Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan     

Hiroshi Sato  Naoshi Hirata  Takaya Iwasaki  Makoto Matsubara  Takeshi Ikawa   《Tectonophysics》2002,355(1-4)

Knowledge of the crustal structure, especially the geometry of seismogenic faults, is key to understanding active tectonic processes and assessing the size and frequency of future earthquakes. To reveal the relationship between crustal structure and earthquake activity in northern Honshu Island, common midpoint (CMP) deep reflection profiling and earthquake observations by densely deployed seismic stations were carried out across the active reverse faults that bound the Ou Backbone range. The 40-km-long CMP profiles portray a relatively simple fault geometry within the seismogenic layer. The reverse faults merge at a midcrustal detachment just below the base of the seismogenic layer, producing a pop-up structure that forms the Ou Backbone range. The top of the reflective middle to lower crust (4.5 s in travel time (TWT)) nearly coincides with the bottom of seismogenic layer. The P-wave velocity structure and surface geology suggest that the bounding faults are Miocene normal faults that have been reactivated as reverse faults.  相似文献   

Runoff generation processes estimated from hydrological observations on a steep forested hillslope with a thin soil layer   总被引：4，自引：0，他引：4  

Makoto Tani 《Journal of Hydrology》1997,200(1-4):84-109

In order to understand runoff generation processes on a forested hillslope involving large heterogeneities, this study monitored runoff from a steep hillslope with a thin soil layer as well as matric potential within it and analyzed their responses to storm rainfall. A comparison of storm runoff responses from the study slope with those from two adjacent catchments, one of which includes it, showed that physical properties of the slope reflected the runoff characteristics: although no responses occurred in very dry conditions because of the absence of wet zones near the stream, the area contributing to storm runoff more rapidly extended to the whole slope due to its topographic properties. They also caused its steep hydrographs produced in the wettest condition where almost all the rainfall contributed to storm runoff. In this wettest condition, tensiometric responses near bedrock showed the vertical quick propagation of the rainfall pulse, and a good agreement of storm hydrograph simulated through a kinematic wave runoff model suggested that runoff from the slope was produced by a lateral flow on the bedrock receiving the quick propagation. In a transition process from dry to the wettest conditions, the development of the lateral flow producing smaller responses at the downslope end was estimated from decreasing of matric potential near bedrock from high negative to low values with increasing cumulative rainfall.  相似文献   

Dynamics of Lithosphere Convergence     

Makoto Yamano  Manik Tulwuni  Kensaku Turnuki 《Island Arc》1997,6(3):233-233

  相似文献   

Long-term temperature monitoring in a borehole drilled into the Nojima Fault, southwest Japan   总被引：2，自引：0，他引：2  

Makoto Yamano  Shusaku Goto 《Island Arc》2001,10(3-4):326-335

Abstract Long-term monitoring of temperature distribution in an active fault zone was carried out using the optical fiber temperature-sensing technique. An optical fiber cable was installed in a borehole drilled into the Nojima Fault in Awaji Island, south-west Japan, and the temperature profile to a depth of 1460 m had been measured for 2.5 years (July 1997–January 2000). Although the obtained temperature records showed small temporal variations due to drifts of the measurement system all along the cable, local temperature anomalies were detected at two depths. One at around 80 m seems to correspond to a fracture zone and may be attributed to groundwater flow in the fracture zone. This anomaly had been stable throughout the monitoring period, whereas the other anomaly at around 500 m was a transient one. The water level in the borehole could be estimated from the diurnal temperature variations in the uppermost part of the borehole and may provide information on the hydrological characteristics of the fault zone, which is connected to the borehole through perforations on the casing pipe. Except for these minor variations, the temperature profile had been very stable for 2.5 years. The conductive heat flow calculated from this profile and the thermal conductivity measured on core samples increases with depth, probably resulting from errors in thermal conductivity due to sampling problems and/or from advective heat transfer by regional groundwater flow. Assuming that the middle part of the borehole (less fractured granite layer) is least affected by these factors, heat flow at this site is estimated to be approximately 70 mW/m².  相似文献   

A New Empirical Formula for the Aerodynamic Roughness of Water Surface Waves     

Koji Ueno  Makoto Deushi 《Journal of Oceanography》2003,59(6):819-831

A new empirical formula for the aerodynamic roughness of water surface waves has been derived from laboratory experimental results using dimensional analysis. The formula has different forms according to wind speed: at moderate wind speeds the formula is a function of the friction velocity of wind, the surface tension, the water density, the kinematic viscosity of water and the acceleration of gravity; at strong winds the formula is expressed by the Charnock relation. The aerodynamic roughness does not depend on such wave state parameters as the spectral peak frequency or the steepness of waves, unlike almost all parameterizations that have been proposed to date. The drag coefficient at moderate winds depends on the surface tension of water and the water temperature through the temperature dependence of the kinematic viscosity of water.  相似文献   

Zooplankton investigations in Yatsushiro-kai,western Kyushu,I     

Reiichiro Hirota  Makoto Hara 《Journal of Oceanography》1975,31(3):115-123

The occurrence of the zooplankton at 21 stations in Yatsushiro-kai, western Kyushu, was investigated in June, September and November of 1968, and March of 1969. Copepods formed the most predominant constituent among the collected Zooplankton. AlthoughParacalanus parvus was abundant in most of the surveyed region, other copepods occurred dominantly in the following order when going from the northeastern area toward the southwest: Oithona nana→Acartia clausi→Microsetella norvegica→Oithona similis→Corycaeus spp. Yatsushiro-kai can be characterized biologically by dividing it into two main regions. The northern half is more embaymental and the southern half is more oceanic, bordered by an area whereMicrosetella norvegica occurred as the dominant. The area whereAcartia clausi occurred dominantly is the most embaymental in the northern half, and the area whereCorycaeus spp. occurred dominantly is the most oceanic in the southern half.  相似文献   

Effect of dietary docosahexaenoic acid on lipogenesis and lipolysis in black sea bream, Acanthopagrus schlegeli   总被引：2，自引：0，他引：2  

JI Hong  OM Ahamd Dau  YOSHIMATSU Takao  UMINO Testuy  NAKAGAWA Heisuke  FURUHASHI Makoto  SAKAMOTO Shuichi 《海洋学报(英文版)》2007,26(1):112-121

1 IntroductionIt is well known that varying dietary fatty acidprofile affects the tissue fatty acid composition and e-ven the growth performance in fish ( Bell et al.,2002; Figueiredo -Silva et al., 2005; Harel andPlace, 2003; Schulz et al., 2005; Tocher et al.,2003). Docosahexaenoic acid (DHA), an importantessential fatty acid for marine species, has the effectnot only on the fatty acid profile of fish body tissue,but also on biological and physiological conditions(Ishizaki et al., 2000; …  相似文献   

Growth characteristics ofChattonella antiqua     

Yasuo Nakamura  Makoto M. Watanabe 《Journal of Oceanography》1983,39(4):151-155

Nutrient requirements of a red tide flagellate,Chattonella antiqua, were investigated in a laboratory culture experiment. Growth ofC. antiqua was supported by nitrate and ammonium, and by urea to a limited extent, but not by glycine, alanine and glutamate. Orthophosphate served as a good phosphorus source but glycerophosphate did not. Fe³⁺ (1µM) fully promoted the flagellate's growth in the presence of 80µM of EDTA. The addition of Mn²⁺ (0–20µM), Zn²⁺ (0–10µM) and Co²⁺ (0–0.4µM) did not show any effect. Among three vitamins tested, only B₁₂ (6 ng 1^?1) served as a growth factor. Glucose, acetate and glycolate did not improve growth in the light nor did they support growth in darkness. The minimum cell quotas for nitrogen, phosphorus, iron and B₁₂ were estimated to be 11 pmoles ce^?1, 1.0, ～0.09 and 1.1 fg cell^?1, respectively.  相似文献   

An Ecological-Physical Coupled Model with Ontogenetic Vertical Migration of Zooplankton in the Northwestern Pacific     

Michio J. Kishi  Hitoshi Motono  Makoto Kashiwai  Atsushi Tsuda 《Journal of Oceanography》2001,57(5):499-507

A vertical one-dimensional ecosystem model with vertical migration of zooplankton was constructed and applied to Station A-7 off Sanriku district of Japan in the northwest Pacific Ocean. The model consists of an eight-compartment ecosystem model coupled with a physical model of the oceanic mixed layer. The transition of phytoplankton species responsible for the spring bloom is well reproduced by this model with vertical migration of zooplankton but is not simulated by the model without vertical migration. This new model also simulates an observed inter-annual variability of the spring bloom, with the timing and intensity of the simulated bloom in a given year depending upon the strength of mixing during the preceding winter. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Warped temperature profiles observed in the sediment of geothermally active areas in the Japan Sea— A hypothesis of double diffusive sinking     

Masashi Yasui  Makoto Yamano  Masataka Kinoshita 《Progress in Oceanography》1988,21(3-4)

Some temperature profiles observed in sea floor sediments of the Japan Sea, west of the northern part of Honshu, show distinct gradients changing with depth, for which we use the term warping. Using a simplified model, this warping can be attributed to an abrupt temperature change in the bottom water just above the sediment. The bottom water temperature change might be explained by the hypothesis that warm and salt surface water in the region sank to the sea bottom, through colder and less saline water, maintaining a relatively warmer temperature than the bottom water which originates from ordinary lateral intrusion.  相似文献