*2003/07/22 11:47:13.21
*IOS HEADER VERSION 1.4  2002/12/04 2002/12/04

*FILE
    START TIME          : UTC 1988/08/30 02:18:00.000
    NUMBER OF RECORDS   : 8
    DATA DESCRIPTION    : Bottle:Wire
    FILE TYPE           : ASCII
    NUMBER OF CHANNELS  : 2

    $TABLE: CHANNELS
    ! No Name               Units    Minimum        Maximum
    ! -- ------------------ -------- -------------- --------------
       1 Depth              metres   10             125
       2 Oxygen:Dissolved   mL/L     1.599          10.11
    $END

    $TABLE: CHANNEL DETAIL
    ! No  Pad   Start  Width  Format  Type  Decimal_Places
    ! --  ----  -----  -----  ------  ----  --------------
       1  0     ' '        7  F       R4      1
       2  -99   ' '        8  F       R4      3
    $END

*ADMINISTRATION
    MISSION             : 1988-14
    AGENCY              : IOS, Ocean Physics Division, Sidney, B.C.
    COUNTRY             : Canada
    PROJECT             : Laperouse, Endeavour Ridge
    SCIENTIST           : Thomson R.E.
    PLATFORM            : Parizeau

*LOCATION
    STATION             : LB08
    EVENT NUMBER        : 60
    LATITUDE            :  48  25.30000 N  ! (deg min)
    LONGITUDE           : 125  28.70000 W  ! (deg min)
    WATER DEPTH         : 129

*HISTORY

    $TABLE: PROGRAMS
    !   Name     Vers   Date       Time     Recs In   Recs Out
    !   -------- ------ ---------- -------- --------- ---------
        SPRD2IS  3.1    2000/11/02 13:12:55         8         8
        REMOVECH 6.0    2003/07/22 11:47:07         8         8
        HDREDIT2 1.6    2003/07/22 11:47:13 ?         ?
    $END
    $REMARKS
        -The following CHANNEL(S) were removed from file.
         flask
    $END

*INSTRUMENT
    TYPE                : Bottle
    MODEL               : Niskin (1.7 litre)

*COMMENTS

   Collection methods:
   -------------------
     Sea Water Temperature:
     - Reversing thermometers mounted on bottles.
     Salinity:
     - Collected in bottles.
     Dissolved Oxygen:
     - Collected in bottles.

   Analyzes methods:
   -------------------------
     Temperatures at depth were measured by deep-sea reversing thermometers of
     German (Richter and Wiese) and/or Japanese (Yoshimo Keiki Co.) manufacture.
     Two protected thermometers were used on all bottles, and one unprotected
     thermometer was used on each bottle at depths of 250 m or greater. The
     accuracy of protected reversing thermometers is believed to be +-0.02C.

     Salinity determinations were made at sea with a Guildline model 8400 lab
     salinometer.

     Depth determinations were made using the "depth difference" method
     described in the U.S.N. Hydrographic Office Publication No. 607 (1955).
     Depth estimates have an approximate accuracy of +-5 m for depths less than
     1000 m, and +-0.5% of depth for depths greater than 1000 m.

     The dissolved oxygen analyses were done in the shipboard laboratory by a
     modified Winkler method (Carpenter, 1965).
!--1--- ---2---
!Depth  Oxygen:
!       Dissolv
!       ed     
!------ -------
*END OF HEADER
    0.0  10.110
   10.0   7.223
   20.0   3.583
   30.0   2.608
   50.0   2.560
   75.0   2.084
  100.0   1.599
  125.0   1.654