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91.
92.
Isobe T Oshihoi T Hamada H Nakayama K Yamada TK Tajima Y Amano M Tanabe S 《Marine pollution bulletin》2011,63(5-12):564-571
Contamination status of brominated flame retardants (BFRs) and persistent organic pollutants (POPs) in blubber of finless porpoises (Neophocaena phocaenoides) stranded along the coasts of Seto Inland Sea and Omura Bay in Japan were investigated. Levels of PCBs, DDTs and CHLs were significantly higher than those of HCHs, HCB, PBDEs and HBCDs. Concentrations of PBDEs and HBCDs, as well as organochlorine compounds in males increased with body length (p<0.05). Among 14 PBDE congeners analyzed, BDE-47 was the predominant, which is similar to those generally reported in biota. PBDEs, HBCDs and PCBs showed no obvious temporal trend in concentrations during the study period, suggesting continuous environmental release of these chemicals. On the other hand, levels of DDT, CHLs and HCHs have decreased. Concentrations of PCBs in liver trematode infected individuals were significantly higher than those in not infected individuals, implying there could be a relationship between contaminant levels and parasitic infection. 相似文献
93.
Yuki Sato Naoto Hirano Shiki Machida Junji Yamamoto Masao Nakanishi Teruaki Ishii 《International Geology Review》2018,60(10):1231-1243
The stress field of oceanic lithosphere controls the distribution of submarine petit-spot volcanoes. However, the eruption sites of these petit-spot volcanoes are considered to be limited to concavely flexed regions of lithosphere off the outer rise. Here, we present new data for a recently identified petit-spot lava field on a convexly flexed section of the lithosphere adjacent to the subduction zone offshore of northeast Japan in an area containing more than 80 volcanoes. This area is marked by strongly alkaline lavas that were erupted on the convexly flexed region. As for the concavely flexed region where the petit-spots previously reported, the base of the lithosphere beneath the eruption sites is under extension, whereas the upper part of the lithosphere is under compression. This change in the stress field, from the lower to upper lithosphere, causes ascending dikes to stall in the mid-lithosphere, leading to metasomatic interaction with the surrounding peridotite. The new geochemical data of rocks and xenocrysts presented in this study indicate that strongly alkaline magmas erupted on the convexly flexed region would have ascended more rapidly through the mid-depth of lithosphere because of the extensional regime of the upper lithosphere and decreasing the degree of metasomatic reaction with the surrounding mantle peridotite. The results indicate that the degree of metasomatism and the compositional variations of petit-spot magmas are controlled mainly by the stress field of the lithosphere. 相似文献
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Simulation of eutrophication and associated occurrence of hypoxic and anoxic condition in a coastal bay in Japan 总被引:1,自引:0,他引:1
A probabilistic method of calculating the occurrence of oxygen-depleted water within a combined hydrothermal and water quality model was presented in this paper to investigate the environmental impact of eutrophication on the living resources. The method was applied to an eutrophicated shallow coastal bay in western Japan, where the occurrence of red tides at the water surface and the onset of bottom hypoxic waters are observed every summer. Both meteorology and freshwater inflow contribute to the development of stratification of the bay, thus limiting the dissolved oxygen supply to bottom waters. The resulting hydrodynamics enhances the development of oxygen-depleted bottom waters by transporting organic matter produced by algal blooms to the inner bay, where it decomposes and exerts high SOD. During August, about 60% of the inner bay is hypoxic for prolonged durations and as a result most of the benthic biota and fish die. The method used here is a very useful and informative way to evaluate the spatial and temporal damage and severity caused by hypoxia on living resources. Moreover, the model results agreed very well with the observed hydrodynamics, thermal structure and water quality data of the stratified bay. The model can be used for other lakes and bays where knowledge of temperature and density stratification is important for assessing water quality. 相似文献
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By using data obtained at about 120 XBT stations, cold water regions in the vicinity of the shoal, Kokushô-sone (30°00N, 128°30E), which is located in the current zone of the Kuroshio in the East China Sea, were investigated.The temperature cross-sections obtained were compared with corresponding cross-sections obtained from the four former cruises which were already reported. On the present cruise forced upwelling area was found along the south slope of the shoal, instead of the north slope as was found on the former cruises.The area of the cold water region found along the south slope tends to decrease with decrease in depth, and at depths shallower than 250 m the cold water region extends northward passing the shoal. The area at a depth of 400 m is comparable to that of the shoal itself, and is about 35 km2.Physical parameters and their scales which seem to be related to the dynamics near the shoal are given in the Appendix. 相似文献
100.
Takeshi Kawano Michio Aoyama Terry Joyce Hiroshi Uchida Yasushi Takatsuki Masao Fukasawa 《Journal of Oceanography》2006,62(6):777-792
An updated batch-to-batch difference table of IAPSO standard seawater (SSW) up to P145 is proposed. The batch-to-batch difference
table is based on several recent SSW comparison experiments, including the experiments conducted independently at the Japan
Agency for Marine-Earth Science and Technology (JAMSTEC) and Woods Hole Institute of Oceanography (WHOI) at about the same
time using the same procedure. Proposed batch-to-batch differences range from 1.2 × 10−3 to −1.9 × 10−3 with reference to the average of those from P91 to P102. Batch-to-batch differences from P29 to P145 with reference to the
recent batches and this average over every 5 years since 1960 are also presented, together with standard deviation. This reveals
that inconsistency among batches has improved since 1980s. In particular, the standard deviation was 0.3 × 10−3 in this decade, which is about one-half the value reported previously and almost equal to the modern measurement precision
(0.2 × 10−3) and is within-batch difference (<0.3 × 10−3). Proposed batch-to-batch differences were applied to the observational results of the WOCE hydrographic onetime section
(WHP onetime) in the Indian Ocean. Average absolute salinity differences at 14 crossover points in the Indian Ocean were slightly
larger, from 1.2 × 10−3 to 1.5 × 10−3, when the batch-to-batch difference table was applied; however, when results from the Indian, Pacific, and Atlantic Oceans
were combined, application of the batch-to-batch difference table yielded statistically acceptable salinity differences. The
table was also applied to WHP sections P1 and P17 (revisited about 10 years after the original observations during the WOCE
period) and sections I1, I7, and I8 (visited twice by different research vessels in the same year). In all cases, the table
corrected unrealistically large salinity changes in space and time. The results suggest that the application of the batch-to-batch
table to well-controlled salinity data such as WOCE datasets would be effective in making the datasets more consistent in
space and time. 相似文献