simulation experiment

  • 文章类型: Journal Article
    晶粒尺寸分析用于研究晶粒尺寸和分布。它是沉积模拟实验(SSE)中的关键指标,这有助于了解水动力条件和确定沉积环境的特征。用于基于图像的粒度分析的现有方法主要集中在其中晶粒边缘不同或晶粒排列规则的场景。然而,这些方法不适用于来自SSE的图像。我们提出了一种包含直方图层的深度学习模型,用于分析具有模糊颗粒边缘和不规则排列的SSE图像。首先,ResNet18用于从SSE图像中提取特征。然后将这些特征输入到直方图层中,以获得局部直方图特征,它们被连接起来以形成整个图像的综合直方图特征。最后,将直方图特征连接到完全连接的层,以估计与累积体积百分比相对应的晶粒尺寸.此外,开发了应用工作流。结果表明,所提出的方法比其他八个模型具有更高的精度,并且在实践中与手动结果高度一致。该方法提高了颗粒分布不规则图像的粒度分析效率和准确性,提高了SSE中粒度分析的量化和自动化程度。它也可用于土壤和岩土工程等领域的粒度分析。
    Grain size analysis is used to study grain size and distribution. It is a critical indicator in sedimentary simulation experiments (SSEs), which aids in understanding hydrodynamic conditions and identifying the features of sedimentary environments. Existing methods for grain size analysis based on images primarily focus on scenarios where grain edges are distinct or grain arrangements are regular. However, these methods are not suitable for images from SSEs. We proposed a deep learning model incorporating histogram layers for the analysis of SSE images with fuzzy grain edges and irregular arrangements. Firstly, ResNet18 was used to extract features from SSE images. These features were then input into the histogram layer to obtain local histogram features, which were concatenated to form comprehensive histogram features for the entire image. Finally, the histogram features were connected to a fully connected layer to estimate the grain size corresponding to the cumulative volume percentage. In addition, an applied workflow was developed. The results demonstrate that the proposed method achieved higher accuracy than the eight other models and was highly consistent with manual results in practice. The proposed method enhances the efficiency and accuracy of grain size analysis for images with irregular grain distribution and improves the quantification and automation of grain size analysis in SSEs. It can also be applied for grain size analysis in fields such as soil and geotechnical engineering.
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  • 文章类型: Journal Article
    本研究调查了罕见的冬季晒太阳行为的影响(在林登虫的野生种群中观察到,Pyrrrhocorisapterus)和冬季变暖(通过气候模型预测)对越冬生存和生理的影响。这些昆虫在实验室中暴露于模拟晒太阳和冬季变暖的情景中。部分昆虫在野外半自然条件下暴露于真实的冬天进行比较。结果表明,冬季晒太阳有明显的积极作用,暗示着晒太阳行为对双翅目越冬生存至关重要。相比之下,发现冬季变暖对越冬生存有强烈的负面影响,可能对中欧人口构成威胁。生理参数(质量,含水量,SCP,能量储备)在这项研究中测量并不能完全解释所有的结果。需要进一步研究以更好地了解冬季晒太阳的积极影响和冬季变暖对越冬双翅目的负面影响背后的机制。
    The present study investigates the effects of rare winter basking behavior (observed in wild populations of the Linden bug, Pyrrhocoris apterus) and the effects of winter warming (predicted by climate models) on overwinter survival and physiology of P. apterus. The insects were exposed to scenarios simulating basking and winter warming in the laboratory. Part of the insects were exposed to real winters under semi-natural conditions in the field for comparison. The results show a clear positive effect of winter basking, implying that basking behavior is critical for overwinter survival in P. apterus. In contrast, winter warming was found to have a strong negative effect on overwinter survival, potentially representing a threat to central European populations of P. apterus. Physiological parameters (mass, water content, SCP, energy reserves) measured in this study cannot fully explain all the results. Further study is needed to better understand the mechanisms behind the positive effects of winter basking and the negative effects of winter warming on overwintering P. apterus.
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  • 文章类型: Journal Article
    随着我国城市化进程的加快,城市人口继续增长,导致公共空间频繁拥挤,进而引发交通拥堵甚至安全事故。为了更有效地控制行人流量,提高公共空间的效率和安全性,本实验对传统的动态窗口法(DWA)进行了深入的研究和改进,并将其应用于行人流量的精细控制。具体来说,本研究全面回顾和分析了行人交通流的特点和传统DWA的工作原理。基于此,指出了传统DWA在处理复杂行人流场景方面的不足,并提出了有针对性的改进方案。这种改进方案的核心在于引入了新的评价函数,使DWA能够更准确地平衡决策过程中的各种因素,包括行人移动速度,方向,和空间分布。随后,通过仿真实验验证了改进的DWA。实验场景设置在18m*18m的区域内,与传统的DWA相比,改进的DWA在轨迹长度和行程时间上显示出显著的优势。具体来说,传统DWA机器人的轨迹长度为19.4m,所需时间为34.8s,改进的DWA机器人的轨迹长度缩短为18.7m,时间缩短至18.6s。该结果充分证明了改进的DWA在优化行人流量控制方面的有效性。本研究提出的改进DWA不仅具有很强的科学性,而且在实际应用中表现出很高的效率。本研究对提高城市公共空间的安全性,改善行人交通流状况具有重要的参考价值,为今后行人流量控制技术的进一步发展提供了新的思路。
    With the acceleration of urbanization in China, the urban population continues to grow, leading to frequent occurrences of crowded public spaces, which in turn trigger traffic congestion and even safety accidents. In order to more effectively control pedestrian flow, enhance the efficiency and safety of public spaces, this experiment conducts in-depth research and improvement on the traditional Dynamic Window Approach (DWA), and applies it to the fine control of pedestrian flow. Specifically, this study comprehensively reviews and analyzes the characteristics of pedestrian traffic flow and the working principles of traditional DWA. Based on this, the shortcomings of traditional DWA in dealing with complex pedestrian flow scenarios are identified, and targeted improvement solutions are proposed. The core of this improvement scheme lies in the introduction of a new evaluation function, enabling DWA to more accurately balance various factors in the decision-making process, including pedestrian movement speed, direction, and spatial distribution. Subsequently, the improved DWA is validated through simulation experiments. The experimental scenario is set in an area of 18 m*18 m, and compared with traditional DWA, the improved DWA shows significant advantages in trajectory length and travel time. Specifically, the trajectory length of the traditional DWA robot is 19.4 m, with a required time of 34.8 s, while the trajectory length of the improved DWA robot is shortened to 18.7 m, and the time is reduced to 18.6 s. This result fully demonstrates the effectiveness of the improved DWA in optimizing pedestrian flow control. The improved DWA proposed in this study not only has strong scientific validity but also demonstrates high efficiency in practical applications. This study has important reference value for improving the safety of urban public spaces and improving pedestrian traffic flow conditions, and provides new ideas for the further development of pedestrian flow control technology in the future.
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  • 文章类型: Journal Article
    NASA的毅力和ESA的罗莎琳德·富兰克林探测器的科学目标是寻找火星上古老生命的证据。由于微生物-矿物相互作用而形成的地球化学生物特征可能在实现这一目标方面发挥关键作用,因为它们可以在地球上保存数百万年,火星也是如此.以前的实验室实验已经探索了封闭系统下生物特征的形成,但是这些并不代表在自然火星环境中发现的开放系统,如河道和湖泊。在这项研究中,我们使用全球风化模拟物(OUCM-1)进行了环境模拟实验,热化学模拟的地下水,和厌氧微生物群落,以探索火星上合理的开放和封闭系统中地球化学生物特征的形成。这项初步调查显示,28天后微生物群落的多样性存在差异。在开放系统模拟(流通实验)中,产乙酸杆菌(相对丰度为49%)和硫酸盐还原剂Desulfosporomusa(相对丰度为43%)是优势属。而在批量实验中,硫酸盐还原剂Desulfovibrio,脱硫微生物,和Desulfuromonas(总计95%的相对丰度)占主导地位。我们还发现了在流通实验中矿物质溶解增强的证据,但是几乎没有证据表明生物群中存在二次沉积物。相比之下,在具有生物群的分批实验中,但在非生物条件下却没有形成SiO2和Fe沉积物。这些初始实验的结果表明,在开放和封闭系统之间可以产生不同的地球化学生物特征,因此,开放系统中的生物特征形成值得进一步调查。
    NASA\'s Perseverance and ESA\'s Rosalind Franklin rovers have the scientific goal of searching for evidence of ancient life on Mars. Geochemical biosignatures that form because of microbe-mineral interactions could play a key role in achieving this, as they can be preserved for millions of years on Earth, and the same could be true for Mars. Previous laboratory experiments have explored the formation of biosignatures under closed systems, but these do not represent the open systems that are found in natural martian environments, such as channels and lakes. In this study, we have conducted environmental simulation experiments using a global regolith simulant (OUCM-1), a thermochemically modelled groundwater, and an anaerobic microbial community to explore the formation of geochemical biosignatures within plausible open and closed systems on Mars. This initial investigation showed differences in the diversity of the microbial community developed after 28 days. In an open-system simulation (flow-through experiment), the acetogenic Acetobacterium (49% relative abundance) and the sulfate reducer Desulfosporomusa (43% relative abundance) were the dominant genera. Whereas in the batch experiment, the sulfate reducers Desulfovibrio, Desulfomicrobium, and Desulfuromonas (95% relative abundance in total) were dominant. We also found evidence of enhanced mineral dissolution within the flow-through experiment, but there was little evidence of secondary deposits in the presence of biota. In contrast, SiO2 and Fe deposits formed within the batch experiment with biota but not under abiotic conditions. The results from these initial experiments indicate that different geochemical biosignatures can be generated between open and closed systems, and therefore, biosignature formation in open systems warrants further investigation.
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  • 文章类型: Journal Article
    持续的气候变化和人为压力对昆虫产生了深远的影响,导致物种多样性下降和种群萎缩。昆虫害虫侵入新的地区并引起经济和人类健康问题。冬季的低温被认为是高纬度地区成功定殖的主要障碍之一。气候模型预测,在温带和极地地区,冬季温度将比夏季温度增加更多,可能允许来自温暖气候的物种在高纬度地区定居。了解气候变化将如何影响昆虫的分布对人类活动的许多领域至关重要。一种可能但很少使用的方法来预测由于气候变化导致的昆虫可能的范围变化是通过模拟实验。这里,我介绍并测试了一种方法,以评估在冬季变暖的情况下,温暖地区的昆虫物种在寒冷地区的冬季生存的潜力。该方法基于对冬季变暖的实验室模拟。以地中海害虫为例证明了该方法的适用性,Sesamianonagrioides,评估了其在冬季变暖情况下生存中欧冬季的能力。这里介绍的方法相对简单,估计的准确性可能很高。
    Ongoing climate change and anthropogenic pressure are having a profound influence on insects, causing species diversity to decline and populations to shrink. Insect pests invade new areas and cause economic and human health problems. Low temperatures in winter are thought to be one of the main barriers to the successful colonization of higher latitudes. Climate models predict that winter temperatures will increase more than summer temperatures in temperate and polar regions, potentially allowing species from warmer climates to colonize higher latitudes. Understanding how climate change will affect the distribution of insects is critical to many areas of human activity. One possible but seldom used way to predict likely range shifts of insects due to climate change is through simulation experiments. Here, I present and test a method to assess the potential of insect species from warmer regions to survive winters in colder regions under a warming winter scenario. The method is based on laboratory simulations of warming winters. The applicability of the method is demonstrated using the example of a Mediterranean pest, Sesamia nonagrioides, whose ability to survive Central European winters under a warming winter scenario is assessed. The method presented here is relatively simple, with potentially high accuracy of estimates.
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  • 文章类型: Journal Article
    背景:我们探讨了医疗服务费调整对北京市高血压患者医疗选择的影响。希望为北京市实现分级诊疗提供决策参考。
    方法:根据建模仿真研究的框架,以北京市居民和医疗机构的数据为基础,我们设计了三种居民模型,疾病模型和医院模型。然后,我们构建了患者选择医疗的状态图,并调整了医疗服务费,以观察不同级别医院高血压患者的门诊选择行为,并找到最佳决策方案。
    结果:模拟结果表明,医疗服务费的调整可以在一定程度上影响一,三级医院就医的患者比例,但对二级医院接受治疗的患者比例影响不大。
    结论:北京可以通过降低基层医院的收费标准和稍微提高三级医院的收费标准来调整现行的医疗服务收费标准,这样可以增加基层医院高血压患者的数量。
    BACKGROUND: We explored the impact of medical service fee adjustments on the choice of medical treatment for hypertensive patients in Beijing. We hope to provide decision-making reference to promote the realization of hierarchical diagnosis and treatment in Beijing.
    METHODS: According to the framework of modeling simulation research and based on the data of residents and medical institutions in Beijing, we designed three models of residents model, disease model and hospital model respectively. We then constructed a state map of patients\' selection of medical treatment and adjusted the medical service fee to observe outpatient selection behaviors of hypertensive patients at different levels of hospitals and to find the optimal decision-making plan.
    RESULTS: The simulation results show that the adjustment of medical service fees can affect the proportion of patients seeking medical treatment in primary and tertiary hospitals to a certain extent, but has little effect on the proportion of patients receiving medical treatment in secondary hospitals.
    CONCLUSIONS: Beijing can make adjustments of the current medical service fees by reducing fees in primary hospitals and slightly increasing fees in tertiary hospitals, and in this way could increase the number of patients with hypertension in the primary hospitals.
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  • 文章类型: Journal Article
    粘土水的压实会将含有高浓度铵的孔隙水释放到相邻的含水层中,可能影响地下水铵的浓度。然而,压实过程中铵在粘土中的释放过程和影响效果尚不清楚。进行了四组预实验和两组模拟实验,以揭示粘土质沉积物压实过程中铵的释放机理。(1)模拟连续沉降条件的实验A结果表明,沉积物铵通过离子交换形式的解吸依次转移到孔隙水中,有机物的降解,同时释放矿物结合的铵。孔隙水铵浓度为3.54~8.20mgN/L,由于沉积物铵的转化,具有明显的周期性变化。压实后期较低的含水量(<42.4%)抑制了铵的生物转化,矿物结构的变化导致钾的同构置换捕获铵,导致释放的孔隙水中的铵浓度降低。(2)模拟人工压实条件(如地面沉降)的实验B结果表明,由于孔隙结构和水分含量的变化,孔隙水铵主要是由离子交换形式铵的解吸引起的。孔隙水中铵浓度为4.72~9.91mgN/L,随着短期内压力的大幅变化而显著增加。(3)陈湖湿地的估算结果表明,黏土压实对邻近含水层地下水铵浓度的贡献为2.68-4.29mgN/L,占地下水铵浓度的相当大一部分,远远高于平流和扩散。这项研究的发现揭示了粘土沉积物压实过程中铵的释放机理,其中反应产物可能会影响相邻的含水层。
    Compaction of clayey aquitard would release pore water containing high levels of ammonium to adjacent aquifers, potentially affecting the concentration of groundwater ammonium. However, the releasing process and impact effect of ammonium within clayey aquitard during compaction remain unknown. Four groups of pre-experiments and two groups of simulation experiments were conducted to reveal the releasing mechanism of ammonium during clayey sediment compaction. (1) The results of Experiment A simulating continuous sedimentation conditions showed that the sediment ammonium transferred into pore water sequentially through desorption of ion exchange form, degradation of organic matter, and simultaneous release of mineral-bound ammonium. The concentration of pore water ammonium was 3.54-8.20 mg N/L, with a significant periodical variation due to sediment ammonium transformation. The lower moisture content (<42.4 %) in the later stage of compaction inhibited the biological transformation of ammonium, and the change in mineral structure caused the isomorphic replacement of K to capture ammonium, resulting in a decrease in ammonium concentration in released pore water. (2) The results of Experiment B simulating artificial compaction conditions (such as land subsidence) showed that the pore water ammonium was primarily caused by desorption of ion exchange form ammonium due to changes in pore structure and moisture content. The ammonium concentration in pore water was 4.72-9.91 mg N/L, with a significant increase in response to a large change in pressure in the short term. (3) The estimate results in the Chen Lake wetland suggested that the contribution of clayey aquitard compaction to groundwater ammonium concentration in the adjacent aquifer would be 2.68-4.29 mg N/L, which accounted for a considerable portion of groundwater ammonium concentration and was far higher than that of advection and diffusion. The findings of this study reveal the releasing mechanism of ammonium during clayey sediments compaction, in which reaction products may affect adjacent aquifers.
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  • 文章类型: Journal Article
    X射线显微断层成像(micro-CT)的内部三维特征在青铜腐蚀领域具有巨大的应用潜力。这项工作提出了一种基于原位显微CT图像模拟青铜病的方法,以研究氯化铜(I)和氯化铜(II)二水合物的氧化水解反应的特征。通过在整个实验过程中的三个关键点进行显微CT,获得了一系列高分辨率的重建图像。我们发现,在micro-CT视图中,氯化铜(I)和氯化铜(II)二水合物的反应在模拟的不同阶段表现出不同的特征。这项工作中提出的方法专门模拟了一种单一类型的青铜腐蚀,并表征了模拟青铜病害的演变特征。它为研究青铜病提供了一个新的视角,并可以帮助改善后续使用Micro-CT来区分真实的青铜腐蚀。
    The internal three-dimensional characteristics of X-ray microtomography (micro-CT) has great application potential in the field of bronze corrosion. This work presents a method of simulating bronze disease based on an in situ micro-CT image to study the characteristics of the oxidative hydrolysis reactions of copper(I) chloride and copper(II) chloride dihydrate. A series of high-resolution reconstruction images were obtained by carrying out micro-CT at three key points throughout the experiment. We found that the reactions of copper(I) chloride and copper(II) chloride dihydrate showed different characteristics at different stages of the simulation in the micro-CT view. The method proposed in this work specifically simulated one single type of bronze corrosion and characterized the evolution characteristics of simulated bronze disease. It provides a new perspective to investigate bronze disease and can help improve the subsequent use of micro-CT to distinguish real bronze corrosions.
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  • 文章类型: Journal Article
    芋收获过程受到粒子力学系统和多体动力学系统组成的复杂系统的影响。离散元法(DEM)可以有效解决收割组分与工作材料相互作用的非线性问题。因此,芋分耕植物的离散元模型对于芋收获具有重要意义。本文提出了一种模拟方法,以建立塔罗耕作机的离散单元柔性植物模型和动态夹紧和拉动过程。利用DEM方法建立了芋球茎和柔枝叶柄和叶片的离散元素模型,并建立了芋植物的离散元柔性模型。设计并搭建了Taro夹紧拉力测试平台。以模拟和台架实验采集的夹紧力相关系数和拉力相关系数为实验指标,采用单因素和Plackett-Burman实验确定了模拟参数,优化了芋植物模型。芋植物离散元模型参数标定结果如下:叶柄-叶柄法/切向接触刚度为8.15×109N·m-3,法向/切向临界应力为6.65×106Pa。假茎球茎法的接触刚度为1.22×109N·m-3,法向/切向临界应力为1.18×105Pa,土壤表面能量为4.15×106J·m-3。当拉伸速度为0.1、0.2、0.3、0.4和0.5m·s-1时,模拟实验与台架实验的相关系数分别为0.812、0.850、0.770、0.697和0.652。相关系数的平均值为0.756,表明模拟的离散元工厂模型与真实工厂模型接近。本文建立的芋厂离散元模型具有较高的可靠性。本文的最终目的是通过离散元方法为芋收获机的设计和优化提供模型参考。
    The taro harvesting process is affected by a complex system composed of particle mechanics system and multi-body dynamics system. The discrete element method(DEM) can effectively solve the nonlinear problem of the interaction between harvesting components and working materials. Therefore, the discrete element model of taro tiller plants is of great importance for taro harvesting. This paper proposes a simulation method to establish a discrete element flexible plant model and dynamic clamping and pulling process of taro tiller plant. Discrete Element models of taro corm and flexible tiller petiole and leaf were established using DEM method, and the discrete element flexible model of the taro plant was established. Taro clamping and pulling force testing platform was designed and built. The single factor and Plackett-Burman experiments were used to determine the simulation parameters and optimize the taro plant model by taking the correlation coefficient of clamping force and correlation coefficient of pulling force collected from the simulation and the bench experiment as the experiment index. The parameter calibration results of discrete element model of taro plant are as follows: petiole-petiole method/tangential contact stiffness was 8.15×109 N·m-3, and normal/tangential critical stress was 6.65×106 Pa. The contact stiffness of pseudostem- corm method was 1.22×109 N·m-3, the critical stress of normal/tangential was 1.18×105 Pa, and the energy of soil surface was 4.15×106J·m-3. When the pulling speed is 0.1, 0.2, 0.3, 0.4 and 0.5 m·s-1, the correlation coefficients between the simulation experiment and the bench experiment are 0.812, 0.850, 0.770, 0.697 and 0.652, respectively. The average value of correlation coefficient is 0.756, indicating that the simulated discrete element plant model is close to the real plant model. The discrete element model of taro plant established in this paper has high reliability. The final purpose of this paper is to provide a model reference for the design and optimization of taro harvester by discrete element method.
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  • 文章类型: Journal Article
    位于中高纬度地区的水库冬季冻结数月,其中污染物的积累特征是由于表面冰层的盐排除和底部沉积物的污染释放的叠加影响而改变的。以东北碧流河水库总氮(TN)为例,我们开发了一个模型来模拟冰期(NACISF)中冰和沉积物影响的TN积累特征,以及冰和沉积物对TN的量化贡献。通过实验室冻结模拟实验和沉积物释放通量模拟实验确定了冰和沉积物的模型参数,水质数据是从实地调查中获得的。结果表明,2015-2020年冰封期间TN年平均投入量为220.77t,输出为400.11t,累积量为589.52t。冬季,从冰中排除并从沉积物中释放的TN占总TN输入的8.12%和7.17%,分别。分析表明,冰层中排除的TN与冰层厚度和初始TN浓度呈正相关。碧流河水库的最大冰层厚度具有13年的循环特征,在不同时期,冰排除的TN占总TN输入的比例为10.68%至17.30%(平均13.18%)。同时,TN按季节累积为夏季>秋季>冬季>春季。考虑到气候变化和人类活动的综合影响,2050年的TN排斥效应将会减弱,与目前相比减少了约40.85%。结论是,NACISF模型考虑了冰和沉积物的影响,详细了解了凝固期TN的积累特性,对冬季水质管理具有重要的参考意义。
    Reservoirs located in middle and high latitudes freeze for months in winter, where the accumulation characteristics of pollutants are changed by superimposed influence of salt exclusion from ice on the surface and pollution release from sediments at the bottom. Taking total nitrogen (TN) of Biliuhe reservoir in Northeast China as an example, we developed a model to simulate TN accumulation characteristics influenced by ice and sediments during the freezing period (NACISF), and quantified contributions of TN from ice and sediments. Model parameters of ice and sediments were determined by laboratory freeze-up simulation experiment and sediment release flux simulation experiment, and water quality data were obtained from field investigations. Results showed that the annual average amount of TN input during the ice-covered period from 2015 to 2020 was 220.77 t, the output was 400.11 t, and the accumulated amount was 589.52 t. TN excluded from ice and released from sediments contributed 8.12% and 7.17% of the total TN inputs in winter, respectively. Analysis showed that the TN excluded from ice was positively correlated with ice thickness and initial TN concentration. The maximum ice thickness of Biliuhe reservoir had a 13 year cyclic feature, and the proportion of TN excluded from ice to the total TN inputs in different periods ranged from 10.68% to 17.30% (mean 13.18%). Meanwhile, TN accumulated seasonally as summer > autumn > winter > spring. The TN exclusion effect in 2050 would be weakened when considering the combined effects of climate change and human activities, with a reduction of about 40.85% compared to the current. It is concluded that the NACISF model took into account the influences of both ice and sediments, which provided a detailed understanding of the accumulation characteristics of TN during freezing period, and had important reference significance for water quality management in winter.
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