*2013/12/16 15:17:43.36 *IOS HEADER VERSION 1.10 2011/10/26 2011/10/26 *FILE START TIME : UTC 1999/05/26 10:32:37.000 TIME INCREMENT : 0 0 0 0.416667E-01 0 ! (day hr min sec ms) NUMBER OF RECORDS : 15 DATA DESCRIPTION : Bottle:Rosette:Up:Stop FILE TYPE : ASCII NUMBER OF CHANNELS : 4 $TABLE: CHANNELS ! No Name Units Minimum Maximum !--- ------------------ --------- -------------- -------------- 1 Sample_Number n/a 814 828 2 Pressure decibar 0.8 313.4 3 Oxygen:Dissolved mL/L 3.602 7.97 4 Salinity:Bottle PSS-78 30.7303 30.8172 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places !--- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 5 I I 0 2 -99 ' ' 7 F ' ' 1 3 -99 ' ' 8 F ' ' 3 4 -99 ' ' 9 F ' ' 4 $END $REMARKS This file converted from Sea-Bird file: E:\data\1999\9906\99060136.ros Comments from secondary file: d:\data\1999\9906\99060136.oxy ------------------------------------------------------------ Raw data in file 9906 VI03 = 10.02 ! Volume of iodate standard (cm**3) NI03 = .0101285 ! Normalitity of iodate standard VREG = 2.0 ! Volume of sample displaced by reagents (cm**3) DOREG = 0.0017 ! Absolute amount of O2 added with reagents (ml) UFLAG = 0 ! 0|-1, -1 indicates DO_mass is valid $END *ADMINISTRATION MISSION : 1999-06 AGENCY : IOS, Ocean Science and Productivity, Sidney, B.C. COUNTRY : Canada PROJECT : Laperouse, Strait of Georgia SCIENTIST : Juhasz T. PLATFORM : John P. Tully *LOCATION GEOGRAPHIC AREA : West Coast Vancouver Island STATION : STN 42 EVENT NUMBER : 136 LATITUDE : 49 1.78000 N ! (deg min) LONGITUDE : 123 26.23000 W ! (deg min) WATER DEPTH : 323 *INSTRUMENT TYPE : Bottle MODEL : Niskin 10 Litre SERIAL NUMBER : 0437 $TABLE: SENSORS ! Name Abs Depth Serial No ! ----------------- -------------- ---------- temperature ' ' primary conductivity ' ' primary pressure ' ' 63502 temperature ' ' secondary conductivity ' ' secondary transmissometer ' ' 192D $END $REMARKS SOFTWARE VERSION 4.235 Comments from secondary file: d:\data\1999\9906\99060136.oxy ------------------------------------------------------------ Dissolved oxygen concentration determined using an automated titration system consisting of a Brinkman Dosimat (model 665) and a PC 900 Colorimeter. $END *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! ------------------------ ------ ---------- -------- --------- --------- SBE_IOS 1.1 1999/06/03 11:09:01 1455 1455 BINAVE 3.0 1999/06/03 13:22:18 1455 15 MERGE 2.3 1999/06/03 15:16:47 15 15 CALIB 7.5 1999/06/04 09:51:09 15 15 MERGE 2.3 1999/06/04 10:14:55 15 15 REMOVECH 3.2 2000/01/11 15:40:53 15 15 HDREDIT2 1.9 2004/01/13 16:33:12 ? ? SORT 3.4.1 2004/01/13 16:33:31 15 15 CLEAN 4.5 2004/01/13 16:33:42 15 15 CHANGE_CTD_CHANNEL_NAMES 1.0 2013/12/16 15:17:43 15 15 $END $REMARKS -The following BINAVE parameters were used: Bin channel = SAMPLE_NUMBER Averaging interval = 1.0 Minimum bin value = 0.000 Bin value was used Interpolated values were NOT used for empty bins Channel 'NUMBER_OF_BIN_RECORDS' was added to file. -The following MERGE parameters were used: Merge Channel: Sample_Number Merge Scheme Used: Add Secondary to Primary Overlap Scheme Used: Keep Primary Primary Channels to Include: Pressure, Temperature:Primary, Temperature:secondar, Salinity:T0:C0, Salinity:T1:C1, Transmissivity, Bottle_Number Secondary Channels to Include: Dissolved_Oxygen:vol, Flask_Number Primary file : d:\data\1999\9906\99060136.avg Secondary file: d:\data\1999\9906\99060136.oxy Comments from secondary file: d:\data\1999\9906\99060136.oxy ------------------------------------------------------------ C.H. Culbertson's paper on Dissolved Oxygen in the 'Woce Hydrographic Program Operations and Methods - July 1991' -The following CALIB parameters were used: Calibration type = C Pressure offset = 0.0 Calibration file = e:\data\1999\9906\9906oxy.cor -The following MERGE parameters were used: Merge Channel: Sample_Number Merge Scheme Used: Add Secondary to Primary Overlap Scheme Used: Keep Primary Primary Channels to Include: Pressure, Temperature:Primary, Temperature:secondar, Salinity:T0:C0, Salinity:T1:C1, Transmissivity, Bottle_Number, Dissolved_Oxygen:vol, Flask_Number Secondary Channels to Include: Salinity:Bottle Primary file : d:\data\1999\9906\99060136.cor Secondary file: d:\data\1999\9906\99060136.sal -The following CHANNEL(S) were removed from file. SALINITY:PRIMARY SALINITY:SECONDARY Temperature:Secondary Temperature:Primary Salinity:T0:C0 Salinity:T1:C1 TEMPERATURE:SAMPLE DISSOLVED_OXYGEN:MASS THIOSULFATE_TITER FLASK_NUMBER FLASK_VOLUME BLANK STANDARD IRRADIANCE_PAR CHL_FLUORESCENCE Transmissivity Bottle_Number SALINITY:CTD TEMPERATURE:CTD Temperature -The following SORT parameters were used. Sorted by channel: Pressure Pressure channel sorted according to values in sort channel CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 0 deleted. - Set channel name post-colon letters to upper case. - Remove Sea-Bird comments from the header. $END *COMMENTS Collection method: ------------------ A rosette, holding 24 ten-litre water samplers, with a CTD was used. Analysis methods: ----------------- Salinity samples are collected in glass bottles and analyzed on Guildline model 8410 Portasal Salinometers which are standardized with IAPSO standard seawater. Oxygen samples are analyzed on an automated Winkler titration system following the procedures of Carpenter (1965). A Brinkmann model 665 Dosimat and model PC910 Colorimeter is controlled by Visual-Basic program to titrate the oxygen samples. References: 1. Carpenter, J.H. 1965. The Chesapeake Bay Institute Technique for the Winkler Dissolved Oxygen Method. Limmnol. & Oceanogr., 10: 141-143. *CALIBRATION $TABLE: CORRECTED CHANNELS ! Name Units Fmla Pad Coefficients ! ------------------------- ------ ---- ------ ------------ Dissolved_Oxygen:volume ml/l 10 -99 () (0 0.9988) $END !-1-- --2--- ---3--- ---4---- !Samp Pressu Oxygen: Salinity !le_ re Dissolv :Bottle !Numb ed !er !---- ------ ------- -------- *END OF HEADER 828 0.8 -99.000 -99.0000 827 1.6 7.970 -99.0000 826 10.4 6.572 -99.0000 825 20.3 5.594 -99.0000 824 30.7 5.275 -99.0000 823 50.6 4.949 -99.0000 822 74.8 5.131 -99.0000 821 100.2 5.314 -99.0000 820 125.4 5.206 -99.0000 819 150.3 5.097 -99.0000 818 175.0 4.929 -99.0000 817 200.6 4.853 -99.0000 816 251.0 3.845 30.7303 815 301.3 3.637 30.8092 814 313.4 3.602 30.8172