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951.
This paper presents a constitutive model for time‐dependent behaviour of granular material. The model consists of 2 parts representing the inviscid and viscous behaviour of granular materials. The inviscid part is a rate‐independent hypoplastic constitutive model. The viscous part is represented by a rheological model, which contains a high‐order term denoting the strain acceleration. The proposed model is validated by simulating some element tests on granular soils. Our model is able to model not only the non‐isotach behaviour but also the 3 creep stages, namely, primary, secondary, and tertiary creep, in a unified way. 相似文献
952.
Multiscale simulation of fluvio‐deltaic stratigraphy was used to quantify the elements of the geometry and architectural arrangement of sub‐seismic‐scale fluvial‐to‐shelf sedimentary segments. We conducted numerical experiments of fluvio‐deltaic system evolution by simulating the accommodation‐to‐sediment‐supply (A/S) cycles of varying wavelength and amplitude with the objective to produce synthetic 3‐D stratigraphic records. Post‐processing routines were developed in order to investigate delta lobe architecture in relation to channel‐network evolution throughout A/S cycles, estimate net sediment accumulation rates in 3‐D space, and extract chronostratigraphically constrained lithosomes (or chronosomes) to quantify large‐scale connectivity, that is, the spatial distribution of high net‐to‐gross lithologies. Chronosomes formed under the conditions of channel‐belt aggradation are separated by laterally continuous abandonment surfaces associated with major avulsions and delta‐lobe switches. Chronosomes corresponding to periods in which sea level drops below the inherited shelf break, that is, the youngest portions of the late falling stage systems tract (FSST), form in the virtual absence of major avulsions, owing to the incision in their upstream parts, and thus display purely degradational architecture. Detailed investigation of chronosomes within the late FSST showed that their spatial continuity may be disrupted by higher‐frequency A/S cycles to produce “stranded” sand‐rich bodies encased in shales. Chronosomes formed during early and late falling stage (FSST) demonstrate the highest large‐scale connectivity in their proximal and distal areas, respectively. Lower‐amplitude base level changes, representative of greenhouse periods during which the shelf break is not exposed, increase the magnitude of delta‐lobe switching and favour the development of system‐wide abandonment surfaces, whose expression in real‐world stratigraphy is likely to reflect the intertwined effects of high‐frequency allogenic forcing and differential subsidence. 相似文献
953.
收缩城市住房空置时空分异及影响机制——基于居民用电量视角 总被引:1,自引:0,他引:1
以中国典型的资源型收缩城市——伊春市的伊春区为研究对象,从居民用电量视角对住房空置情况进行判定,同时综合运用核密度估计、网络分析以及问卷访谈等方法,基于区域、居住区、格网3种尺度,对2013—2018年住房空置时空分异格局及影响机制进行深入探究。结果表明:① 伊春区空置住房总量和空置率总体表现为波动上升态势,在国际通行标准下处于“供需基本平衡”状态;② 伊春区住房空置格局在区域尺度、居住区尺度、格网尺度等不同尺度下表现出一定差异性,但各尺度均总体呈现“核心?边缘”的空间分布特点;③ 人口流失、经济支撑、城市功能地位以及居民感知等因素影响伊春区住房空置时序演变,而城市空间开发扩展、住区建设演变、教育医疗设施布局、公共交通可达性等因素共同作用于住房空置的空间分异。 相似文献
954.
Biological invasion poses a huge threat to ecological security.Spartina alterniflora was introduced into China in 1979,and its arrival corresponded with negative effects on native ecosystems.To explore geographical variation of its expansion rate in coastal China,we selected 43 S.alterniflora sites from Tianjin Coastal New Area to Beihai.The area expansion rate,expansion rate paralleling and vertical to the shoreline were analysed based on Landsat images and field survey in 2015.Simple Ocean Data Assimilation(SODA)and climate data were collected to statistically analyse the influential factors of expansion rate.Results showed that significant difference of S.alterniflora area expansion rate among different latitude zones(P<0.01),increasing from 6.08%at southern(21°N–23°N)to 19.87% in Bohai Bay(37°N–39°N)along latitude gradient.There was a significant difference in expansion rate vertical to shoreline in different latitude zones(P<0.01)with the largest occurring in Bohai Bay(256m/yr,37°N–39°N),and showed an decreasing tendency gradually from north to south.No significant difference and latitudinal clines in expansion rate paralleling to shoreline were observed.Expansion rate had significant negative correlation with mean seawater temperature,the lowest seawater temperature,current zonal velocity and meridional velocity and presented a reducing trend as these biotic factors increased;however,they were not significantly correlated with the highest seawater temperature and mean seawater salinity.We identified significant correlations between expansion rate and annual mean temperature,the lowest temperature in January and annual precipitation,but there was little correlation with annual diurnal difference in temperature and the highest temperature in July.The rapid expansion rate in high-latitude China demonstrated a higher risk of potential invasion in the north;dynamic monitoring and control management should be established as soon as possible. 相似文献
955.
我国东部中低山区第四纪冰川的存在与否一直存在争议,但冰川必然对山体进行冰蚀作用形成冰蚀地貌。为了分析我国东部中低山区的山体地貌是否具有冰蚀特征,该文选取了现代冰川集中发育区-喜马拉雅山脉作为冰蚀地貌的研究对象,通过宏观分析,除了由缩口、三角脊、残弧组成的冰斗系统外,还发现冰蚀作用过程存在避谷、吞脊、切壁、穿梁等特殊习性。分析认为冰蚀过程主要受制于雪线高程、积雪高程与坡向坡角三方面因素的控制。以此为基础,对我国东部的江西庐山、山东蒙山、大兴安岭主峰黄岗梁三个地区的山体地貌进行对比分析,发现这些山区的山体地貌与喜马拉雅山脉的冰蚀地貌具有一致性。文章从冰蚀过程的角度确认了我国东部中低山区存在第四纪冰川的事实。 相似文献
956.
局限于仅有观测数据的情况下,利用模拟手段研究土壤风蚀引起的粉尘释放是非常必要的,有助于评估区域土壤风蚀及大气环境质量和气候效应。本文通过分析塔克拉玛干沙漠观测站不同高度层风速及计算平均摩阻风速,利用DPM模型计算粉尘释放通量,综合分析了摩阻风速与粉尘释放通量的相互关系。结果表明:1)不同观测日不同高度层的风速变化各不相同,2m高度层风速的变化范围是0.05~7.73 m·s-1,4m高度层风速的变化范围是0.09~7.19 m·s-1,10m高度层风速的变化范围是0.5~8.09 m·s-1。2)4月1日~4月30日各个观测日24小时内平均摩阻风速分别为0.423 m·s-1、0.344 m·s-1、0.271 m·s-1、0.343 m·s-1、0.161 m·s-1、0.315 m·s-1,其变化范围为0.16~0.42 m·s-1。3)DPM模型研究发现实测跃移通量约为模拟值的122%,模拟值与实测值相关性较好,R2为0.91。上述研究结果对定量评估区域乃至全疆的土壤风蚀对粉尘释放通量的影响具有重要意义。 相似文献
957.
During the pre-summer rainy season, heavy rainfall occurs frequently in South China. Based on polarimetric radar observations, the microphysical characteristics and processes of convective features associated with extreme rainfall rates(ERCFs) are examined. In the regions with high ERCF occurrence frequency, sub-regional differences are found in the lightning flash rate(LFR) distributions. In the region with higher LFRs, the ERCFs have larger volumes of high reflectivity factor above the freezin... 相似文献
958.
局限于仅有观测数据的情况下,利用模拟手段研究土壤风蚀引起的粉尘释放是非常必要的,有助于评估区域土壤风蚀及大气环境质量和气候效应。本文通过分析塔克拉玛干沙漠观测站不同高度层风速及计算平均摩阻风速,利用DPM模型计算粉尘释放通量,综合分析了摩阻风速与粉尘释放通量的相互关系。结果表明:1)不同观测日不同高度层的风速变化各不相同,2m高度层风速的变化范围是0.05~7.73 m·s-1,4m高度层风速的变化范围是0.09~7.19 m·s-1,10m高度层风速的变化范围是0.5~8.09 m·s-1。2)4月1日~4月30日各个观测日24小时内平均摩阻风速分别为0.423 m·s-1、0.344 m·s-1、0.271 m·s-1、0.343 m·s-1、0.161 m·s-1、0.315 m·s-1,其变化范围为0.16~0.42 m·s-1。3)DPM模型研究发现实测跃移通量约为模拟值的122%,模拟值与实测值相关性较好,R2为0.91。上述研究结果对定量评估区域乃至全疆的土壤风蚀对粉尘释放通量的影响具有重要意义。 相似文献
959.
The Digital Elevation Model (DEM) is one of the important parameters of soil erosion assessment and notable uncertainties are found in using different resolutions of the DEM. Revised Universal Soil Loss Equation model has been applied to analyze the effect of open-source DEMs with different resolution and accuracy on the uncertainties of soil erosion modelling in a part of the Narmada river basin in Madhya Pradesh in central India. Selected open-source DEMs are GTOPO30 (1 km), SRTM (30 and 90 m), CARTOSAT (30 m) and ASTER (30 m), used for estimating erosion rate. Results with better accuracy are achieved with the high-resolution DEMs (30 m) with higher vertical accuracy than the coarse resolution DEMs with lower accuracy. This study has presented potential uncertainties introduced by the open-source DEMs in soil erosion modelling for better understanding of appropriate selection and acceptable errors for researchers. 相似文献
960.
随着全球四大卫星导航系统格局的成型,卫星定位系统已从单系统模式发展为如今多系统、多频率融合定位、交互操作的模式。在分析多系统精密单点定位模型及各误差项处理策略的基础上,利用RTKLIB进行GPS,GLONASS,GALILEO,BDS多系统融合精密单点定位试验,并分析其动/静态定位性能。实验结果表明:在单系统空间几何构型较差的情况下,多系统融合精密单点定位较单GPS定位精度可提高20%~40%,收敛时间可缩短35%~50%;在截止高度角超过40°的情况下,单系统会因可见卫星数量不足而无法完成连续定位,而多系统仍能实现高精度的连续定位。这在城区、山区或卫星遮蔽较严重的不利环境中有重要的利用价值。 相似文献