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Yuan, X.*; Hu, Q. H.*; Fang, X.*; Wang, Q. M.*; Ma, Y.*; 舘 幸男
Sedimentary Geology, 465, p.106633_1 - 106633_14, 2024/05
Archie's cementation factor, m, is a critical parameter for petrophysical studies, and the value is influenced by several factors such as the shape, type, and size of grains, degrees of diagenesis, and associated pore structure. Using integrated experimental and theoretical approaches, the goal of this study is to obtain the cementation factor of rocks (both reservoir rock and caprock) and assess the impact of diagenesis processes on the values of the cementation factor. Thirteen samples of geologically diverse rocks (six mudstones, four fossiliferous limestones, two marbles, and one sandstone) were selected to achieve these research objectives. Two approaches, the diffusion of gas tracers and the Bosanquet formula calculation using pore-throat sizes from mercury intrusion porosimetry analyses, were used to derive the cementation factors of these rock samples. These rocks were categorized into two groups based on the correlation between average pore-throat diameter and diffusivity, and an exponential-law relationship between the cementation factor and porosity was determined for these sample groups. In addition, thin-section petrography and field emission-scanning electron microscopy observations were utilized to investigate diagenetic processes, with four diagenetic patterns being established: (1) strong compaction, strong cementation, and weak dissolution-diagenesis pattern; (2) weak compaction, medium cementation, and weak dissolution-diagenesis pattern; (3) weak compaction, medium cementation, and strong dissolution-diagenesis pattern; and (4) fracture-matrix pattern. The results indicated that diagenetic processes and microfractures contribute to the variability in the cementation factors in these rock samples.
Hu, Q.*; Wang, Q. M.*; Zhang, T.*; Zhao, C.*; Iltaf, K. H.*; Liu, S. Q.*; 深津 勇太
Energy Reports (Internet), 9, p.3661 - 3682, 2023/12
被引用回数：4 パーセンタイル：78.27(Energy & Fuels)This study evaluates petrophysical properties of representative geological rocks in the context of injectivity, storage space, and caprock integrity for effective utilization and long-term storage of carbon dioxide. A total of 10 geological rocks were selected as representative storage media for consideration as saline aquifers & depleted oil and gas reservoirs, basalts, and cap rocks, as well as utilization in organic-rich shale and coal seams. An integrated suite of laboratory tests, including liquid immersion porosimetry, gas expansion porosimetry, grain size distribution, mercury intrusion porosimetry, and gas diffusion, were performed on these various rock samples. The results exhibit a disparity of petrophysical properties among two broad groups of rocks: rocks selected for possible storage of CO
have porosities of 
10-25%, permeabilities of 10
-10
m
, 
m-sized pore-throat size distribution, and mostly good pore connectivity; in contrast, the potential caprocks have porosities of 0.5-5%, permeabilities of 10
-10
m, pore throat sizes of 
50 nm, and probably poorly connected pore networks. An understanding of the measured facets of pore structure and contribution of fractures is also critical in the context of different testing principles and data interpretation of petrophysical analyses, as well as observational scales in the laboratory and field, and therefore reliable confidence of CO storage and utilization performance. Our work further illustrates the controlling influence of grain size distribution and geological processes on pore size distribution and pore connectivity for a wide range of rock types and lithologies, and particularly presents the extent and behavior of CO gas diffusion with a custom-designed apparatus for a holistic understanding of various petrophysical attributes of widely different geological rocks.
Fe
intermetallic compoundCao, Y.*; Zhou, H.*; Khmelevskyi, S.*; Lin, K.*; Avdeev, M.*; Wang, C.-W.*; Wang, B.*; Hu, F.*; 加藤 健一*; 服部 高典; et al.
Chemistry of Materials, 35(8), p.3249 - 3255, 2023/04
被引用回数：1 パーセンタイル：40.78(Chemistry, Physical)静水圧や化学圧力は、結晶構造を変化させる効率的な刺激であり、材料科学において電気的、磁気的特性のチューニングによく利用されている。しかし、化学圧力は定量化が困難であり、これら両者の定量的な対応関係はまだよくわかっていない。本研究では、負の熱膨張(NTE)を持つ永久磁石の候補である金属間化合物を調べた。放射光X線その場観察により、AlをドープしたHoFeに負の化学圧力があることを明らかにし、単位セル体積の温度・圧力依存性を用いそれを定量的に評価した。また、磁化測定と中性子回折測定を組み合わせることで、磁気秩序に対する化学圧力と静水圧の違いを比較した。興味深いことに、圧力はNTEの抑制と増強を制御するために使用することができた。電子状態計算から、圧力がFermiレベル(EF)に対する主要バンドの上部に影響を与えたことを示しており、これは磁気安定性に影響を与え、それが磁気とNTEを調節する上で重要な役割を果たしていることがわかった。本研究は、圧力の影響を理解し、それを利用して機能性材料の特性を制御する良い例を示している。
Zhang, W. Q.*; 山口 敏男*; Fang, C. H.*; 吉田 亨次*; Zhou, Y. Q.*; Zhu, F. Y.*; 町田 真一*; 服部 高典; Li, W.*
Journal of Molecular Liquids, 348, p.118080_1 - 118080_11, 2022/02
被引用回数：2 パーセンタイル：30.05(Chemistry, Physical)3mol/kgのRbCl水溶液におけるイオンの水和・会合と水素結合した水の構造を、298K/0.1MPa, 298K/1GPa, 523K/1GPa, 523K/4GPaにおける中性子回折と経験的ポテンシャル構造精密化モデリングにより調べた。その結果、構造パラメータは温度と圧力に依存していることがわかった。高圧・高温条件では、Rb
とCl
の第二水和層がより明確になる。第一水和層におけるRbの平均酸素配位数は、配位距離を0.290nmから0.288nmに縮めながら、常圧では6.3だったのが、4GPaでは8.9に増加した。第一水和シェルのClの平均酸素配位数は、常圧で5.9、4GPaで9.1と圧力により増加し、対応する配位距離は0.322nmから0.314nmへと減少した。Rbと中心の水分子の第一溶媒和シェルにおける水双極子の配向は圧力に敏感であるが、Clの第一溶媒和シェルにおける水双極子の配向は温度圧力によらずあまり変化しなかった。Rb-Clの隣接イオンペアの数は、温度が高くなると減少し、圧力が高くなると増加する。水分子は密に詰まっており、極限状態では水分子の四面体水素結合ネットワークはもはや存在しない。
Fe(n,
)
Fe cross section from the surrogate ratio method and its effect on the Fe nucleosynthesisYan, S. Q.*; Li, X. Y.*; 西尾 勝久; Lugaro, M.*; Li, Z. H.*; 牧井 宏之; Pignatari, M.*; Wang, Y. B.*; Orlandi, R.; 廣瀬 健太郎; et al.
Astrophysical Journal, 919(2), p.84_1 - 84_7, 2021/10
被引用回数：1 パーセンタイル：8.24(Astronomy & Astrophysics)The long-lived Fe (with a half-life of 2.62 Myr) is a crucial diagnostic of active nucleosynthesis in the Milky Way galaxy and in supernovae near the solar system. The neutron-capture reaction Fe(n,)Fe on Fe (half-life=44.5 days) is the key reaction for the production of Fe in massive stars. This reaction cross section has been previously constrained by the Coulomb dissociation experiment, which offered partial constraint on the E1 -ray strength function but a negligible constraint on the M1 and E2 components. In this work, for the first time, we use the surrogate ratio method to experimentally determine the Fe(n,)Fe cross sections in which all the components are included. We derived a Maxwellian-averaged cross section of 27.5
3.5 mb at 
= 30 keV and 13.41.7 mb at = 90 keV, roughly 10%-20% higher than previous estimates. We analyzed the impact of our new reaction rates in nucleosynthesis models of massive stars and found that uncertainties in the production of Fe from the Fe(n,)Fe rate are at most 25
. We conclude that stellar physics uncertainties now play a major role in the accurate evaluation of the stellar production of Fe.
Kong, L.*; Gong, J.*; Hu, Q.*; Capitani, F.*; Celeste, A.*; 服部 高典; 佐野 亜沙美; Li, N.*; Yang, W.*; Liu, G.*; et al.
Advanced Functional Materials, 31(9), p.2009131_1 - 2009131_12, 2021/02
被引用回数：23 パーセンタイル：81.42(Chemistry, Multidisciplinary)有機-無機ハロゲン化物ペロブスカイトは非常に柔らかいために、圧力などの外部刺激により格子定数を容易に変化させることができ、有用な光電特性を引き出すのに有効である。一方でこの特性は、多少の加圧でも、格子を歪ませてしまい、光と物質の相互作用を弱め、それによる性能の低下を引き起こす。そこで本研究では、代表的な物質であるヨウ化メチルアンモニウム鉛に対して圧力効果および同位体効果を調べ、それらが格子歪を抑制することが分かった。このことは、それらが、これまで得られなかったような光学的,機械的特性を持つ物質を得る手段として有効であることを示している。
Hu, Q.*; Wang, Q. M.*; Zhao, C.*; Zhang, T.*; Iltaf, H.*; 舘 幸男; 深津 勇太
no journal, ,
Fine-grained and clay-rich mudrocks play an important role in the long-term performance of a geological repository for storing high-level nuclear wastes and petroleum production in shale formations. However, low-permeability mudrocks whose pores are poorly interconnected are known to have anomalous diffusion properties that strongly impact long-term net diffusion. The complex pore structure involving predominantly nano-sized pore space is related to compaction and diagenesis from the maturation process of organic matter-rich mudrocks at deep depths, leading to a much smaller effective porosity. Working with various clay minerals, shallow clayey sediments of Wakkanai formation around Horonobe URL in Japan and Opalinus clay of Mt. Terri URL in Switzerland, as well as various deep shales (Barnett, Eagle Ford and Wolfcamp from Texas), using a wide range of sample sizes, this multi-approach and -scale work utilizes a complementary suite of techniques for pore structure characterization (e.g., mercury intrusion porosimetry, small angle X-ray/neutron scattering, scanning electron microscopy), gas diffusion, batch sorption and column transport. The experimental results show that deep mudrocks has a much poor pore connectivity than the shallow ones, and the effective porosity, diffusion coefficients, sorption coefficients are also dependent upon the sample sizes used in the measurement.
Hu, Q. H.*; Zhang, T.*; Shen, Y. Q.*; 舘 幸男; 深津 勇太; Borglin, S.*; Chang, C.*; Hampton, J.*
no journal, ,
In a deep geological repository of high-level nuclear wastes, the near-field systems consist of waste packages, buffer materials, and natural barrier systems. It is expected that the initial thermal loading after waste emplacement will last several hundred years. It is important to investigate the effects of this thermal loading on the near-field components under in situ stress conditions, in terms of thermal-hydrological-mechanical-chemical (THMC) processes and subsequent radionuclide retention and migration. Preliminary tests have been performed via integrated combinations of buffer materials and host rocks, at nm-dm scales, subjected to a range of elevated temperatures under true-triaxial conditions, which is complemented by a suite of nano-petrophysical characterization approaches such as small-angle neutron/X-ray scattering techniques to quantify total pore space and sample size-dependent effective porosity. For multiple-approach radionuclide retention and migration tests before- and after-THMC experiments, a complementary range of tests will include batch, column, and gas diffusion for granular samples, as well as gas/liquid diffusion and fractured core transport tests for intact rock samples under different temperature and pressure conditions.
亀島 敬; 小瀧 秀行; 神門 正城; 大東 出; 川瀬 啓悟; 福田 祐仁; Chen, L. M.*; 本間 隆之; 近藤 修司; Esirkepov, T. Z.; et al.
no journal, ,
レーザープラズマ電子加速は非常に高い電場を持っているが、加速空間が非常に短いという問題点を持っているため、その電子ビームの加速エネルギーは100MeV程度に制限されていた。近年、このレーザープラズマ電子加速が抱える問題点をキャピラリー放電管を用いることで大幅に解決がなされた。プラズマは密度が高いほど屈折率が低くなる特徴を利用して放電管の中でプラズマ密度を中心で薄く、その外周を高く分布させれば光ファイバーと同じ原理でレーザーは放電管内のプラズマ中を集光伝搬しながら相互作用する。ゆえに、加速空間を大幅に拡張することができる。この実験を2006年に中国工程物理研究院とKEK、及び原子力機構で共同実験を行い、キャピラリ放電管を用いて4.4Jのレーザーパルスの集光伝搬及び0.56GeVの電子ビームの生成に成功した。加えて、JAEAにて同様の実験を2007年に行い、1Jのレーザーパルスの集光伝搬及び電子ビームの発生に成功した。
