IC培训
   
 
Visual MODFLOW Flex | 三维地下水和污染物运移模拟软件培训
 
   班级人数--热线:4008699035 手机:15921673576/13918613812( 微信同号)
      增加互动环节, 保障培训效果,坚持小班授课,每个班级的人数限3到5人,超过限定人数,安排到下一期进行学习。
   授课地点及时间
上课地点:【上海】:同济大学(沪西)/新城金郡商务楼(11号线白银路站) 【深圳分部】:电影大厦(地铁一号线大剧院站)/深圳大学成教院 【北京分部】:北京中山/福鑫大楼 【南京分部】:金港大厦(和燕路) 【武汉分部】:佳源大厦(高新二路) 【成都分部】:领馆区1号(中和大道) 【广州分部】:广粮大厦 【西安分部】:协同大厦 【沈阳分部】:沈阳理工大学/六宅臻品 【郑州分部】:郑州大学/锦华大厦 【石家庄分部】:河北科技大学/瑞景大厦
开班时间(连续班/晚班/周末班):2021年10月25日(欢迎您垂询,视教育质量为生命!)
   课时
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        ☆注重质量 ☆边讲边练

        ☆若学员成绩达到合格及以上水平,将获得免费推荐工作的机会
        ★查看实验设备详情,请点击此处★
   质量以及保障

      ☆ 1、如有部分内容理解不透或消化不好,可免费在以后培训班中重听;
      ☆ 2、在课程结束之后,授课老师会留给学员手机和E-mail,免费提供半年的课程技术支持,以便保证培训后的继续消化;
      ☆3、合格的学员可享受免费推荐就业机会。
      ☆4、合格学员免费颁发相关工程师等资格证书,提升您的职业资质。

课程大纲
 
  • HYDROGEOCHEM - Hydrologic Transport and Mixed Geochemical Kinetic/Equilibrium Model
  • HYDROGEOCHEM 1 is a coupled model of hydrologic transport and geochemical reaction in saturated-unsaturated media. It is designed to simulate transient and/or steady-state transport of Na, aqueous components and transient and/or steady-state mass balance of Ns adsorbent components and ion-exchange sites. Along the transport path, HYDROGEOCHEM computes the species distribution of N component species, Mx complexed species, My adsorbed species. Mz ion-exchanged species, and Mp potentially precipitated species. HYDROGEOCHEM is the only commercially-available model for the simulation of reactive multispecies-multicomponent chemical transport through saturated-unsaturated media. It is not a path model; it is a true transport model coupled with homogeneous and heterogeneous geochemical reactions.
  • HYDROGEOCHEM 2 is a modification of HYDROGEOCHEM which was designed to solve coupled hydrologic transport and geochemical equilibrium problems. The modification includes replacement of the EQMOD chemical equilibrium subroutines by a mixed chemical Kinetic and Equilibrium Model (KEMOD) to deal with species whose concentrations are controlled by either thermodynamics or kinetics. HYDROGEOCHEM2 is a coupled model of hydrologic transport and geochemical reaction in saturated-unsaturated media. HYDROGEOCHEM 2 comprises two basic modules: the transport module and the geochemical reaction module. The transport module is designed to simulate: (1) transient and/or steady-state transport of N saqueous components, (2) transient and/or steady-state mass balance of N sadsorbent components and NSITE ion-exchange sites. The geochemical reaction module is designed to compute the species distribution of N = (Na+ Ns) component species, Mx-Kx equilibrium-controlled complexed species, (My– Ky) equilibrium-controlled adsorbed species, Ky kinetic-controlled adsorbed species, (Mz– Kz) equilibrium-controlled ion-exchanged species, Kz kinetic-controlled ion exchanged species, (Mp– Kp) equilibrium-controlled potentially precipitated species, and Kp kinetic controlled precipitated species. The transport module includes advection, dispersion/diffusion, and slight deformation.
  • INTRODUCTION TO HYDROGEOCHEM
  • The purpose of HYDROGEOCHEM is to simulate transient and/or steady-state density-dependent flow fields and temperature distribution and to compute transient and/or steady-state distribution of reactive multispecies chemical concentrations in subsurface media.
  • HYDROGEOCHEM computes and predicts the distribution of pressure head, moisture content, flow velocity, and total head over a three-dimensional plane in either completely saturated, completely unsaturated, partially unsaturated, or partially saturated subsurface media. It also computes and predicts the spatial-temporal distribution of multi-chemical components. The media may consist of as many types of soils and geologic units as desired with different material properties. Each soil type may be isotropic or anisotropic. The processes governing the distribution of chemical distribution include (1) geochemical equilibrium of aqueous complexation, reduction-oxidation, sorption, and precipitation and dissolution, and (2) hydrological transport by flow advection, dispersion, and effect of unsaturation.
  • The generalized Richards' equation and Darcy's law governing pressure distribution and water flow in saturated-unsaturated media are simulated with the Galerkin finite-element method subject to appropriate initial and four types of boundary conditions. The hydrological transport equations (a set of PDEs) are derived based on the principle of conservation of mass, and the geochemical equilibrium equations (a set of AEs) are derived based on the mass balance and mass action. The coupled set of PDEs and AEs are simulated with either the conventional finite-element methods or the hybrid Langrangian-Eulerian finite-element method with peak capturing scheme subject to appropriate initial and four types of boundary conditions. Hexahedral elements, triangular prism, and tetrahedral elements are used to facilitate the discretization of the region of interest.
  • HYDROGEOCHEM is a coupled model of hydrologic transport and geochemical reaction in saturated-unsaturated media. It is designed to simulate transient and/or steady-state transport of Na, aqueous components and transient and/or steady-state mass balance of Ns adsorbent components and ion-exchange sites. Along the transport path, HYDROGEOCHEM computes the species distribution of N component species, Mx complexed species, My adsorbed species. Mz ion-exchanged species, and Mp potentially precipitated species. The physical, hydrological and chemical settings are as follows.
  • Media: Heterogeneous and Anisotropic.
  • Flow Conditions: Saturated-Unsaturated Flows.
  • Hydrologic Processes: Advection, Dispersion and Diffusion.
  • Chemical Processes: Aqueous Complexation, Adsorption/Desorption (Surface Complexation, Constant Capacitance, and Double Layer Approaches), Ion-Exchange, Precipitation/Dissolution, Redox, and Acid-Base Reactions.
  • Source/Sink: Spatially- and Temporally-Dependent Element and Point Sources/Sinks.
  • Initial Conditions: Prescribed Initial Condition or the Simulated Steady-State Solution as the Initial Condition.
  • Boundary Conditions: Prescribed Total Analytical Concentrations on Dirichlet Boundaries, Prescribed Fluxes on Flow-In Boundaries, Natural Advective Fluxes on Flow-Out Boundaries - All Boundary Values (Concentrations or Fluxes) are Spatially- and Temporally-Dependent.
  • Numerical Discretization: Finite-Element Methods with Quadrilateral Elements, Triangular Elements, or the Mixtures of These Two Types.
  • Approximation Options: Consistent Matrix or Mass Lumping, Nodal Quadrature or Gaussian Quadrature for Surface and Element Integrations.
  • Solvers: Direct Band Matrix Solver, Basic Point Iterations, and 4 PCG Methods (polynomial PCG, Incomplete Cholesky PCG, Modified Incomplete Cholesky PCG, and Symmetric Successive Over-Relaxation PCG).
  • Time Stepping: Implicit Difference, Crank-Nicholson Central Difference, or Mid-Difference.
  • Solution Methods for Geochemical Reactions: Newton-Raphson with Full Pivoting to Solve the Jacobian Matrix Equation and Constraints on Species Concentrations.
  • HYDROGEOCHEM is the only commercially-available model for the simulation of reactive multispecies-multicomponent chemical transport through saturated-unsaturated media. It is not a path model; it is a true transport model coupled with homogeneous and heterogeneous geochemical reactions.
  • HYDROGEOCHEM SPECIAL FEATURES
  • The special features of HYDROGEOCHEM are its flexibility and versatility in modeling as wide a range of problems as possible. The model is designed to (1) treat heterogeneous and anisotropic media, (2) consider spatially and temporally-distributed as well as point sources/sinks, (3) accept the prescribed initial conditions or obtain initial conditions by simulating the steady-state version of the system under consideration, (4) deal with prescribed transient concentrations distributed over a Dirichlet boundary, (5) handle time-dependent fluxes over variable boundaries, (6) deal with time-dependent total fluxes over Cauchy boundaries, (7) include the off-diagonal dispersion coefficient tensor components in the governing equation for dealing with cases when the coordinate system does not coincide with the principal directions of the dispersion coefficient tensor, (8) provide two options for treating the mass matrix - consistent and lumping, (9) give three options (exact relaxation, under- and over-relaxation) for estimating the nonlinear matrix, (10) include two options (direct solution with Gaussian elimination method and successive point iterations) for solving the linearized matrix equations, (11) include both quadrilateral and triangular elements to facilitate the discretization of the region, (12) automatically reset time step size when boundary conditions or sources/sinks change abruptly, and (13) include simultaneous chemical processes of aqueous complexation, precipitation/dissolution, adsorption, ion exchange, redox, and acid-base reactions.
  • HYDROGEOCHEM INPUT
  • (1) Geometry in terms of nodes and elements, and boundaries in terms of nodes and segments; (2) soil properties including (a) saturated hydraulic conductivities or permeabilities; (b) compressibility of water and the media, respectively; (c) bulk density; (d) three soil characteristic curves for each type of soil or geologic unit which are the retention curve, relative conductivity vs head curve, and water capacity curve; (e) effect porosity; and (f) dispersivities, and effective molecular diffusion coefficient for each soil type or geologic unit; (3) initial distribution of pressure head over the region of interest; (4) net precipitation, allowed ponding depth, potential evaporation, and allowed minimum pressure head in the soil; (5) prescribed head on Dirichlet boundaries; (6) prescribed fluxes on Cauchy and/or Neumann boundaries; (7) artificial withdrawals or injections of water; (8) number of chemical components as well as chemical species and their thermodynamic data base; (9) artificial sources/sinks of water and all chemical components; (10) prescribed total concentrations of all chemical components on Dirichlet boundaries; (11) prescribed fluxes of all chemical components on variable boundaries; and (12) initial distribution of all chemical component concentrations. All inputs in items 4 through 11 can be time-dependent or constant with time.
  • HYDROGEOCHEM OUTPUT
  • (1) pressure head, total head, moisture content, and flow velocity over the two-dimensional grid at any desired time; (2) water fluxes through all types of boundaries and amount of water accumulated in the media at any desired time; (3) distribution of total analytical concentrations, total dissolved concentrations, total sorbed concentrations, total precipitated concentrations, and free ion concentrations of all chemical components over a three-dimensional grid at any desired time; (4) amount of waste fluxes through the variable boundary; and (5) equivalent kds as a function of time and space in the region of interest.
  • HYDROGEOCHEM Requirements: Pentium with 16 MB RAM and FORTRAN Compiler, any Workstation, e.g., IBM RS6000, DEC Alpha, Silicon Graphics, Sun SparcStation, and HP 9000 Series
曙海教育实验设备
android开发板
linux_android开发板
fpga图像处理
曙海培训实验设备
fpga培训班
 
本课程部分实验室实景
曙海实验室
实验室
曙海培训优势
 
  合作伙伴与授权机构



Altera全球合作培训机构



诺基亚Symbian公司授权培训中心


Atmel公司全球战略合作伙伴


微软全球嵌入式培训合作伙伴


英国ARM公司授权培训中心


ARM工具关键合作单位
  我们培训过的企业客户评价:
    曙海的andriod 系统与应用培训完全符合了我公司的要求,达到了我公司培训的目的。 特别值得一提的是授课讲师针对我们公司的开发的项目专门提供了一些很好程序的源代码, 基本满足了我们的项目要求。
——上海贝尔,李工
    曙海培训DSP2000的老师,上课思路清晰,口齿清楚,由浅入深,重点突出,培训效果是不错的,
达到了我们想要的效果,希望继续合作下去。
——中国电子科技集团技术部主任 马工
    曙海的FPGA 培训很好地填补了高校FPGA培训空白,不错。总之,有利于学生的发展, 有利于教师的发展,有利于课程的发展,有利于社会的发展。
——上海电子,冯老师
    曙海给我们公司提供的Dsp6000培训,符合我们项目的开发要求,解决了很多困惑我 们很久的问题,与曙海的合作非常愉快。
——公安部第三研究所,项目部负责人李先生
    MTK培训-我在网上找了很久,就是找不到。在曙海居然有MTK驱动的培训,老师经验 很丰富,知识面很广。下一个还想培训IPHONE苹果手机。跟他们合作很愉快,老师很有人情味,态度很和蔼。
——台湾双扬科技,研发处经理,杨先生
    曙海对我们公司的iPhone培训,实验项目很多,确实学到了东西。受益无穷 啊!特别是对于那种正在开发项目的,确实是物超所值。
——台湾欧泽科技,张工
    通过参加Symbian培训,再做Symbian相关的项目感觉更加得心应手了,理 论加实践的授课方式,很有针对性,非常的适合我们。学完之后,很轻松的就完成了我们的项目。
——IBM公司,沈经理
    有曙海这样的DSP开发培训单位,是教育行业的财富,听了他们的课,茅塞顿开。
——上海医疗器械高等学校,罗老师
  我们新培训过的企业客户以及培训的主要内容:
 

一汽海马汽车 DSP培训
苏州金属研究院 DSP培训
南京南瑞集团技术 FPGA培训
西安爱生技术集团 FPGA培训,DSP培训
成都熊谷加世电气 DSP培训
福斯赛诺分析仪器(苏州) FPGA培训
南京国电工程 FPGA培训
北京环境特性研究所 达芬奇培训
中国科微系统与信息技术研究所 FPGA高级培训
重庆网视只能流技术开发 达芬奇培训
无锡力芯微电子股份 IC电磁兼容
河北科研究所 FPGA培训
上海微小卫星工程中心 DSP培训
广州航天航空 POWERPC培训
桂林航天工 DSP培训
江苏五维电子科技 达芬奇培训
无锡步进电机自动控制技术 DSP培训
江门市安利电源工程 DSP培训
长江力伟股份 CADENCE 培训
爱普生科技(无锡 ) 数字模拟电路
河南平高 电气 DSP培训
中国航天员科研训练中心 A/D仿真
常州易控汽车电子 WINDOWS驱动培训
南通大学 DSP培训
上海集成电路研发中心 达芬奇培训
北京瑞志合众科技 WINDOWS驱动培训
江苏金智科技股份 FPGA高级培训
中国重工第710研究所 FPGA高级培训
芜湖伯特利汽车安全系统 DSP培训
厦门中智能软件技术 Android培训
上海科慢车辆部件系统EMC培训
中国电子科技集团第五十研究所,软件无线电培训
苏州浩克系统科技 FPGA培训
上海申达自动防范系统 FPGA培训
四川长虹佳华信息 MTK培训
公安部第三研究所--FPGA初中高技术开发培训以及DSP达芬奇芯片视频、图像处理技术培训
上海电子信息职业技术--FPGA高级开发技术培训
上海点逸网络科技有限公司--3G手机ANDROID应用和系统开发技术培训
格科微电子有限公司--MTK应用(MMI)和驱动开发技术培训
南昌航空大学--fpga 高级开发技术培训
IBM 公司--3G手机ANDROID系统和应用技术开发培训
上海贝尔--3G手机ANDROID系统和应用技术开发培训
中国双飞--Vxworks 应用和BSP开发技术培训

 

上海水务建设工程有限公司--Alter/Xilinx FPGA应用开发技术培训
恩法半导体科技--Allegro Candence PCB 仿真和信号完整性技术培训
中国计量--3G手机ANDROID应用和系统开发技术培训
冠捷科技--FPGA芯片设计技术培训
芬尼克兹节能设备--FPGA高级技术开发培训
川奇光电--3G手机ANDROID系统和应用技术开发培训
东华大学--Dsp6000系统开发技术培训
上海理工大学--FPGA高级开发技术培训
同济大学--Dsp6000图像/视频处理技术培训
上海医疗器械高等专科学校--Dsp6000图像/视频处理技术培训
中航工业无线电电子研究所--Vxworks 应用和BSP开发技术培训
北京交通大学--Powerpc开发技术培训
浙江理工大学--Dsp6000图像/视频处理技术培训
台湾双阳科技股份有限公司--MTK应用(MMI)和驱动开发技术培训
滚石移动--MTK应用(MMI)和驱动开发技术培训
冠捷半导体--Linux系统开发技术培训
奥波--CortexM3+uC/OS开发技术培训
迅时通信--WinCE应用与驱动开发技术培训
海鹰医疗电子系统--DSP6000图像处理技术培训
博耀科技--Linux系统开发技术培训
华路时代信息技术--VxWorks BSP开发技术培训
台湾欧泽科技--iPhone开发技术培训
宝康电子--Allegro Candence PCB 仿真和信号完整性技术培训
上海天能电子有限公司--Allegro Candence PCB 仿真和信号完整性技术培训
上海亨通光电科技有限公司--andriod应用和系统移植技术培训
上海智搜文化传播有限公司--Symbian开发培训
先先信息科技有限公司--brew 手机开发技术培训
鼎捷集团--MTK应用(MMI)和驱动开发技术培训
傲然科技--MTK应用(MMI)和驱动开发技术培训
中软国际--Linux系统开发技术培训
龙旗控股集团--MTK应用(MMI)和驱动开发技术培训
研祥智能股份有限公司--MTK应用(MMI)和驱动开发技术培训
罗氏诊断--Linux应用开发技术培训
西东控制集团--DSP2000应用技术及DSP2000在光伏并网发电中的应用与开发
科大讯飞--MTK应用(MMI)和驱动开发技术培训
东北农业大学--IPHONE 苹果应用开发技术培训
中国电子科技集团--Dsp2000系统和应用开发技术培训
中国船舶重工集团--Dsp2000系统开发技术培训
晶方半导体--FPGA初中高技术培训
肯特智能仪器有限公司--FPGA初中高技术培训
哈尔滨大学--IPHONE 苹果应用开发技术培训
昆明电器科学研究所--Dsp2000系统开发技术
奇瑞汽车股份--单片机应用开发技术培训


 
 
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