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Title

    OBS-2013: Instrumentation notes

By
O.M.
Date
06 February 2014
Version
0.1
Click to see OBS-2013 photo album.
Click to see OBS-2013 photo album.

SURVEY, PROJECT DESCRIPTION


Survey duration 14 - 17 September 2013
Project name -
Project leader Prof. Rolf Mjelde, Department of Earth Science,
University of Bergen
Project funding -
Project duration -
Party chief Asbjørn Breivik, Department of Geosciences,
University of Oslo


GEOPHYSICAL EQUIPMENT


Item no. Name Description / Setup
1 Mini-streamer We are using an 8-channel mini-streamer: MicroEel, by Geometrics
2 Recording for Mini-streamer Geometrics GEODE.
  • S/N: 4153 ("CIPR-1")
  • Sample interval: 2 ms
  • Recording time: 8 s
  • Data format: SEG-Y
  • Filter settings: Only anti-alias filter (automatically adapted to sample rate).
3 Gravitymeter
  • Manufacturer, electronics: ZLS
4 Magnetometer
  • Manufacturer:Geometrics
  • Model: Mod. G-882
5 Time stamping equipment ProFlex Lite DG14
6 Navigation system
  • EIVA Survey Computer
  • Diff GPS:
    • Fugro "SeaStar", mod. 3510 LR
7 Airguns
  • 4 ea, Bolt model 1500, each 1200 inch 3 , in total 4800 inch 3
  • Air pressure, firing moment: 138 Bar = 2000 psi
  • Source depth: 6 m
8 Gun control system Geco GUNCO


DATA


Profiles


LINE INFORMATION EIVA SURVEY COMPUTER GPS TIMESTAMPS MINI-STREAMER UKOOA LOG SHEETS COMMENTS
ID SP INT [m] START
SP Date Time [UTC]
Easting Northing (UTM Zone 33)
END
SP Date Time [UTC]
Easting Northing (UTM Zone 33)
EVENT FILE 10 SECONDS LOGFILE RAW PROCESSED LOG FILES SEG-Y P1/90 FILES P1/90 QC FILES
LINE 1 200 0003
15.09.2013
03:48:37
575366.9 7705601.1
881
16.09.2013
01:00:49
428585.7 7802715.8
Link Link Link Link Link 2436.sgy Link (preliminary) Link (preliminary) - -


PRELIMINARY ANALYSIS OF MINI-STREAMER IRREGULARITIES


Description of irregularities


  1. First breaks (= direct arrival of air gun signal, following a straight line from source to receiver) arrives much too early.
  2. From FFID = 2809 the frequency content of the signal changes considerably. The recording log does not indicate any changes in system configuration - like number of guns firing, air pressure, de-activation of filtering in the GEODE mini-streamer recording system. The sudden change in signal characteristics is easily observable both in the time and frequency domain (see plots below).
  3. In shot gather displays, channel 8 - the most remote channel - appears to be nearest to the vessel.
  4. The frequency plots show an unusual amount of signal energy in the very low-frequency part of the spectrum.

Conclusions


Based on error analysis below, we have arrived at the following conclusions:

  1. The Mini-streamer tail buoy has probably been snagged into airgun floats, causing the streamer to take the shape of an "U" behind the ship. Channel no 8 was thus located nearest to the ship.
  2. Before FFID=2809 offset between source and center of nearest group (no. 8, due to the streamer U-shape mentioned above) is approx. 24 meter, and after FFID=2811 it is approx. 9 meter. Offset is of course much too small. It is assumed that hydrophone group no. 8 has been damaged because of this. Normal offset should be approx. 102 meter.
  3. The frequency spectrum indicates presence of unusual amount of signal energy in the very low frequency part (0-10 Hz). We believe this is due to the streamer U-shape causing lots of oscillations.
  4. After FFID=2811 it seems the streamer positioned itself much deeper in the water. By looking at bottom reflections before and after FFID=2811 the depth difference seems to be 15.6ms, which is two-way travel time; thus increased depth should be (15.6ms * 750m/s) = 11.7 meter. This will increase the streamer's ability to capture low frequency signals.

Mini-streamer layout, source position, expected First Break times


  • Mini-streamer:
    • Number of hydrophone groups: 8 ea
    • Group center spacing: 6.25 m
    • Number of hydrophones per group: 12
    • Hydrophone spacing within group: 0.5 m. Thus group length is (11*0.5 m) = 5.5 m
    • Lead-in length: 150 m
    • Lead-in deployed, from stern: 135 m
    • It appears that channel 8 is defective (no reflections).
  • Source:
    • Distance from stern to source: 36 meter
  • Offset between center of source, and midpoint of first group in streamer should thus be: (135m-36m) + (5.5m/2) = 101.75m. Assuming sound velocity of 1500 m/s, first break should arrive after 0.0678s = 67.8 ms
Calculating offset between source and first group.
Offset between source and first group: Before FFID 2809, group 7 (as no. 8 is defective) has First Break after 20ms; which means that ch. 8 should have First Break after (20-4.2) = 15.8ms (see below). That means offset is (15.8ms * 1500m/s) = 23.7m. After FFID=2811, offset is (13.5ms-4.2ms)*1500m/s => (9.3ms*1500m/s) = 9.3m.
  • Mini-streamer group center spacing is 6.25 m. With a water sound velocity of 1500 m/s the first break time difference between each channel should be: (6.25 m / 1500 m/s) = 0.0042 s = 4.2 ms
Measuring First Breaks between groups.
The 8 individual channels in each shot gather shown. Measured First Break time difference between two successive groups: 4.1 ms - expected 4.2 ms - that's a fairly good match. We can thus assume active section is aligned to ship's long axis.

Dimensions:

  Lead-in ............................: 150.00 m
  Active section: (7*6.25m) + 5.5m  ..:  49.25 m   (8 hydrophone groups 6.25 m apart, one half group (group length 5.5 m) at each end.
  Tail ...............................:  12.50 m
                                        --------
                       Total length ..: 211.75 m
                       -------------------------

Viewing data in time domain


Data in time domain - click to enlarge

Click to enlarge. Click to enlarge.
Click to enlarge. Click to enlarge.
Click to enlarge. Click to enlarge.
Difference between arrival time of bottom refection before and after FFID=2810 measured to 15.6 ms (TWT), which amounts to 11.7 meter.


Frequency domain analysis


Data in frequency domain - click to enlarge

Click to enlarge. Click to enlarge.
Click to enlarge.
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