R/V Shumpu Maru Cruise SU9309 1 Cruise Narrative 1.1 Highlights Expedition Designation Shumpu Maru Cruise SU9309 Chief Scientists Leg 3:Noriya YOSHIOKA, Kobe Marine Observatory(KMO) Ship R/V Shumpu Maru Ports of Call Leg 3:Hososima to Kochi Cruise Dates Leg 3:October 2 to October 6,1993 1.2 Cruise Summary The cruise track and station locations of leg 3 are shown in Figure 1. The ship departed Hososima on October 2,1993, and made 3 CTD/rosette stations of a section PR17. 1 XBT stations were made between CTD/rosette stations. To first CTD/rosette station the ship reached at 1153 UTC on October 2, from last station departed at 2009 UTC on October 2. The CTD is EG&G NBIS Mark III B(6500 db type, no oxygen sensor). Water samples were collected from 1.7 liter Niskin bottles mounted on the General Oceanics Rosette multisampler. However, surface water samples were collected by a bucket. 1.3 List of Principal Investigators The principal investigators for all the parameters measured on the cruise are listed in Table 1. Table 1: Principal Investigators for All Measurements Name Responsibility Affiliation Sukeyoshi TAKATANI Oxygen,Nutrients KMO Ryohei OKADA CTD,S KMO 1.4 List of Cruise Participants The cruise participants for leg 3 are listed in Table 2. Table 2: Cruise Participants for leg 3 Name Responsibility Affiliation Noriya YOSHIOKA Chief Scientist KMO Ryohei OKADA CTD Hardware KMO Nobuo SATO Oxygen, Nutrients KMO Satoshi SUGIMOTO CTD Software KMO Sukeyosi TAKATANI Oxygen, Nutrients KMO Keiichi SATO Watch Stander KMO Akira NAKADATE Oxygen, Nutrients KMO Toshiaki BABA Watch Stander KMO Hiroki SUZUKI Watch Stander KMO 2 Measurement Techniques and Calibrations 2.1 CTD The CTD is EG&G NBIS Mark III B(6500 db type, no oxygen sensor). A HP 9000 Series 300 model 330(Hewlett Packard) with a 4 MByte of memory was used as the primary data collection device. The temperature and pressure sensor were calibrated at the calibration facility of S¥E¥A CO., LTD before the cruise. The results are shown in Table 3. Temperature and pressure(increasing) calibration values are used to correct CTD data, by linear interpolation inside the calibrated regime. CTD data outside of the regime is corrected by the calibration values on the boundary, at the each side. Notice that the upcast pressure data is corrected by Pressure(increasing), not Pressure(decreasing) in Table 3. Table 3: The temperature and pressure sensor calibration values Temperature(Caliblated on October 9, pre-cruise) Standard Temperature CTD Temperature Difference 0.1512 0.1522 0.0000 15.1490 15.1498 0.0008 30.0912 30.0912 0.0010 Pressure (increasing, Caliblated on september 6, pre-cruise) Standard Pressure CTD Pressure Difference 0.0 0.1 -0.1 1516.8 1515.8 1.0 3033.7 3030.3 3.4 4550.5 4545.7 4.8 6067.4 6067.8 -0.4 Pressure (decreasing, Caliblated on september 6, pre-cruise) Standard Pressure CTD Pressure Differrence 0.0 0.1 -0.1 1516.8 1520.0 -3.2 3033.7 3030.8 -2.9 4550.5 4545.8 4.7 6067.4 6068.0 -0.6 The conductivity sensor were calibrated at sea using data from the analyses of salinity collected at 4 stations. The salinometer is AUTOSAL 8400B(Guildline) for the analyses of salinity of the water samples. The calibration constant is determined assuming that the bias 0. The results are shown in Table 4. Table 4: The conductivity sensor calibration constants Bias Slope 0 1.00040 The temperature of "SU9309.SEA" and "SU9309.CTD" files is described with the international temperature scale of 1990, ITS-90. 2.2 Oxygen Measurements The determination of dissolved oxygen was done by the modified version of the Winkler method described in "Kaiyo Kansoku Shishin (Manual of Oceanographic Observation)" published by the Oceanographical Society of Japan(1970). No estimation of accuracy and precision and reagent blank has been done. 2.3 Nutrients Analyses The nutrients analyses were done by the Technicon Auto Analyzer II described in "Kaiyo Kansoku Shishin (Manual of Oceanographic Observation)" published by the Oceanographical Society of Japan(1970). No estimation of accuracy and precision has been done.