Abstract:
A seabed region ( 18 ) that lies under a seabed surface area of over one square meter, is analyzed by comparing a core sample taken near the middle of the region and/or data from a geotechnical insitu cone penetrometer installed at the middle of the region, to an acoustic analysis of the region. Locations of the acoustic analysis are precisely correlated to the location of the core test sample or cone test by mounting an acoustic imaging apparatus ( 16 ) that holds acoustic transducers ( 44, 46 ), on a carriage ( 26 ) that is positioned on the core drill ( 12 ) or cone penetrometer barrel staff. The carriage of the acoustic imager apparatus is clamped to the core drill when the core drill is not rotating. An arm ( 30  and/or  32 ) is supported on the carriage through a frame ( 28 ), with at least one acoustic generator ( 44 ) and one acoustic echo detector ( 46 ) mounted on the arm. The arm can be rotated to positions lying about the drill axis ( 14 ) to accurately scan a wide area.

Description:
BACKGROUND OF THE INVENTION 
       [0001]    There are many cases wherein it is necessary to determine the structure of the sea bed in a limited region. One case is where piles are to be driven into the sea bed to support a construction project such as columns of an offshore hydrocarbon loading platform or of various types of structures that are to lie offshore. If the seabed below a certain depth is consolidated (firm and secure) then piles driven therein will remain stationary, while if piles are driven into soft subsea soil then the piles are not as secure and soil strength must be considered. There is also the costly refusal of the pile by the presence of boulders. One way to determine the condition of the sea bed is to produce samples of the sea bed using core drills, which range in diameter between about 5 centimeters (2 inches) and 30 centimeters (12 inches). Another way is to conduct insitu cone tests. In insitu cone tests, a cone containing sensors is driven into the seabed and seabed characteristics at that location are measured. These two methods will sometimes be collectively referred to herein as seabed penetration measurement, by a seabed data penetrator. Since offshore core drilling and insitu cone tests are expensive and difficult to conduct, only a limited number of locations are drilled or interrogated by a cone. This leads to uncertainty about the condition of the sea bed. For example, if the core sample shows rock material extending down from a predetermined depth, there is uncertainty as to whether the rock is bedrock or is part of a boulder, or is part of a discontinuous hard pan layer. 
         [0002]    The seabed can take the form of soft sedimentary lenses, boulders and/or cobble stones, a glacial till (clay, sand, gravel, and boulders intermingled), hard pan (compacted clay soil), mud layers, gas hydrates and gaseous sediments, and frozen soil. Many of these seabed materials are of different conditions when lying in situ (in the sea bed) than when present in a core sample, as where liquid and/or gas escape and/or very fine particulates drop out of the core or the temperature changes. It is possible to analyze the seabed by acoustic (sonar and seismic) apparatus wherein the sound is directed at the sea bed and the echos are detected. The echos indicate the reflectivity, attenuation, back-scatter, and velocities of sound at selected frequencies in the materials, from which the characteristics of the sea bed can be estimated. The interpretation of such acoustic sea bed characteristics is a more reliable presentation of the spatial extend of the layers than from a core sample or insitu core test alone. Acoustic imaging can cover a much wider area and at lower cost. It can also provide for lateral confirmation of the physical core properties. 
       SUMMARY OF THE INVENTION 
       [0003]    In accordance with one embodiment of the present invention, a method and apparatus are provided for imaging a sea bed by imaging it, which enables the more accurate evaluation of a region lying under a seabed surface area of more than one square meter. The method includes the use of a core drill or insitu geotechnical cone to produce detailed information about a small volume of the sea floor. The same core drill or cone is used to support and accurately locate a wide area acoustic imaging apparatus during its movement to obtain acoustic data about a large area of the seabed. The acoustic apparatus includes a clamping carriage that can slide down the shank of the core drill (or cone) and then clamp to the core drill. An arm is supported on a frame that is, in turn, supported on the carriage. The arm extends radially away from the drill and holds at least one set of transducers. These transducers include an acoustic generator that produces acoustic radiation and an acoustic detector that detects acoustic radiation that represents echos from the seabed. 
         [0004]    With the core drill (or cone) lying adjacent to, or preferably against the sea floor, before or after a core sample has been drilled, the acoustic generator on the arm is operated to produce acoustic echos, with the output of the detector recorded. After acoustic readings have been taken at a plurality of locations along the arm, the carriage is rotated around the core drill as in increments of 15°, with acoustic readings taken at each angular position. As a result, a large and more accurate assessment of the sea bed is made, based on both the core sample and the acoustic imaging. A general assessment of the sea bed over the considerable area that has been acoustically imaged, is made more definite by comparing the assessment at areas acoustically similar to where the core sample was taken, to the actual core sample. 
         [0005]    The novel features of the invention are set forth with particularity in the appended claims. The invention will be best understood from the following description when read in conjunction with the accompanying drawings. 
     
    
     
       BRIEF DESCRIPTION OF THE DRAWINGS 
         [0006]      FIG. 1  is a side elevation view of a seabed evaluation apparatus of the invention in an installation configuration, with the arms projecting upward from the clamping carriage. 
           [0007]      FIG. 2  is a side elevation view of the apparatus of  FIG. 1 , with the arms deployed to imaging positions. 
           [0008]      FIG. 3  is a view of a map of the seabed at a particular depth. 
           [0009]      FIG. 4  is an isometric view showing the acoustic characteristics of a seabed at vertically spaced planes, and also showing a drill core. 
       
    
    
     DESCRIPTION OF THE PREFERRED EMBODIMENTS 
       [0010]      FIG. 1  shows a seabed evaluation complex  10  for evaluating a seabed region  18 , which includes a core drill  12  that extends along a primarily vertical axis  14  and an acoustic interrogation apparatus, or acoustic imaging apparatus  16 . The core drill is of the usual type that includes a hollow drilling portion  20  and a shank  22 . The shank is rotated or pounded down by Equipment (not shown) at the sea surface, while the core drill is lowered into the seabed  24  and thereafter pulled up to the surface so a core sample can be recovered. Instead of penetrating the seabed with a core drill, the seabed can be penetrated by an insitu Geotechnical cone, which is a device with sensors that is pounded or otherwise inserted into the seabed. Both devices can be referred to as a seabed data penetrator, which penetrates deep (at least one meter) into the seabed to gather data. The acoustic apparatus  16  of  FIG. 1  includes a clamping carriage  26  that is centered on the drill axis and that can clamp (i.e. fix itself) to the drill. The apparatus also includes a rotatable frame  28  that is rotatable about the carriage. The acoustic apparatus also includes a pair of arms  30 ,  32  that are pivotally connected to the frame at primarily horizontal axes  34 ,  36  that are circumferential to the drill axis. 
         [0011]      FIG. 1 . shows the acoustic imaging apparatus  16  during the course of its installation to allow acoustic reading to be taken. The arms  30 ,  32  have been pivoted up so they extend primarily vertically and parallel to the drill axis to facilitate sliding them down along the drill. With the carriage lower end  38  lying against the sea bed surface  40  ( FIG. 2 ), the arms are pivoted down to the configuration of  FIG. 2 . At least one transducer set  42  which includes an acoustic generator  44  and an acoustic detector  46  is established at a particular position along each arm  30 ,  32 , such as at the radially outer end of each arm. Applicant notes that  FIG. 2  shows two modes for the transmission and reception of acoustic energy. One mode is the use of multiple acoustic detectors  46  whose positions (e.g. fixed on the carriage  26 ) do not change and with applicant repeatedly repositioning only the acoustic generators  44 . In the other mode, co-located transmitter(s) and receptor(s) move along the arm. 
         [0012]    With the acoustic generator  44  at a selected position on the arm, the acoustic generator is energized by electronic signals such as short pulses, to produce acoustic waves that penetrate into the seabed  24 . To penetrate to a depth of up to 10&#39;s of meters, applicant produces acoustic waves of a frequency that is typically 1 KHz to 50 KHz. The acoustic waves generate echos which are detected by the detectors  46 . The times after acoustic transmission when various parts of an echo are detected and the amplitudes of the detected echo parts indicate many characteristics of the seabed. These include the density at various depths (which can indicate rock or soil), and the locations of the top and bottom of boulders (where there are strong reflections) and other materials in the sea bed. The acoustic generator produces a beam that interrogates (produces images of) a tall column-shaped location under the seabed surface. 
         [0013]    Each acoustic generator is repeatedly moved along an arm  30 ,  32  to image many column-like volumes spaced along the arm. After all locations along one arm position are interrogated, the arm is pivoted, as by 15°, about the drill axis  14 . At each rotational position, the seabed is insonified (echos are detected from transmitted sonic pulses) at a plurality of positions of the acoustic generator along each arm. The result is a two-dimensional map such as shown at  50  in  FIG. 3  for each of a plurality of depths under the seabed surface. Each arm  30 ,  32  ( FIG. 2 ) has a length of more than 0.5 meter, so the area of the seabed surface under which the seabed is insonified, is more than one square meter (more than 10 square feet). Preferably, each arm has a length of a plurality of meters, so the area of the seabed under which the seabed is acoustically examined is a plurality of 10&#39;s of square meters. 
         [0014]    In one example, the drill core indicates rock at location  54 , while the map  50  of  FIG. 3  indicates rock at  56  which form boulders because they have small horizontal dimensions. The map  50  indicates a wide expanse of rock at  58  which could be bedrock and which could be further interrogated. Sometimes even the core sample is deceiving as where it contains material that changes state under pressure or contains fluids or has been blocked by large particulates during the sampling.  FIG. 4  shows the physical core  52  which extends about 20 meters below the seabed surface  40 , and shows four acoustic images taken at 5 meter intervals. The acoustic images indicate fine sand at  51 , course sand at  53 , boulders at  56  and fine clay at  55 . 
         [0015]    It is important that the positions of locations on the acoustic examination map  50  be accurately correlated to the position of the core sample(s) at  52  for that volume of the sub-seabed. The correlation should be within an inch (2.5 centimeters) in perpendicular lateral directions, and also be accurate in a vertical direction. The acoustic imaging apparatus  16  shown in the figures enables such close correlation of positions. 
         [0016]    After applicant lowers the drill ( FIG. 1 ) to the seabed (and usually after a core is drilled), applicant positions a passage  29  in the carriage  26  so it receives the drill  12 . Then, applicant lowers the carriage along the drill until the carriage lower end  38  lies against the seabed  24  as in  FIG. 2 . An umbilical  62  extends from a facility at the sea surface down to the carriage. The umbilical is used to lower the carriage until the carriage lower end contacts the sea floor. A cable  64  also extends to the sea surface. A clamp  65  on the carriage is then operated to clamp the carriage to the drill, at the drill shank. The drill  12  preferably lies in contact with the seabed at the walls of a core hole  66  that has been drilled or that is to be drilled, to accurately position the acoustic apparatus with respect to the core hole. With the carriage fully lowered, a winch  68  is operated to lower the arms  30 ,  32  until they are horizontal, as shown in  FIG. 2 . Applicant can use a single arm  30 , or can use two arms to interrogate more rapidly. 
         [0017]    With the arms lowered, the acoustic generators  44  are energized and the echos are detected by the receivers  46 . After each acoustic insonification by detecting the echos, the transducer(s) is moved along the arm  30 ,  32  to a new position. The column-shaped volumes imaged by the transducers  44 ,  46  usually overlap. After sounding a series of volumes lying under the length of the arm, the arm  30 ,  32  is rotated to a new position. Data from the interrogation apparatus is stored in a data file  48  although it can be transmitted to a recorder at the sea surface. An actuator apparatus typically formed by an electric motor  70  with gear set  72  or pneumatic or hydraulic actuator, rotates the frame  28  on which the arms  30 ,  32  are mounted, about the carriage  26  that is, clamped to the drill. Each rotation angle is preferably about 15° and proceeds in typically twelve to twenty-four steps to provide twenty-four angularly spaced arm positions for the two arms. However, if an area of special interest is found (e.g.  58  in  FIG. 3 ) the frame may be rotated in steps of perhaps 1°. 
         [0018]    In a system that applicant has designed, the arms  30 ,  32  each had a length of 7 meters. As a result, a volume of the sea bed was acoustically interrogated which lay under a sea floor area of 68 square meters. The arms were located above the seabed by a distance A of more than a Meter, and actually was about 3 meters above the sea floor, which allowed the pulse initially generated by the generator 44 to produce sound waves of a frequency of 1 KHz to 20 KHz in a broadening beam that passed into the seabed. 
         [0019]    The ability to precisely position the transducers  42 , enables applicant to employ synthetic aperture sonic techniques to augment the analysis of the seabed. In synthetic aperture sonic techniques, applicant, detects and co-locates the phases of returned (reflected and/or refracted) signals, or echos, in addition to their amplitude and time of detection (after transmittal), which enables a more precise analysis of seabed characteristics. 
         [0020]    Thus, the invention provides a method and apparatus for analyzing a seabed volume that lies under an area of more than one square meter of the sea bed surface. The invention involves the penetration of over one meter of the seabed by a seabed data penetrator, and the acoustic imaging, or interrogation, of a volume in the sea bed that lies around the location where the seabed penetration was made to gather data from a hole in the seabed. This allows the evaluation of a large volume of the sea bed, using only one or a limited number of core drillings and/or insitu cones. This is accomplished by using the acoustic interrogation to evaluate the lateral extent of layers in the seabed and by cross-correlating with the core sample and/or data from the cone to check that acoustic iterations between the two sources of information produce a final consistent calibrated interpretation of conditions of the seabed. Accurate information about the location of the core sample with respect to the locations where the acoustic evaluation data were taken, is assured by positioning the acoustic transducer(s) on an apparatus that is mounted on the core drill, with the bottom of the carriage placed in contact with the seabed while the core drill lies in contact with the sea bed at the location where the core was taken or is to be taken. This is accomplished by mounting the transducers on an arm(s) that rotates about the axis of the drill. 
         [0021]    Although particular embodiments of the invention have been described and illustrated herein, it is recognized that modifications and variations may readily occur to those skilled in the art, and consequently, it is intended that the claims be interpreted to cover such modifications and equivalents.