Observation of B̅0→D(*)0pp̅

journal articl

Probabilistic Operation of Electric Power Systems Considering Environmental Constraint (Part 16)* -Consideration of the Effects of the Operation of An Energy Storage Facility-

application/pdfTo improve the power supply probability considering the envoromental pollution, the operation effectiveness of an energy storage facility is explained. The output power of two power stations is adjusted to satisfy the line capacities in the proposed method when the ordinary power dispatch introduces overflows in some power lines. By simulating the results of a model system, relations between the improvement of the power supply probability and the capacity of the energy storage facility is shown. It is also argued that the optimum operation cannot simply he decided by the minimum expected value of the operating cost.departmental bulletin pape

Studies on Probabilistic Analysis of λ-opt for Traveling Salesperson Problems

奈良先端科学技術大学院大学博士(工学)doctoral thesi

五先生の御退職に際して

departmental bulletin pape

タブレット操作ログによる受講態度の取得とその解析

application/pdf三重大学大学院 工学研究科 博士前期課程 電気電子工学専攻38pthesi

Lanthanide tetrad effect of Naegi granite-pegmatite suite, central Japan : Convex tetrad effect by fractional loss of fluid from hydrous felsic melt

2007The Late Cretaceous (ca. 67 Ma) Naegi granite-pegmatite suite in Nakatsugawa City, Gifu Prefecture, central Japan, has been studied in view of the lanthanide tetrad effect in evolved felsic rocks. The pegmatite occurring sparsely in the granite body as small patches (<20 cm) and the matrix granite were sampled. REE including Y, major and some minor elements in the samples have been determined. The REE data for mineral separates (quartz, plagioclase, K-feldspar, biotite, and residual heavy minerals) from a granite sample have also been obtained. The chondrite-normalized REE patterns for pegmatite and granite commonly show convex tetrad effects and huge negative Eu anomalies of Eu/Eu^*=0.02-0.004 but no notable Y/Ho fractionation. The whole-rock sample of granite and its mineral separates show similar convex tetrad effects, suggesting the convex tetrad effect in the original magma before crystallization. The granite and pegmatite show no significant differences in major element chemistry and mineralogy except mineral size and texture, but the pegmatite is depleted in Eu, Sr, and Ba relative to the granite. In addition, the pegmatite exhibits a convex tetrad effect and a fairly large negative Eu anomaly, when normalized by the granite. The field occurrence of pegmatite suggests a heterogeneous distribution of aqueous fluid inside of the granitic magma, which is possibly related to the unmixing phenomenon of fluid and silicate melt. Here is proposed a simple model of fractional loss of fluid from hydrous felsic melt. Applying the model to the observed REE fractionation between pegmatite and host granite pairs, REE partition coefficients between aqueous fluid and melt, K_d(REE: fluid/melt), have been evaluated. The logK_d(REE: fluid/melt) values indeed exhibit small concave tetrad effects, positive Eu anomalies, and light REE enrichment trends. Fractional loss of fluid from a hydrous felsic melt system leaves residual silicates in which the small concave tetrad effect and positive Eu anomaly of logKd(REE: fluid/melt) can be exaggerated in reversed manners. As a result, the residual silicates acquire pronounced convex tetrad effects and huge negative Eu anomalies.国立情報学研究所で電子化したコンテンツを使用している。departmental bulletin pape

Femoral BMD and serum markers of bone turnover in mice infused for 21 days.

<p><b>A.</b> BMD was measured <i>in vivo</i> at beginning and end of infusion with vehicle or PTH in WT and <i>Cox2</i> KO mice and the percent change calculated relative to the beginning BMD for each mouse. <b>B, C.</b> Serum parameters for bone formation (osteocalcin) and bone resorption (CTX) were measured at the end of study. Bars are means ± SEM for 6 WT and 6 KO mice infused with vehicle and 7 WT and 7 KO infused with PTH. ^aSignificant effect of PTH, p<0.01; ^bp<0.05. ^cSignificant effect of genotype, p<0.01.</p

Body weight and serum calcium (Ca) in 3-mo old wild type (WT) and <i>Cox2</i> KO mice infused with vehicle or PTH for 21 days.

<p>Data are means ± SEM for (n) mice.</p><p>^aSignificant effect of PTH, p<0.01.</p><p>^bSignificant effect of genotype, p<0.01,</p><p>^cp<0.05.</p><p>Body weight and serum calcium (Ca) in 3-mo old wild type (WT) and <i>Cox2</i> KO mice infused with vehicle or PTH for 21 days.</p

Morphometry of femoral trabecular bone and L3 vertebrae in mice infused for 21 days.

<p><b>A.</b> Representative μCT images (top panel) and morphometric analyses (bottom panel) of trabecular bone in the metaphyseal region of distal femur. <b>B.</b> Representative μCT images (top panel) and morphometric analyses (bottom panel) of trabecular bone in L3 vertebrae. Bars are means ± SEM for 6 WT and 6 KO mice infused with vehicle and 7 WT and 7 KO mice infused with PTH. ^aSignificant effect of PTH, p<0.01; ^bp<0.05. ^cSignificant effect of genotype, p<0.01. <b>C</b>. Representative μCT cross-sectional images of midshaft of femurs.</p

Morphometry of femoral bone and L3 vertebral bone in mice infused for 12 days.

<p><b>A.</b> Representative μCT longitudinal images (top panel) and morphometric analyses (bottom panel) of trabecular bone in the metaphyseal region of distal femur. Bars are means ± SEM for 7 WT and 7 KO mice treated with vehicle and 8 WT and 8 KO mice treated with PTH. <b>B</b>. Representative μCT cross-sectional images (top panel) and morphometric analyses (bottom panel) of trabecular bone in the L3 vertebrae. Bars are means ± SEM for 7 WT and 7 KO mice treated with vehicle and 8 WT and 8 KO mice treated with PTH. <b>C</b>. Representative μCT cross-sectional images of midshaft of femurs. ^aSignificant effect of PTH, p<0.01; ^bp<0.05. ^cSignificant effect of genotype, p<0.01; ^dp<0.05.</p