*2004/02/23 16:49:19.81 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : PST 1977/09/24 14:03:00.000 NUMBER OF RECORDS : 9 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII NUMBER OF CHANNELS : 7 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- -------- -------------- -------------- 1 Depth metres 0 150 2 Oxygen:Dissolved mL/L 1.745 6.106 3 Salinity:Bottle ppt 31.386 33.223 4 Temperature:Reversing 'deg C' 6.82 11.59 5 Phosphate umol/L 1.41 2.9 6 Nitrate umol/L 8.2 32.5 7 Silicate umol/L 21.4 63.1 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 6 F R4 0 2 -99 ' ' 8 F R4 3 3 -99 ' ' 8 F R4 3 4 -99 ' ' 7 F R4 2 5 -99 ' ' 7 F R4 2 6 -99 ' ' 6 F R4 1 7 -99 ' ' 6 F R4 1 $END *ADMINISTRATION MISSION : 1977-14 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Inner Passage SCIENTIST : Thomson R.E. PLATFORM : Parizeau *LOCATION STATION : QD16 EVENT NUMBER : 30 LATITUDE : 53 27.50000 N ! (deg min) LONGITUDE : 130 45.00000 W ! (deg min) *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- SPRD2IS 3.4.6 2001/12/17 10:57:35 9 9 HDREDIT2 1.6 2003/06/04 14:40:26 ? ? CLEAN 4.2 2003/06/04 14:42:28 9 9 HDREDIT2 1.9 2004/02/23 16:49:19 ? ? $END $REMARKS CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 0 deleted. $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). Nutrient samples are analyzed frozen using a Technicon autoanalyzer under contract to Seakem Oceanography Ltd. References: R.E. Thomson, W.S. Hugget and L.S.C. Kuwahara. 1980. Data Record of Current Observations Volume VIII; Discovery Passage, Johnstone Strait, and Queen Charlotte Strait; Part 1 - Water Property Observations 1976, 1977, 1978, (1979). Institute of Ocean Sciences. !--1-- ---2--- ---3--- --4--- --5--- --6-- --7-- !Depth Oxygen: Salinit Temper Phosph Nitra Silic ! Dissolv y: ature: ate te ate ! ed Bottle Revers ! ing !----- ------- ------- ------ ------ ----- ----- *END OF HEADER 0. 6.106 31.386 11.59 1.41 8.2 21.4 10. 5.547 31.532 11.00 1.49 11.2 25.2 20. 4.947 31.903 10.18 1.66 16.3 31.0 30. 4.458 32.109 9.63 1.91 18.2 32.5 50. 4.179 32.275 9.03 1.93 20.6 36.2 75. 3.684 32.673 8.39 2.19 24.1 42.5 100. 2.757 33.036 7.33 2.61 29.0 49.0 125. 1.907 33.164 6.94 2.90 32.5 63.1 150. 1.745 33.223 6.82 2.90 32.2 61.5