Bispectrum and asymmetry of wave shape

Ｂｉｓｐｅｃｔｒｕｍａｎｄａｓｙｍｍｅｔｒｙｏｆｗａｖｅｓｈａｐｅ￥ＤｉｎｇＰｉｎｇｘｉｎｇ；ＫｏｎｇＹａｚｈｅｎ；ａｎｄＳｕｎＦｕ（ＳｔａｔｅＫｅｙＬａｂｏｒａｔｏｒｙＯｆＥｓｔｕａｒｉｎｅａｎｄ￣ａｌＲ￣ｈ，ＩｎｓｔｉｔｕｔｅｏｆＥＳｔｕａｒｉｎ...     

Nonlinear Dynamic Analysis of Flexible Marine-Risers

A nonlinear dynamic analysis model is estabilished on the basis of "lumped mass" approach, which takes the influence of the fluid flow within the pipe into consideration. Numerical results are compared with the published works, and the effects of internal fluid flow, internal pressure, dyanmics as well as the nonlinear characteristics on the behavior of flexible risers are discussed. From this work, some useful conclusions are drawn.     

斜带髭鲷Hapalogenys nitens（Richardson）和横带髭鲷H．mucronatus （Eydoux et Souleyet）的核型

采用ＰＨＡ体内注射肾细胞直接制片法研究青岛近海常见经济鱼类斜带髭鲷和横带髭鲷的核型．得出核型公式前者为：２ｎ＝４８，２ｍ＋８ｓｍ＋２ｓｔ＋３６ｔ，ＮＦ＝５８，后者为２ｎ＝４８，２ｍ＋８ｓｍ＋１４ｓｔ＋２４ｔ，ＮＦ＝５８。斜带钱绸核型中ｔ５和ｔ１６对染色体及横带货绸核型中ｔ７对染色体为具次缢痕的染色体。两种鱼的核型特点符合典型的高位类群鱼类核型特征。     

二倍体与三倍体太平洋牡蛎(Crassostrea gigas)的细胞学比较研究

研究比较了太平洋牡蛎 (Crassostrea gigas)二倍体与三倍体鳃上皮细胞核长轴、外套膜与唇瓣结缔组织中血淋巴核径、直肠上皮细胞高度的大小。结果显示 ,三倍体鳃上皮细胞核长轴、外套膜与唇瓣结缔组织中血淋巴核径显著大于二倍体 (P<0 .0 1) ,而二倍体和三倍体直肠上皮细胞高度没有明显差别。本研究结果支持了多倍体的巨态性假说 ,并揭示了倍性对细胞核大小的影响。     

The morphology and tectonics of the Mark area from Sea Beam and Sea MARC I observations (Mid-Atlantic Ridge 23° N)

High-resolution Sea Beam bathymetry and Sea MARC I side scan sonar data have been obtained in the MARK area, a 100-km-long portion of the Mid-Atlantic Ridge rift valley south of the Kane Fracture Zone. These data reveal a surprisingly complex rift valley structure that is composed of two distinct spreading cells which overlap to create a small, zero-offset transform or discordant zone. The northern spreading cell consists of a magmatically robust, active ridge segment 40–50 km in length that extends from the eastern Kane ridge-transform intersection south to about 23°12′ N. The rift valley in this area is dominated by a large constructional volcanic ridge that creates 200–500 m of relief and is associated with high-temperature hydrothermal activity. The southern spreading cell is characterized by a NNE-trending band of small (50–200 m high), conical volcanos that are built upon relatively old, fissured and sediment-covered lavas, and which in some cases are themselves fissured and faulted. This cell appears to be in a predominantly extensional phase with only small, isolated eruptions. These two spreading cells overlap in an anomalous zone between 23°05′ N and 23°17′ N that lacks a well-developed rift valley or neovolcanic zone, and may represent a slow-spreading ridge analogue to the overlapping spreading centers found at the East Pacific Rise. Despite the complexity of the MARK area, volcanic and tectonic activity appears to be confined to the 10–17 km wide rift valley floor. Block faulting along near-vertical, small-offset normal faults, accompanied by minor amounts of back-tilting (generally less than 5°), begins within a few km of the ridge axis and is largely completed by the time the crust is transported up into the rift valley walls. Features that appear to be constructional volcanic ridges formed in the median valley are preserved largely intact in the rift mountains. Mass-wasting and gullying of scarp faces, and sedimentation which buries low-relief seafloor features, are the major geological processes occurring outside of the rift valley. The morphological and structural heterogeneity within the MARK rift valley and in the flanking rift mountains documented in this study are largely the product of two spreading cells that evolve independently to the interplay between extensional tectonism and episodic variations in magma production rates.     

The continental shelf wave of the East China Sea and its effect on the Kuroshio

The free shelf wave theory is applied to the practical case of the continental shelf in the East China Sea to analyse the effects of the shelf wave on the Kuroshio. The results indicate that the shelf wave in lower frequency travels from north to south and its phase velocity is proportional to the Kuroshio's current velocity) the maximum current velocity of the Kuroshio lies at the continental margin. The analytical solutions obtained indicate that the hydrodynamic characters of the sea region over the shelf present band structure. The horizontal motion ( x -component) caused by the shelf wave at the margin may be one of the causes for generating wavy pattern of the Kuroshio's axis .     

Similarity solution for cavity expansion in thermoplastic soil

This paper presents an analytical solution for cavity expansion in thermoplastic soil considering non‐isothermal conditions. The constitutive relationship of thermoplasticity is described by Laloui's advanced and unified constitutive model for environmental geomechanical thermal effect (ACMEG‐T), which is based on multi‐mechanism plasticity and bounding surface theory. The problem is formulated by incorporating ACMEG‐T into the theoretical framework of cavity expansion, yielding a series of partial differential equations (PDEs). Subsequently, the PDEs are transformed into a system of first‐order ordinary differential equations (ODEs) using a similarity solution technique. Solutions to the response parameters of cavity expansion (stress, excess pore pressure, and displacement) can then be obtained by solving the ODEs numerically using mathematical software. The results suggest that soil temperature has a significant influence on the pressure‐expansion relationships and distributions of stress and excess pore pressure around the cavity wall. The proposed solution quantifies the influence of temperature on cavity expansion for the first time and provides a theoretical framework for predicting thermoplastic soil behavior around the cavity wall. The solution found in this paper can be used as a theoretical tool that can potentially be employed in geotechnical engineering problems, such as thermal cone penetration tests, and nuclear waste disposal problems.     

The July 10, 2020, red-bed landslide triggered by continuous rainfall in Qianxi,Guizhou, China

Landslides - On July 10, 2020, a catastrophic landslide with a slope angle of only 8° occurred in the red-bed series strata in Qianxi, Guizhou, southwestern China, due to prolonged rainfall,...     

Dynamic process analysis of the Xinmo landslide via seismic signal and numerical simulation

Landslides - On 24 June 2017, a rockslide-debris avalanche occurred in Xinmo Village, Maoxian County, Sichuan Province, China. The displaced materials traveled approximately 2.6&nbsp;km and...     

大同矿区5#煤层煤岩煤质特征及其清洁利用方式

大同矿区位于山西省大同市的西南,主要含煤地层为侏罗系大同组和石炭二叠系山西组、太原组,是我国典型的双纪煤田。在收集大同矿区以往勘查资料的基础上,系统分析了大同矿区5#煤层的煤岩煤质特征,煤质主要为中灰、高挥发分、中硫、高热稳定性煤,整体以弱黏结煤为主,煤层的黏结性变化规律受深成变质作用影响,变质程度由低至高,煤的黏结性也随之逐渐增强。5#煤层煤岩特征以半亮-半暗煤为主,镜质组含量较高,以较干燥森林沼泽相和湖沼相为主。绘制了煤质指标的等值线图,研究其分布特征及变化规律,并参照焦化、气化、液化用煤指标体系对5#煤清洁利用方式进行划分,结果显示,5#煤洗选后大部分可作为焦化用煤,部分煤可作为直接液化用煤。