*2003/07/22 11:47:12.70 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1988/08/29 01:18:00.000 NUMBER OF RECORDS : 14 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII NUMBER OF CHANNELS : 2 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ------------------ -------- -------------- -------------- 1 Depth metres 10 400 2 Oxygen:Dissolved mL/L 1.925 6.547 $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 : LF06 EVENT NUMBER : 37 LATITUDE : 48 58.10000 N ! (deg min) LONGITUDE : 126 38.90000 W ! (deg min) WATER DEPTH : 448 *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- SPRD2IS 3.1 2000/11/02 13:12:54 14 14 REMOVECH 6.0 2003/07/22 11:47:07 14 14 HDREDIT2 1.6 2003/07/22 11:47:12 ? ? $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 6.482 10.0 6.403 20.0 5.790 30.0 6.206 50.0 6.547 75.0 6.395 100.0 4.759 125.0 2.810 150.0 2.901 175.0 2.781 200.0 2.666 250.0 2.333 300.0 2.311 400.0 1.925