 10/564,939, filed 17 Jul. 2006, entitled “Apparatus and Method for Measuring Concentrations of Scale-Forming Ions” which is incorporated herein by reference and which was based on PCT application PCT/GB2004/003040, filed 12 Jul. 2004, entitled “Apparatus and Method for Measuring Concentrations of Scale-Forming Ions”. This application claims priority under 35 U.S.C. 119 from Great Britain Patent No. 2404252, filed 24 Jul. 2003, entitled “Measuring concentrations of ions in downhole water”.
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Number | Date | Country | |
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20100255587 A1 | Oct 2010 | US |
Number | Date | Country | |
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Parent | 10564939 | US | |
Child | 12820363 | US |