PASSIVE IMAGING OF HYDROFRACTURES IN THE SOUTH BELRIDGE DIATOMITE

We present the results of a seismic analysis of two hydrofractures spa nning the entire diatomite column(1110-1910 ft or 338-582 m) in Shell' s Phase II steamdrive pilot in South Belridge, California, These hydro fractures were induced at two depths (1110-1460 and 1560-1910 ft) and imaged passively using the seismic energy released during fracturing. The arrivals of shear waves from the cracking rock (''microseismic eve nts'') were recorded at a 1 ms sampling rate by 56 geophones in three remote observation wells, resulting in 10GB of raw data. These arrival times were then inverted for the event locations, from which the hydr ofracture geometry was inferred. A five-dimensional conjugate-gradient algorithm with a depth-dependent, but otherwise constant shear wave v elocity model (CVM) was developed for the inversions. To validate CVM, we coated a layered shear wave velocity model of the formation and us ed it to calculate synthetic arrival times from known locations chosen at various depths along the estimated fracture plane. These arrival t imes were then inverted with CVM and the calculated locations compared with the known ones, quantifying the systematic error associated with the assumption of constant shear wave velocity. We also performed Mon te Carlo sensitivity analyses on the synthetic arrival times to accoun t for all other random errors that exist in field data. After determin ing the limitations of the inversion algorithm, we hand-picked the she ar wave arrival times for both hydrofractures and inverted them with C VM. Finally, to correct for the areal inhomogeneity of the rock, we ca lculated the distortion of conical waves that were generated by air gu n blasts in a remote observation well. This novel technique improved s ignificantly the accuracy of the event locations in the shallow hydrof racture. The azimuth of both hydrofractures was N21 degrees +/- 4 degr ees E. In each treatment well, there were two separate hydrofractures at two different depths that correspond to the diatomite layers with h igher permeabilities. Both shallow hydrofractures were asymmetrical. I nitially, the upper NE wing was 230 ft long, whereas the lower SW wing was only 30 ft long. The deep hydrofracture was symmetrical and the w ings of its two parts were initially 130 and 10 ft long, respectively. These conclusions agree well with temperature surveys in the surround ing observation wells during steam injection.