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Kazue Tazaki Issei Morii 《地学前缘》2008,15(6):54-65
在日本Ishikawa Prefecture的Kanazawa大学进行了为期8个月的排水池培养实验,利用特征水和营养元素的基本因素对Sinohyliopsis schlegeli贝壳珍珠质所记录的环境变化进行观察。在2007年5月份到11月份之间,每个月向贝壳珍珠质注入四环素作为指示剂。定期测量水质,诸如pH、氧化还原势、电导率、溶解氧以及水温,通过过滤法除掉水中悬浮固体并进行光学显微镜和荧光X射线分析以及扫描电镜 能量色散X射线观察(SEM EDX)。对贝壳珍珠质的X射线荧光化学分析表明那些富含四环素的层对应高含量的Si、Mn、Fe和Sr离子。氧化还原势和溶解氧分析都证明在珍珠质中存在层。排水池中悬浮物质主要由Si、Mn和Fe元素组成,这与2007年夏季贝壳珍珠层的生物固定化中所涉及的元素一致。SEM EDX分析证明离子来自Siderocapsa sp.和Gallionella ferruginea硅藻的胃部。冬季几乎没有发生离子的生物固定化。结果表明在层化的贝壳珍珠质中存在元素的固定化,Sinohyliopsis schlegeli 在夏季以离子为食来生长珍珠质。具有这些生物氧化物的Sinohyliopsis schlegeli可能对自然界水体中重金属的清除有一定的贡献。 相似文献
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A 100 m laser strainmeter system installed in a 1 km deep tunnel at Kamioka, Gifu, Japan 总被引：1，自引：0，他引：1
Shuzo Takemoto Akito Araya Junpei Akamatsu Wataru Morii Hideo Momose Masatake Ohashi Ichiro Kawasaki Toshihiro Higashi Yoichi Fukuda Shinji Miyoki Takashi Uchiyama Daisuke Tatsumi Hideo Hanada Isao Naito Souichi Telada Nobuo Ichikawa Kensuke Onoue Yasuo Wada 《Journal of Geodynamics》2004,38(3-5):477
We have installed a laser strainmeter system in a deep tunnel about 1,000 m below the ground surface at Kamioka, Gifu, Japan. The system consists of three types of independent interferometers: (1) an EW linear strainmeter of the Michelson type with unequal arms, (2) an NS-EW differential strainmeter of the Michelson type with equal arms and (3) a NS absolute strainmeter of the Fabry–Perot type. These are configured in L-shaped vacuum pipes, each of which has a length of 100 m. (1) and (2) are highly sensitive (order of 10−13 strain) and have wide dynamical range (10−13–10−6). Observations with strainmeters (1) and (2) started on June 11, 2003. (3) is a new device for absolute-length measurements of the order of 10−9 of a long-baseline (100 m) Fabry–Perot cavity by the use of phase-modulated light. This third strainmeter will be ready for operation before the end of 2004. The laser source of strainmeters (1) and (2) is a frequency-doubled YAG laser with a wavelength of 532 nm. The laser frequency is locked onto an iodine absorption line and a stability of 2 × 10−13 is attained. The light paths of the laser strainmeter system are enclosed in SUS304 stainless steel pipes. The inside pressure is kept to be 10−4 Pa. Consequently, quantitative measurement of crustal strains of the order of 10−13 can be attained by employing the laser strainmeter system of (1) and (2) at Kamioka. This resolving power corresponds to that of a superconducting gravimeter. Using the laser strainmeter system, we expect to determine parameters related to fluid core resonance, core modes and core undertone as well as other geodynamic signals such as slow strain changes caused by silent earthquakes or slow earthquakes. 相似文献
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The seismic observation network in Shiga prefecture iscomposed of four systems.All the observation data obtained were used to estimatethe dynamic characteristicsof the surface soils around the lake and the seismichazard for Hikone City. Since1995, 21 records have been obtained at the USP site ofwhich those for the 1999Shigaken-Hokubu Earthquake and 1999 Wakayarnaken-HokubuEarthquake wereused in this study. Transfer functions of the surfacesoil in each ward of ShigaPrefecture based on the Mt. Kojin site (KJY), whichhas relatively hard soil, werecalculated from the records of the two earthquakes.Assuming a scenario earthquakeat the Hyakusaiji fault close to Hikone City, maximumground motions were obtainedfor 15 city blocks in order to establish a damageestimation for that city. The numberof collapsed wooden houses and the damage ratiowere calculated based on the distributionof construction of wooden houses by year. Blockswith a larger ratio of old, wooden housesin Hikone showed a close correlation with blockswith a large ratio of aged persons inthem, indicative that weak persons, such as theelderly, may find themselves in a severesituation during a natural disaster. 相似文献
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Measurements of the Turbulent Energy Dissipation Rate around the Shelf Break in the East China Sea 总被引：1，自引：0，他引：1
Takeshi?MatsunoEmail author Manabu?Shimizu Yasuhiro?Morii Hideaki?Nishida Yasuaki?Takaki 《Journal of Oceanography》2005,61(6):1029-1037
Using the micro-structure profiler, TurboMAP, large values for the turbulent energy dissipation rate ε were found just above the bottom of the shelf and around the thermocline near the continental shelf break in the East China
Sea. The values found above the bottom are produced by the bottom stress due to tidal currents, resulting in a distinct bottom
mixed layer where the vertical eddy diffusivity Kz is also large. Distinct maxima in the values of ε detected around the thermocline are located at the depth of the fine-scale shear maxima detected with the moored ADCP. The
vertical profiles of ε were compared with those of the current velocity, and it was found that the maxima in ε appear to correspond to those of the shear with fine scale. The magnitude of the observed ε coincided approximately with the ε calculated from the fine-scale shear and the buoyancy frequency according to the parameterization proposed by Gregg (1989),
if the large-scale mean shear caused by the Kuroshio is subtracted. However, it is not clear whether the parameterization
for the internal wave fields in the open ocean is applicable to the estimation of ε in the shelf break. Whereas the most predominant value of ε was found just above the bottom and around the thermocline, the maxima of ε could be found in the internal area. They could have been caused by the propagation of the vertically high wave number internal
tides along the characteristic ray. 相似文献
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