90 research outputs found
Soil Liquefaction Potential Evaluation with Use of the Simplified Procedure
A simplified method based on both a liquefaction resistance factor, FL and a liquefaction potential factor, PL has been proposed for evaluating soil liquefaction potential. The factor FL indicates the liquefaction potential at a given depth of a site, and the factor PL indicates the one at a site. The effectiveness of the proposed method is investigated by calculating the factors FL and PL at both liquefied and non-liquefied sites during past typical earthquakes in Japan, and carrying out shaking table tests
Eine spektrophotometrische Schnellmethode zur Bestimmung von Brom in Meerwasser und in der Asche mariner Algen
ChemInform Abstract: THERMAL REACTIONS OF PHENYL DERIVATIVES OF DIMETHYLSULFONIUM 1-AROYL-6-OXO-2,4-HEXADIENYLIDE. A REMARKABLE EXAMPLE OF REACTIONS CONTROLLED BY INTRAMOLECULAR STERIC INTERFERENCES
Long-term consolidation behavior of Pleistocene clays in Osaka Bay and applicability of elasto-viscoplastic one-dimensional consolidation model
A Study on Nested Logit Mode Choice Model for Intercity High-Speed Rail System with Combined RP/SP Data
Physical, Chemical Properties and Crystallization Tendency of the New Fluoroaluminate Glasses
Temporary earthquake observation with very high density at residential valley-filling sites in Yokohama City, Japan
Appropriate frequency and time of day to measure methane emissions from an irrigated rice paddy in Japan using the manual closed chamber method
Rice agriculture is a large anthropogenic source of atmospheric methane (CH 4 ). The reliable estimation of CH 4 emissions requires frequent measurements to trace diurnal and seasonal variations. To evaluate the appropriate intervals and optimal time of day to measure CH 4 emissions using the manual closed chamber method, this study analysed four datasets of CH 4 fluxes in a Japanese irrigated rice paddy measured at 2-hour intervals using the automated closed chamber method. The typical diurnal variation in the CH 4 flux was observed after the rice's heading stage, during which the daily time-weighted mean CH 4 flux was observed twice, in the 08:00 11:59 and 18:00 21:59 time windows. During the flooded rice-growing period, the CH 4 emissions, which were estimated by weekly measurements once per day during the 10:00 11:59 time window, corresponded to 93 106% of the emissions calculated using the automated measurement method. In contrast, no regular measurement strategies produced a satisfactory estimate of the CH 4 emissions during the non-flooded rice-growing period because of a sharp increase in the CH 4 flux just after the drainage. Consequently, the combination of weekly measurements once per day at approximately 10:00 as local mean time for the flooded rice-growing period and daily measurements once per day during the daytime for 1 week after each drainage event is recommended as a strategy to obtain the estimation with a ±10% error
Evaluation of compliance with electronic pretransfusion check for blood administration at the bedside: a 10·5-year experience at a university hospital
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