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最新版
GMS 6.5 於2008.10.17更新
相關軟體
SMS 10.0
│WMS 8.0
GMS 6.5已經上市了! 新特點和改進使GMS比以往更有生產力! GMS是最尖端的和全功能的地下水模擬軟體,數以千計的人在全世界90多個國家使用在政府機關、私人公司和國際站點
等,它已被證明是有效的和令人興奮的模型系統。GMS提供每一個階段的地下水模擬工具,包括工地的表徵模型開發、校準後處理和可視化。GMS也提供在二維和三維的有限微分和有限元素法模型包括MODFLOW 2000, MODPATH, MT3DMS/RT3D, SEAM3D, ART3D, UTCHEM, FEMWATER, PEST, UCODE, MODAEM
和 SEEP2D。不論你的需要哪些模擬,GMS都有工具幫助你。
GMS的模組化設計讓使用者只選擇那些所需要的地下水模擬功能,可以隨時填購其他模組。
Groundwater Flow &
Transport Options
The variety of modeling options in GMS is unparalleled!
Rather than being limited to one main model (such as MODFLOW) and accompanying “add-on” codes, GMS provides
interfaces to a wide range of 2D or 3D models. Here is
a brief overview of the options available to you:
2D Flow
● Perform fast, easy modeling with the MODAEM analytical element model integrated into GMS!
● 2D finite-element seeepage modeling is supported in the SEEP2D model - perfect for dams, levees, cutoff trenches, etc.
3D Flow
● 3D finite difference modeling with MODFLOW 2000 (saturated zone)
● 3D finite-element modeling with FEMWATER (saturated and unsaturated zone)
Solute Transport
● Simple analytical transport modeling with ART3D
● Simple 3D transport with MT3D, MODPATH, or FEMWATER
● Reactive 3D transport with RT3D or SEAM3D
● Multi-phase reactive transport with UTCHEM
Unsaturated Zone Flow and Transport
● Fully 3D unsaturated/saturated flow and transport modeling with FEMWATER or UTCHEM
GIS-based Model Conceptualization
One of GMS's greatest strengths traditionally has been the conceptual model approach. This approach makes it possible to build a conceptual model in the GMS Map Module using GIS feature objects (points, arcs, and polygons). The conceptual model defines the boundary conditions, sources/sinks, and material property zones for a model. The model data can then be automatically discretized to the model grid or mesh. The conceptual model approach makes it possible to deal with large complex models in a simple and efficient manner.
The GIS Module now available in GMS has made creating conceptual models from GIS data even easier. With direct linkage to ArcGIS and almost any format of GIS data, you can access geometry and attributes faster than ever before.
Whether the GIS data is created in GMS or imported from GIS files, the method of model building remains the same. You edit the model at a GIS object level and let GMS do the hard work of grid or mesh building and parameter assignment to each element of the model.
3D Model Conceptualizationn
GMS presents new and improved tools for the creation of
complex 3D stratigraphy models and the ability to
translate that 3D object direclty to a finite-difference
grid model or fininte-element mesh model.
The “Horizons” approach allows you to create complex
solids from borehole and cross section data quickly and
easily. These tools alow you to create solids with
complex stratigraphy such as pinch out zones,
truncations, and outcroppings.

You can transfer the results (material properties) of
a solid model direclty to a numerical model such as a
MODFLOW grid or a FEMWATER mesh. You can also direclty
generate MODFLOW 2000 HUF data - GMS is the only system
that allows you to do this!
Site Visualization
GMS is a powerful graphical tool for model creation and visualization of results. Models can be built using digital maps and elevation models for reference and source data. During the model building process, the graphical representation of the model allows quick review and presentation of your work. Fully 3D views, with contouring and shading, of your model allow anyone to see and understand the domain and parameters of your analysis.
A groundwater model can be displayed in plan view or
3D oblique view, and rotated interactively.
Cross-sections and fence diagrams may be cut arbitrarily
anywhere in the model. Hidden surface removal, and color
and light source shading can be used to generate highly
photorealistic rendered images. Contours and color
fringes can be used to display the variation of input
data or computed results. Cross-sections and iso-surfaces
can be interactively generated from 3D meshes, grids,
and solids, allowing the user to quickly visualize the
3D model.
Both steady-state and transient
solutions can be displayed in an animated format (as if
viewing a movie) using either vector, iso-surface, color
fringe, or contour animation. For example, animation of
a transient solution allows the user to observe how
head, drawdown, velocity, and contaminate concentration
vary with time. In addition, GMS can also sweep an iso-surface
through the 3D model. The minimum and maximum iso-surface
values are determined from the model and the program
will then linearly interpolate and display multiple iso-surfaces
in rapid succession. This allows the user to quickly
understand the spatial variation of a contaminant plume,
for example.
Risk Assessment (Stochastic)
Modeling
One of the most exciting features in GMS is a suite
of tools for performing stochastic simulations with
MODFLOW and accompanying transport models.
The Risk Analysis Wizard is a new tool associated with
the stochastic modeling tools in GMS. Two types of
analysis are currently supported: probabilistic
threshold analysis and probabilistic capture zone
delineation. This wizard allows you to quantify the
risk of a contaminant exceeding critical levels in
groundwater or the risk of a capture zone including key
areas at a site. Such analysis helps determine
appropriate action to be taken in design or remediation.
Two approaches are supported for setting up stochastic
simulations: parameter randomization and indicator
simulation. The parameter randomization can be done
using either a “Monte Carlo” or a “Latin Hypercube”
approach. The indicator simulation approach randomizes
the spatial distribution of the parameter zones using
the T-PROGS software. The T-PROGS software is used to
perform transition probability geostatistics on borehole
data. The output of the T-PROGS software is a set of N
material sets on a 3D grid. Each of the material sets is
conditioned to the borehole data and the materials
proportions and transitions between the boreholes
follows the trends observed in the borehole data. These
material sets can be used for stochastic simulations
with MODFLOW.
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Automated Model Calibration
Calibration is the process of modifying the input
parameters to a groundwater model until the output from
the model matches an observed set of data. GMS includes
a suite of tools to assist in the process of calibrating
a groundwater model to point and/or flux observations.
When a computed solution is imported to GMS, the point
and flux residual errors are plotted on a set of
calibration targets and a variety of plots can be
generated showing overall calibration statistics. Most
of the calibration tools can be used with any of the
models in GMS.

Automated parameter estimation is supported in GMS for the MODFLOW simulations using MODFLOW PES, PEST, and UCODE. These are sometimes called "inverse models". Most of the steps involved in setting up an inverse model in GMS are the same regardless of the selected inverse model. The basic process for inverse modeling is:
● Build a base model with MODFLOW
● Input observed data (point or flux data)
● Indicate the model input parameters that the
inverse model can adjust to make the model match the
observations.
● Let the inverse model run - it will adjust input
parameters and run the MODFLOW simulation repeatedly
until the best match betweeen computed data and
observed data is obtained.

You can transfer the results (material properties) of a solid model direclty to a numerical model such as a MODFLOW grid or a FEMWATER mesh. You can also direclty generate MODFLOW 2000 HUF data - GMS is the only system that
allows you to do this!
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