*2014/03/03 10:13:19.23
*IOS HEADER VERSION 1.10 2011/10/26 2011/10/26

*FILE
    START TIME          : PST 1933/07/26 10:22:00.000
    NUMBER OF RECORDS   : 10
    DATA DESCRIPTION    : Bottle:Wire
    NUMBER OF CHANNELS  : 6

    $TABLE: CHANNELS
    ! No Name                    Units    Minimum        Maximum
    !--- ----------------------- -------- -------------- --------------
       1 Depth                   metres   1              185
       2 Temperature:Reversing   'deg C'  8.3            15.8
       3 Salinity:Bottle         ppt      28.06          32.56
       4 Oxygen:Dissolved        mL/L     0.441          7.728
       5 Silicate                umol/L   14.1           65.7
       6 Phosphate               umol/L   0.33           2.48
    $END

    $TABLE: CHANNEL DETAIL
    ! No  Pad     Start  Width  Format  Type  Decimal_Places
    !---  ------  -----  -----  ------  ----  --------------
       1  -99.9   ' '        6  F       ' '     0
       2  -99.99  ' '        7  F       ' '     2
       3  -99.99  ' '        7  F       ' '     2
       4  -99.99  ' '        7  F       ' '     2
       5  -99.99  ' '        6  F       ' '     1
       6  -99.99  ' '        7  F       ' '     2
    $END

*ADMINISTRATION
    MISSION             : 1933-01
    AGENCY              : PBS
    PROJECT             : Nootka Sound Study
    SCIENTIST           : J. P. Tully
    PLATFORM            : CGS Wm. J. Stewart

*LOCATION
    GEOGRAPHIC AREA     : Nootka Sound
    STATION             : 2233-K
    EVENT NUMBER        : 11
    LATITUDE            :  49  51.20000 N  ! (deg min)
    LONGITUDE           : 126  39.90000 W  ! (deg min)

*INSTRUMENT
    $REMARKS
        Water samples were taken  with an unnamed type of sample bottles.
        Temperatures were presumably obtained with  reversing thermometers but the
        paper makes no mention of reversing thermometers.
        The paper reports chlorinity (presumbably determined by titration) and it ha
        been converted to salinity.
        Dissolved oxygen, silicate and phosphate were reported in the paper but
        once again no methods were described.
        Time is presumed to be PST.
        Reference:
        Tully, John P., 1937
        Oceanography of Nootka Sound.  J. Biol.Bd. Can., 3(1) 1937.
    $END

*HISTORY

    $TABLE: PROGRAMS
    !   Name               Vers   Date       Time     Recs In   Recs Out
    !   ------------------ ------ ---------- -------- --------- ---------
        CLEAN              2.8.2  2000/04/06 10:54:57        10        10
        CALIB              11.0   2003/05/26 13:44:50        10        10
        HDREDIT2           1.6    2003/05/26 13:45:25 ?         ?
        CHANGE_MISSION_IDs 1.0    2014/03/03 10:13:19        10        10
    $END
    $REMARKS
        CLEAN functions:
         - Reset #RECS, MIN & MAX values in header.
         - Customise the Data Column Headings at the end of the header.
        -The following CALIB parameters were used:
         Calibration type = Correct
         Mode: ONLY - calibration specs from Cal File only.
         Calibration file = H:\New_Archive\Work\CALIB\oxygen.CCF
         Calibrations applied:
         Ch Name                          Units    Fmla Coefficents
         -- ----------------------------- --------- --- -----------------------------
          4 Dissolved_Oxygen:vol          mL/L       10  0.0000000E+00  0.7000000E+00
    $END

*CALIBRATION

    $TABLE: CORRECTED CHANNELS
    !   Name                   Units  Fmla Pad    Coefficients
    !   ---------------------- ------ ---- ------ ------------
        Dissolved_Oxygen:vol   mL/L     10 -99.99 () (0 0.7)
    $END
!--1-- --2--- --3--- --4--- --5-- --6---
!Depth Temper Salini Oxygen Silic Phosph
!      ature: ty:    :      ate   ate   
!      Revers Bottle Dissol             
!      ing           ved                
!----- ------ ------ ------ ----- ------
*END OF HEADER
    1.  15.80  28.06   7.51  14.1   0.33
    2.  12.20  29.94   7.73  15.0   0.52
    4.  10.80  30.08   7.21  18.1   0.69
    6.   9.90  31.18   6.66  26.8   0.73
   10.   8.90  31.71   3.81  47.4   1.33
   15.   8.90  31.80   3.67  42.1   1.42
   25.   8.60  32.01   3.21  42.1   1.54
   45.   8.40  32.23   3.15  42.1   1.45
   95.   8.30  32.30   2.54  41.5   1.50
  185.   8.50  32.56   0.44  65.7   2.48