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THE DESIGN OF KNEE JOINTS FOR RIGID STEEL FRAMES WITH THIN WALLED SECTION 薄壁型钢刚架膝关节的设计
Pub Date : 1968-05-20 DOI: 10.2208/JSCEJ1949.1968.153_1
T. Okumura, N. Ishizawa
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引用次数: 4
ANALYSIS OF SNOW DEPTH DISTRIBUTION ON AERIAL PHOTOGRAPHS 航拍积雪深度分布分析
Pub Date : 1968-05-20 DOI: 10.2208/JSCEJ1949.1968.153_41
T. Maruyasu, M. Uchida, H. Taura
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引用次数: 0
ANALYSIS OF GRID WORKS AND ORTHOTROPIC PLATES ON WINKLER-TYPE FOUNDATIONS 温克尔型基础的格网及正交各向异性板分析
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_26
T. Kusama
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引用次数: 1
A STUDY ON THE MINIMUM THICKNESS-TO-DEPTH RATIO OF PLATE GIRDER WEBS 板梁腹板最小厚深比研究
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_9
H. Yonezawa, I. Mikami
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引用次数: 0
ON ELONGATION CAPACITY OF STRUCTURAL STEEL PLATES 浅谈结构钢板的伸长率
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_34
T. Okumura, K. Horikawa
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引用次数: 1
PRACTICAL FORMULAS FOR CURVED BOX GIRDER BRIDGE 弯箱梁桥实用计算公式
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_45
R. Komatsu, Masa Hayashi
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引用次数: 0
ON THE STATIC AND DYNAMIC PROPERTIE'S OF EPOXY RESIN 环氧树脂的静、动态性能研究
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_1
Y. Niwa, M. Sato
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引用次数: 1
YIELDED PATTERNS IN THE STRUCTURAL STEEL MEMBERS (PHOTOELASTIC COATING STUDY) 结构钢构件的屈服图样(光弹性涂层研究)
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_16
Tutomu Usami, T. Kawamoto, Y. Fukumoto
鋼構造物 の極 限強度 は,通 常,構 成す る構造部材 の一 部 が荷重 によ り弾性 限を こえて塑性 域 に入 り,構 造 物 の 剛性 が低下す る結果 ひきおこ され る座 屈,不 安定現象, 過度 の塑性変形 な どに より決め られ る。 構造 物 の挙動 が弾性 限をこえて塑 性域に入 ると,構 造 物 の荷重一変形 関係 を忠 実に追跡 してい くことは,面 倒 な数値計算 を含 む困難 な問題 にな って くる。平 面骨組構 造物 がその面 内で過度 の塑性 変形 を生 じ,つ い には崩壊 にい たる場合,全 塑 性曲げモー メン トに達 した断面 に塑 性 ヒンジが形成 された とみな し,部 材 に発生す る弾塑性 域 の拡 が りを考 えないで解 くのが単 純塑性解析 による塑 性設計法 である。この方法 では,崩 壊 にいた るまでの厳 密 な荷重 一変形性 状を求 め ることはで きない。非弾 性域 で の構造物 の荷重 一変形性 状を厳密に もとめるには,そ れ ぞれ の荷重段 階に対応 して,部 材に発生す る塑性領域 を求 めるのであるが,力 のつ り合 い条件,変 形の適合条 件 を同時 に満 足 させ ようとす るには,ど うして もtria1and-errorに よる計算)手法が要求 され る。 部材 に発生す る弾塑性境界 は使 用材料の降伏条件式 か ら求 め られるが,こ れは弾性応 力,ま たは弾性ひずみが 降伏 関数
钢结构的极限强度,通常是指构造的结构件的一部分因负荷而超过弹性极限进入塑性区,导致构造的刚性降低而引起的座屈。由稳定现象,过度的塑性变形等决定。如果构造物的行为超过弹性界限而进入塑性区域,那么忠实地追踪构造物的荷载一变形关系就会成为包含表面的数值计算在内的困难的问题。平面骨架结构在其面内产生过度的塑性变形,以至崩溃时,可视为在达到全塑弯曲摩门特的断面上形成塑性铰链,部材中发生的弹塑性域的扩大不考虑解的是根据单纯塑性解析的塑性设计法。用这个方法,到坍塌为止的紧密的负荷一变形状求不出来。为了严格求出非弹性区域的构造物的受力一变形状态,要求出与各受力阶段对应的部材产生的塑性区域,力的匹配条件,变形的匹配条要同时满件,无论如何都要求采用tria1and-error的计算)方法。发生在构件上的弹塑性边界是从所用材料的屈服条件式求出的,这是弹性应力或弹性形变屈服函数
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引用次数: 0
STUDY ON SETTLEMENT ASSOCIATED WITH LIQUEFACTION OF SAND SUBJECTED TO IMPACT LOADS 冲击荷载作用下砂土液化沉降研究
Pub Date : 1968-04-20 DOI: 10.2208/JSCEJ1949.1968.152_39
K. Tanimoto, M. Nishi
quakes resulted in severe damage to engineering works. Extensive laboratory investigations1)-10) on this liquefaction phenomenon have been conducted by many soil engineers for many years, especially since the Niigata earthquake of 1964 which provided much valuable information of this phenomenon. Some important conclusions have been obtained, on the necessary combination of soil conditions and vibratory deformations leading to liquefaction and on the liquefaction process, from these studies. Unfortunately only a few attempts, however, seem to have been made to study this phenomenon in a quantitative way. Ref. 9) may be one of such works of solving case problem in Niigata. The present
地震对工程造成了严重破坏。多年来,许多土壤工程师对这种液化现象进行了广泛的实验室研究,特别是自1964年新泻地震以来,对这种现象提供了许多有价值的信息。从这些研究中获得了一些重要的结论,即土壤条件和振动变形导致液化的必要组合以及液化过程。然而,不幸的是,似乎只有少数人试图以定量的方式研究这一现象。参考文献9)可能是新泻地区解决案例问题的此类著作之一。目前的
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引用次数: 0
EXPERIMENTAL ESTIMATION OF DETENTION IN STORM SEWER SYSTEM 雨排水系统滞留的实验估计
Pub Date : 1968-03-20 DOI: 10.2208/JSCEJ1949.1968.151_47
T. Sueishi, A. Katsuya
In this paper, the results of experimental study on the storm runoff in urban area were described. The former investigations have been performed mainly based on theories or practical observations. The practical survey, however, is extremely difficult because of the problems of provision for sudden storm, scarcety of design storm occurrence and also the selection of proper gauge station in sewers. These difficulties may be the principal reasons why the progress of investigations of urban storm runoff is so slow. The model configuration of sewer system is not unable because the drainage area and sewer include comparatively many artificial elements. The present laboratory model herein used is only the system model of storm-plain basin-single sewer and will not be sufficient for the complete study, but would make a step further toward the better model to study the storm detention and runoff. The results of the present investigation will be summarized as follows.i) It was pointed out that the phenomena called as the flow detention, retardation, storage and flooding were the hydraulically identical phenomena and might be called “detention” in a wide sense. The detention formula may be available for the estimation of depression rate X for drainage pump capacity, provided that limits for b in Talbot's formula and the length of sewer are carefully selected, but the theoretical depression rate would become X'( = √ 2 X). The detention coefficient α is of different significance hydraulically from X and several questions are remained concerning with the theoretical procedure.ii) Experiments were made for the sewer slopes of 1/200 and 1/1 000. Applying the rational method, the rate of runoff becomes the maximum more rapidly than the actual. Sewer section design, therefore, is in safety side. The hydrograph agrees comparatively well with the actual one in case of the steep slope sewer if the roughness is selected properly. But the hydrograph is much different in the gentle slope, and the correction is difficult in the practical range of the roughness. This fact is ascribed to the so called natural detention and suggests that the Manning's formula which is the equation of motion of the rational method is no longer established in the gentle slope. If this detention is evaluated experimentally by the term of detention coefficient α, α becomes 1.30 in the slope of 1/1 000 but is unity in 1/200, so that α should be understood as the correction factor representing the difference between the hydrographs by the rational method and the actual one.iii) Any of control structure is understood to have the negative effects upon the capacity of dynamic storage except when the flooding in lower area is concerned or when the drainage pump capacity is designed to be depressed.iv) When the storage function method is used, the calculated hydrograph for steep slope agrees with the actual hydrograph. In the gentle slope area, the hydrograph is also not so good to be fitted. This met
本文介绍了城市暴雨径流的试验研究结果。以前的调查主要是根据理论或实际观察进行的。然而,由于暴雨的准备、设计暴雨发生的稀缺性以及在下水道中选择合适的测量站等问题,使实际调查工作极为困难。这些困难可能是城市暴雨径流调查进展缓慢的主要原因。由于排水区域和下水道中包含较多的人工因素,因此不能对下水道系统进行模型配置。本文所采用的实验室模型仅为暴雨平原流域-单沟渠系统模型,尚不足以进行完整的研究,但可以向更好的暴雨滞留和径流研究模型迈进一步。本文的研究结果总结如下:1)指出,所谓的流阻、滞流、蓄流和泛流现象是水力学上相同的现象,可以在广义上称为“滞流”。如果仔细选择塔尔博特公式中b的极限和下水道长度,则可以使用滞留公式来估计排水泵容量的下降率X,但理论上的下降率将成为X'(=√2 X)。滞留系数α与X在水力上的意义不同,并且在理论过程中还存在几个问题。ii)对1/200和1/ 1000的下水道坡度进行了实验。应用合理的方法,径流量达到最大值的速度比实际更快。因此,污水段的设计是在安全方面。在陡坡沟渠中,如果选择适当的粗糙度,所得的水文曲线与实际情况吻合较好。但在坡度较缓的地形上,其水文曲线差异较大,在粗糙度的实际范围内很难进行校正。这一事实归因于所谓的自然滞留,并表明曼宁公式即理性方法的运动方程在缓坡中不再成立。如果实验用滞留系数α项来评价这种滞留,则α在1/1 000的斜率上变为1.30,但在1/200的斜率上是统一的。因此,α应理解为用合理方法得到的线线与实际线线之差的修正系数。iii)任何控制结构对动态库容的负面影响,除考虑下游洪水或设计降低排水泵容量的情况外。iv)采用蓄水函数法时,陡坡的计算线线与实际线线一致。在缓坡地区,水文曲线也不太适于拟合。这种方法在理论上是有局限性的,而且储水系数的确定是相当困难的。5)洪水并不总是随着回归期的增加而发生,因为用合理的方法计算最大径流量时,径流量已趋于稳定。相反,任何考虑滞洪的设计方法计算时,最大径流量并不一定处于稳定状态,洪水必然是随着回归期的增加而发生的。应根据较强降雨造成洪水的可能性来确定恢复周期,以尽量减少成本和损失的总和。
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Transactions of the Japan Society of Civil Engineers
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