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Energy consumption simulations of rural residential buildings considering differences in energy use behavior among family members

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Building Simulation 2024年第8期17卷 1335-1358页

作者： xi Luo Lina Du School of Building Services Science and Engineering Xi'an University of Architecture and Technology(XAUAT)Xi'an 710055China State Key Laboratory of Green Building Xi'an 710055China

The“average occupant”methodology is widely used in energy consumption simulations of residential buildings;however,it fails to consider the differences in energy use behavior among family *** on a field survey on the Central Shaanxi Plain,to identify the energy use behavior patterns of typical families,a stochastic energy use behavior model considering differences in energy use behavior among family members was proposed,to improve the accuracy of energy consumption simulations of residential *** results indicated that the surveyed rural families could be classified into the following four types depending on specific energy use behavior patterns:families of one elderly couple,families of one middle-aged couple,families of one elderly couple and one child,and families of one couple and one ***,on typical summer days,the results of daily building energy consumption simulation obtained by the“average occupant”methodology were 2..39%and 2.%lower than the simulation results obtained by the model proposed in this study for families of one elderly couple and families of one middle-aged couple,and 13.05%and 2..05%higher for families of one elderly couple and one child,and families of one couple and one *** typical winter days,for the four types of families,the results of daily building energy consumption simulation obtained by the“average occupant”methodology were 2..69%,10.84%,1.2.%,and 8.39%lower than the simulation results obtained by the model proposed in this study,respectively.

关键词： typical energy use behavior pattern differences in occupant behavior building energy consumption simulation stochastic energy use behavior simulation

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Determination of tectonic background for sedimentary basin from sandstone geochemistry

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Chinese Science Bulletin 1998年第14期43卷 1191-1196页

作者： SHAO Lei 1, K. Stattegger 2.and LI Wenhou 3 1. Laboratory of Marine geology, Tongji university, Shanghai 2.0092.{2. 2. Geological and Paleontological Institute, university of Kiel, 2.118 Kiel, Germany 3. Department of geology, northwest Unive Laboratory of Marine geology Tongji University Shanghai China Geological and Paleontological Institute University of Kiel Kiel Germany Department of geology Northwest University Xi’an China

The chemical composition of sedimentary rocks is mainly controlled by source rocks. Through examining chemical composition of terrigenous rocks, the tectonic evolution of a sedimentary basin can be modeled. The Turpan Basin belongs to a continental sedimentary basin and its source rocks are derived from the upper continental crust.

关键词： sedimentary rock geochemistry basin analysis Turpan Basin.

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Geochronological evidence of Indosinian(high-pressure) metamorphic event and its tectonic significance in Taxkorgan area of the Western Kunlun Mountains,NW china

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Science china Earth Sciences 2010年第10期53卷 1445-1459页

作者： YANG WenQiang1,LIU Liang1,CAO YuTing1,WANG Chao1,2.HE ShiPing2.LI RongShe2.& ZHU xiaoHui1 1 State Key Laboratory of Continental Dynamics,Department of geology,northwest {2.,xi’an 710069,china 2.xi’an Institute of geology and Mineral Resource,xi’an 710054,china 1. State Key Laboratory of Continental Dynamics Department of Geology Northwest University Xi’an 710069 China2. Xi’an Institute of Geology and Mineral Resource Xi’an 710054 China

The CL images,LA-ICP-MS in situ trace elements analysis,and U-Pb dating for zircons indicate that the metamorphic ages of the sillimanite-garnet-biotite gneiss and the garnet-amphibole gneiss from eastern Taxkorgan of the Western Kunlun Mountains are 2.0±2.and 2.0±3 Ma respectively,and their protolith ages are younger than 2.3±2.and 480±8 Ma *** samples were collected at the same outcrops with HP mafic granulite and HP pelitic *** assemblage of the sillimanite-garnet-biotite gneiss(Grt+Sill+Per+Q) is consistent with that of HP pelitic granulite at early high amphibolite-granulite facies *** assemblage of the garnet-amphibole gneiss(Grt+Amp+Pl+Q) is consistent with retro-metamorphic assemblage of HP mafic granulite at amphibolite facies *** dating results suggest that these HP granulites underwent peak metamorphism at 2.0±2.to 2.3±2.***,the Kangxiwar tectonic zone was probably formed by subduction and collision of the Paleo-Tethys Ocean during *** ages of the two samples,together with previously published U-Pb zircon dating age,suggest that the sillimanite-garnet schist-quartzite unit is a late Paleozoic unit,not a part of the Paleoproterozoic Bulunkuole Group.

关键词： Western Kunlun Mountains LA-ICP-MS zircon dating Bulunkuole Group Indosinian Kangxiwar tectonic zone

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On the Mean Value Formula of Dedekind Sums

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Acta Mathematica Sinica,English Series 1999年第2期15卷 245-254页

作者： xiali He Wenpeng Zhang, Department of Mathematics, northwest university, xi’an 710069, P. R.{2. Department of Mathematics Northwest University Xi’an P. R. China

The main purpose of this paper is to use the mean value theorem of the Dirichlet L-function to study the distribution property of Dedekind sums, and to give a sharper mean value formula.

关键词： Dedekind sums Distribution of the mean value Asymptotic formula

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Pairwise entanglement and local polarization of Heisenberg model

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Science china(Physics,Mechanics & Astronomy) 2008年第10期51卷 1515-1522页

作者： xi xiaoQiang1,2. ZHANG Tao3, YUE RuiHong3,4 & LIU WuMing2.1 Department of Applied Mathematics and Physics, xi’an Institute of Post and Telecommunications, xi’an 710061, china 2.Beijing National Laboratory for Condensed Matter Physics, Institute of Physics, Chinese Academy of Sciences, Beijing 100080, china 3 Institute of Modern Physics,{2., xi’an 710069, china 4 Department of Physics, Ningbo university, Ningbo 3152.1, china Department of Applied Mathematics and Physics Xi’an Institute of Post and Telecommunications Xi’an 710061 China Beijing National Laboratory for Condensed Matter Physics Institute of Physics Chinese Academy of Sciences Beijing 100080 China Institute of Modern Physics Northwest University Xi’an 710069 China Department of Physics Ningbo University Ningbo 315211 China

The characteristics of pairwise entanglement and local polarization (LP) are dis-cussed by studying the ground state (states) of the Heisenberg XX model. The re-sults show that: the ground state (states) is (are) composed of the micro states with the minimal polarization (0 for even qubit and 1/2.for odd qubit); LP and the prob-ability of the micro state have an intimate relation, i.e. the stronger the LP, the smaller the probability, and the same LP corresponds to the same probability; the pairwise entanglement of the ground state is the biggest in all eigenvectors. It is found that the pairwise entanglement is decreased by the state degeneracy and the system size. The concurrence approaches a fixed value of about 0.3412.(for odd-qubit chain) or 0.3491 (for even-qubit chain) if the qubit number is large enough.

关键词： Heisenberg XX model local polarization pairwise entanglement

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Thoughts on studies of china continental geology and tectonics

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Progress in Natural Science:Materials International 2006年第10期16卷 1022-1026页

作者： ZHANG Guowei, GUO Anlin and YAO Anping (Ministry of Education Key Laboratory of Continental Dynamics, Department of geology, northwest university,{2., china) [a]Ministy if Education Key Laboratory of Dynamics Department of Geology Northwest University Xi an China

As an important part of the global continents, china continent has long been situated in the peculiar tectonic position and experienced extremely complicated activities, which resulted in the regional unique characteristics for china continent on the global common geological background. These characteristics contain abundant information regarding scientific key issues of modern geological frontier. Thus, china continent can be a natural laboratory and excellent arena for the modern geosciences. The modern earth sciences have started entering the era featured with earth systematic science and beyond plate tectonics. How to take the regional advantage and exploit the treasure resource to participate the new theoretical and methodological creation is a historic opportunity and great challenge we are facing. This paper generalizes research priorities in four fields on china continental geology and tectonics for discussion. They are: china continental tectonics and dynamics; Mesozoic-Cenozoic crustal deformation and deep-seated processes in china continent and the adjacent regions; deep-seated dynamic background and evolutionary trend of crustal tectonic activities on the time scale of human existence; deep-seated background and processes of conjunction and transformation of different tectonic systems.

关键词： china continental geology and continental tectonics plate tectonics continental dynamics key scientific issues.

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Timing and geochemical characters of the Sanchazi magmatic arc in Mianlüe tectonic zone,South Qinling

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Science china Earth Sciences 2004年第4期47卷 317-328页

作者： LI Shuguang1, HOU Zhenhui1, YANG Yongcheng2. SUN Weidong1,1), ZHANG Guowei3, & LI Qiuli1 1. School of Earth and Space Sciences,university of Science and Technology of china ,Hefei 2.002.,{2. 2. Regional Geological Survey Team of Shaanxi Province,xianyang 712.00, china 3. Department of geology, northwest university,xi抋n 710069, china Present address: Max-Planck-Institut f. Chemie Postfach 3060 55020 Mainz Germany School of Earth and Space Sciences University of Science and Technology of China Hefei 230026 China Regional Geological Survey Team of Shaanxi Province Xianyang 712000 China Department of geology Northwest University Xi’an 710069 China

The Sanchazi mafic-ultramafic complex in Mianlüe tectonic zone,South Qinling can be subdivided into two blocks,*** paleo-magmatic arc and Zhuangkegou paleo-oceanic crust fragment (ophiolite).The Sanchazi paleo-magmatic arc is mainly composed of ande-site,basaltic and basalt-andesitic gabbro(or diorite),andesitic dyke,plagiogranite and minor ul-tramafric rocks,which have typical geochemical features of island arc volcanic rocks,such as high field strength element(***,Ti)depletions and lower Cr,Ni *** Light rare earth element (LREE) and K enrichments of these rocks and zircon xenocrystals of 900 Ma from plagiogranite suggest that this magmatic arc was developed on the South active continental margin of the South Qinling *** U-Pb age of (300±61) Ma for zircons from plagiogranite in-dicates that the Mianlüe paleo-oceanic crust was probably subducted underneath the South Qinling micro-continent in *** is consistent with the formation time (309Ma) of the Huwan eclogite originating form oceanic subduction in Dabie Mountains,suggesting that the Mianlüe paleo-ocean probably extended eastward to the Dabie Mountains in *** high-Mg adakitic rocks in Sanchazi paleo-magmatic arc suggest thet the subducted oceanic crust was relatively young (2.Ma) and hot.

关键词： Qinling orogen, magmatic arc, U-Pb zircon age, ophiolite complex.

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PRELIMINARY GROUP CLASSIFICATION OF EQUATION v_t=f(x, v_x)v_(xx)+g(x, v_x)

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Acta Mathematica Scientia 1997年第3期17卷 255-261页

作者：屈长征 Department of Mathematics Northwest University Xi'an 710069 China

Using the method of preliminary group classification introduced by Ibragimov et al[***.32.2.88(1991)], we give a classification of equations vt= f(x, vx)vxx+g(x, vx) which admitting an extension by one of the principal Lie algebra of the equation. The result of this paper is a table of nonequivalent equations possessing an additional symmetry.

关键词： SYMMETRY CLASSES COEFFICIENT

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DISCUSSION ABOUT THE PETROGENESIS OF THE CENOZOIC VOLCANIC ROCKS FROM YUMEN AND HOH xiL AREA, QINGHAI-TIBET PLATEAU

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地学前缘 2000年第S1期7卷 145-146页

作者： Lai Shaocong[WT5,5”BX](Department of geology, northwest university,{2.,china)

The Cenozoic volcanic rocks in the Yumen and Hoh xil area formed in the intracontinental orogenic belt, which primary magma originated from a particular enrichment upmantle and accreted crust\|mantle belt or directly originated from asthenosphere superface by partial melting of *** the deeply study of the Cenozoic volcanic rocks, the effective petrological constraints on the deep\|internal geology process can be obtained. And of course, it is the window for discussion the orogeny/uplift machinism of the Qinghai—Tibet plateau.1\ Brief regional geology\;The Yumen Cenozoic volcanic rock lithodistrict belongs to the north margin of Qinghai—Tibet plateau. This lithodistrict mainly consists of Hongliuxia and Hanxia volcanic rock bodies. The Hongliuxia Pleistocene epoch volcano neck is located to the {2. of Yumen City about 40km away, consisted of tephrite and trachybasalt. The boundary line between the volcano neck and the country rocks well defined and the contact plane is almost erect. The drag structure and wrinkle have been identified in the country rocks, which were due to the upthrusting of the magma. About 100 meters away to the south of the volcano neck, there is a basaltic flowage which covers on the Cretaceous—Tertiary shale and argillaceous *** Hanxia Cenozoic volcanic rock lithodistrict is located to the west of Yumen City about 15km away, which is a river valley extending into the north piedmont of Qilian Mountain. It dissected the Cretaceous—Tertiarystratigraphic sequence. The Cenozoic volcanic rock distributed in the Hanxia river valley is a lava flowage and NWW\|trending as a long lava *** Hoh xil Cenozoic volcanic rock lithodistrict is located in the north part of Qinghai—Tibet plateau. The Cenozoic intensely intracontinental volcanism in this region had formed a number of lava sheets and subvolcanic rock bodies which were in different size and now present as lava platforms with about an elevation of 5000 meters. Affected

关键词： Qinghai—Tibet plateau Cenozoic era volcanic rock petrogenesis

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Variational Analysis Based on Proximal Subdifferential on Smooth Banach Spaces

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Acta Mathematica Sinica,English Series 2024年第2期40卷 595-618页

作者： xi Yin ZHENG Department of Mathematics Yunnan UniversityKunming 650091P.R.China

This paper first shows that for any p∈(1,2.there exists a continuously differentiable function f on l^(p)(and L^(p))such that the proximal subdifferential of f is empty everywhere,and hence it is not suitable to develop theory on proximal subdifferential in the classical Banach spaces l^(P)and L^(P) with p∈(1,2..On the other hand,this paper establishes variational analysis based on the proximal subdifferential in the framework of smooth Banach spaces of power type 2.which conclude all Hilbert spaces and all the classical spaces l^(P)and L^(P)with p∈(2.+∞).In particular,in such a smooth space,we provide the proximal subdifferential rules for sum functions,product functions,composite functions and supremum functions,which extend the basic results on the proximal subdifferential established in the framework of Hilbert *** of our main results are new even in the Hilbert space *** applications,we provide KKT-like conditions for nonsmooth optimization problems in terms of proximal subdifferential.

关键词： Smooth Banach space proximal subdifferential proximal normal cone KKT condition

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