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  • 1
    Electronic Resource
    Electronic Resource
    Synthesis of radiolabeled ethyl 0-benzoyl-3-chloro-2,6-dimethoxybenzohydroximates. Oxime-14C, carbonyl-14C, and 2-methoxy-14C (1972)
    s.l. : American Chemical Society
    Journal of agricultural and food chemistry 20 (1972), S. 936-939 
    Details
    ISSN: 1520-5118
    Source: ACS Legacy Archives
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/jf60183a026
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Lithium Dilution Cardiac Output Measurements Using a Peripheral Injection Site: Comparison with Central Injection Technique and Thermodilution (1999)
    Springer
    Journal of clinical monitoring and computing 15 (1999), S. 279-285 
    Details
    ISSN: 1573-2614
    Keywords: Heart: cardiac output ; Measurement techniques: thermodilution ; Measurement techniques: lithium dilution ; Measurement techniques: electromagnetic flowmetry
    Source: Springer Online Journal Archives 1860-2000
    Topics: Computer Science , Medicine
    Notes: Abstract Objective. The lithium dilution technique for the measurement of cardiac output by the central injection of lithium chloride was introduced by Linton et al. in 1993. In the present report, we compare lithium dilution cardiac output measurement (LD) by the peripheral injection of lithium chloride (pLD) and by central venous injection (cLD), cardiac output determined by electromagnetic flowmetry (EM), and conventional thermodilution cardiac output measurement (TD) on ten swine. Methods. The animals were monitored with a pulmonary artery catheter, a femoral artery catheter, and an electromagnetic flowmeter placed around the ascending aorta. cLD, pLD, TD, and EM were determined at the baseline, then in a hyperdynamic state produced by dobutamine administration, at a second baseline, and finally in a hypodynamic state induced by propranolol during deep anesthesia. Data were analyzed by linear regression analysis and the comparison method described by Bland and Altman; bias and precision were calculated using the method of Sheiner and Beal. Results. The correlation coefficient between pLD and EM (0.86) was significantly less than that between cLD and EM (0.96), however it was not significantly different from that between TD and EM (0.85). The precision value of pLD (0.14) was the same as that of TD (0.14). Conclusion. The results of the present study indicate that pLD is a reliable technique.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1009918904525
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  • 3
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    The List of volcanoes and Their Activities Records in the Adjacent Seas of Japan 2nd Revised Edition (2019)
    Details
    Publication Date: 2021-05-19
    Description: The Hydrographic Department of Japan actively participates in The Volcanic Eruption Prediction Plan since the Plan started in 1973. Observation of volcanic activities in the adjacent seas of Japan is very important, not only to protect safety navigation, fishery and other activities in the sea area against a disaster, but also to manage the sea area itself effectively. This list is a 2nd revised edition of “The List of Volcanoes and Their Activities Records in the Adjacent Seas of Japan" prepared by lwabuchi, Kato and Shibata (1994). There is no intensive volcanic eruption occurred in the sea area during the past five years, but a lot of fundamental data on geology and geophysics were collected from the surveys on Sumisu Sima, Tori Sima, Sohu Gan, Hatizyo Sima in the Nanpo Syoto arc and Others.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp. 15-71
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  • 4
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    Three Dimensional Multi-Channel Seismic Survey of the Northern Tokyo Bay (2020)
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    Publication Date: 2021-05-19
    Description: On the south of the Kanto plain, there is the Tokyo Bay northern fault that named after Kato (1983). The northern fault is one of the most remarkable fault in this area. In general, Fault is result of the past crustal movement. Thus it is important to predict earthquakes in the Kanto region to reveal the characteristics of the fault. Hydrographic Department conducted multi channel seismic survey for the purpose of clarifing the characteristics of the fault. The survey was carried out as the three-dimensional seismic method by multi-channel seismic survey with the very close line spacing. Geological structure of the fault is summarized as follows: 1) General trend of the Tokyo Bay northern fault is N60W, however, it is N35W at the center of the survey area. 2 ) It is difficult to distinguish whether the fault is normal or reverse because of the high dip angle of the fault plane. 3 ) According to the hor包ontalgeologic section (time slice), the strike of the sedimentary layer seems to be bended by left lateral movement. However, considering the dip of the sedimentary layers, the left lateral movement is not required. 4) The Tokyo Bay northern fault displaces the middle of the Kazusa group that is correlated with early middle Pleistocene.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: e.g.pp1-15
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  • 5
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    Multi-channel seismic reflection survey in the Sagami Trough. (2020)
    Details
    Publication Date: 2021-05-19
    Description: In 1984 and 1985, a multi-channel seismic reflection survey on the six survey lines were carried out by the Survey Vessel Takuyo of the Hydrographic Department of Japan in the Sagami Trough bordering the northeastern margin of the Philippine Sea plate. The survey has revealed some characteristics of the geological structure in the Sagami Trough. Acoustic basement reflector of the southern trough slope is traced beneath the Awa Canyon and bottom of the trough near the Boso Canyon. The basement is inclined northeastward, so the Philippine Sea plate is overlain by the Eurasia plate. Well-deformed layer and inclosed meardering canyon in the central part of the Sagami Trough presents a contrast to the other convergence boundary of plates. These indicate the change of tectonics after sedimentation of the layer and support the change of the direction of the plate motion. There is a large possibility that a zone of the Boso Canyon is a former accretionary prism, when the Philippine Sea plate moved to north and subducted beneath the northern slope
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.95-111
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  • 6
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    Summary of the multi-channel seismic reflection survey in the Nankai, Suruga and Sagami Troughs. (2020)
    Details
    Publication Date: 2021-05-19
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.1-4
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  • 7
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    Landforms of the Izu-Ogasawara Trench by the narrow multi beam echo sounder. (2020)
    Details
    Publication Date: 2021-05-19
    Description: The narrow multi-beam bathymetric survey in the Izu-Ogasawara Trench conducted by the survey vessel ”Takuyo”of Hydrographic Department of Japan. The survey area is from 27。30’N to 32°-20' N and about 45 km wide along trench axis. The Izu-Ogasawara Trench extends in N-S direction along the east of the Izu-Ogasawara Arc, and is situated on the boundary between the Philippine Sea Plate and the Pacific Plate. The trench is subdivided into three major geomorphological units as follows : 1) the landward wall of the trench, 2) the trench floor, 3) the seaward wall of the trench which are arranged from west to east. On the landward wall of the trench,many gentle slopes originated from submarine landslides are recognized. The size of landslides in the southern part of the trench become more large scale than those in the northern part. In the southern end of the survey area, there is a gigantic landslide which moves the landward wall of the trench to east and narrows the trench floor. The trench floor is separated into several basins by the ridges which extend in the NNW-SSE direction. On the central trench floor, there is a subducting seamount which is deforming by normal fault. The seaward wall of the trench has many horsts and grabens which formed by normal faults. The normal faults are subdivided into two types as follows . 1) faults with the strikes parallel to the trench axis, 2) faults with the strikes oblique to the trench axis. The parallel faults are formed by the bend of the oceanic plate (the Pacific Plate) which is subducting beneath the Philippine Sea Plate. In the southern part, the oblique faults is more well distributed than those in the northern part. The strike (NW-SE) of the oblique faults correspond to that of the faults of the fracture zone : the Bosδ Fracture Zone, the Ogasawara Fracture Zone on the western part of the Pacific Plate. The fact supports the idea that the plate bending also forms oblique faults which make use of the lineament of the fracture zones.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.173-180
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  • 8
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    Submarine topography around Io-Zima. (2020)
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    Publication Date: 2021-05-19
    Description: The submarine topographic survey around Iwo-Zima situated 1200 km south of Tokyo was carried out by the Hydrographic Department in 1981. By the result of this survey, a submarine topographic chart was drawn on the scale of 1 : 100, 000 (Fig. 2). The submarine topography around Iwo-Zima has some characteristics as follows; i ) Iwo-Zima is located at the summit of a concentric volcano of more than 40 km in basal diameter, and more than 2000 m in elevation. ii) Iwo-Zima volcano has two big lateral volcanoes, Kaise-Nisi-no- Ba located at 15 km WNW of the island and Kaise-Minami-no-Ba located at 25 km south of the island. There are also many small lateral volcanoes on the south and west slopes. iii) Topographic chart of Iwo-Zima volcano exhibits a caldera of about 10 km in diameter, and Motoyama which is the northeast part of the island is the central cone of this caldera. iv) An abrasion platform fringing the island is formed by wave erosion faster than the uplift of which rate is 50 cm/year in maximum. v) Front slope of the abrasion platform has become shallow about 20-40 m for 47 years because of uplift and elastics mainly supplied by the erosion of abrasion platform. vi) It is considered that the high rate uplift of lwo-Zima occurs at shallow waters but such uplift does not reach the caldera rim.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.59-73
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  • 9
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    Preliminary report of continental shelf surveys of " Titi Sima ” quadrangle. (2020)
    Details
    Publication Date: 2021-05-19
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.98-104
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  • 10
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    Chemical compositions of rocks erupted from submarine volcanoes and of volcanic rocks occurring in adjacent areas in the Izu-Ogasawara arc. (2020)
    Details
    Publication Date: 2021-05-19
    Description: This paper reports chemical compositions and chemical characteristics of volcanic rocks erupted from submarine volcanoes in the Izu・Ogasawara arc (from Myozin Reef(Myojin Reef) to Hukuzin Seamount (Fukujin Seamount)) . SiO2 content of the volcanic rocks ranges from 45 to 70 weight percent. The rocks from the north of Sohu Rock (Sofu Rock) are relatively poor in Na2O, K2O and P2O5, whereas most of the rocks from the south of Nisi-no-Sima (Nishinoshima) are enriched in these oxides. The alkaline rocks from lo- Sima Iwojima), Hukutoku-Oka-no-Ba(Fukutokuoka-no-ba)and Minami-Hiyosi Seamount (MinamiHiyoshi Seamount), which erupted recently, show the further enrichment in Na2O and K2O.
    Description: Published
    Repository Name: AquaDocs
    Type: Journal Contribution , Refereed
    Format: pp.61-85
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