Numerical Simulation of Reactive Flow in Hot Aquifers : SHEMAT and Processing SHEMAT （2003）

個数：

Numerical Simulation of Reactive Flow in Hot Aquifers : SHEMAT and Processing SHEMAT （2003）

Clauser, Christoph (EDT)

ウェブストア価格 ¥22,866（本体¥20,788）
Springer-Verlag Berlin and Heidelberg GmbH & Co. K（2014/04発売）
外貨定価 US$ 109.00
ポイント 207pt

提携先の海外書籍取次会社に在庫がございます。通常3週間で発送いたします。
【重要ご説明事項】
1. 納期遅延や、ご入手不能となる場合が若干ございます。
2. 複数冊ご注文の場合は、ご注文数量が揃ってからまとめて発送いたします。
3. 美品のご指定は承りかねます。

●3Dセキュア導入とクレジットカードによるお支払いについて

【入荷遅延について】
世界情勢の影響により、海外からお取り寄せとなる洋書・洋古書の入荷が、表示している標準的な納期よりも遅延する場合がございます。
おそれいりますが、あらかじめご了承くださいますようお願い申し上げます。

◆画像の表紙や帯等は実物とは異なる場合があります。

◆ウェブストアでの洋書販売価格は、弊社店舗等での販売価格とは異なります。
また、洋書販売価格は、ご注文確定時点での日本円価格となります。
ご注文確定後に、同じ洋書の販売価格が変動しても、それは反映されません。

製本 Paperback:紙装版/ペーパーバック版／ページ数 332 p.
言語 ENG
商品コード 9783642628665

Full Description

Christoph Clauser and Jom Bartels SHE MAT (Simulator for HEat and MAss Transport) is an easy-to-use, general- purpose reactive transport simulation code for a wide variety of thermal and hy- drogeological problems in two and three dimensions. Specifically, SHEMAT solves coupled problems involving fluid flow, heat transfer, species transport, and chemical water-rock interaction in fluid-saturated porous media. It can handle a wide range of time scales. Therefore, it is useful to address both technical and geo- logical processes. In particular, it offers special and attractive features for model- ing steady-state and transient processes in hydro-geothermal reservoirs. This makes it well suited to predict the long-term behavior of heat mining installations in hot aquifers with highly saline brines. SHEMA T in its present form evolved from a fully coupled flow and heat transport model (Clauser 1988) which had been developed from the isothermal USGS 3-D groundwater model of Trescott and Larson (Trescott 1975; Trescott and Larson 1977).
Transport of dissolved species, geochemical reactions between the solid and fluid phases, extended cou- pling between the individual processes (most notably between porosity and per- meability), and a convenient user interface (developed from Processing Modflow (Chiang and Kinzelbach 2001)) were added during several research projects funded by the German Science Foundation (DFG) under grant CL 12117 and the German Federal Ministries for Education, Science, Research, and Technology (BMBF) under grant 032 69 95A-D and for Economics and Technology (BMWi) under grant 0327095 (Bartels et al. 2002, Kuhn et al. 2002a).

1 Introduction.- 2 Numerical Simulation of Reactive Flow using SHEMAT.- 2.1 General.- 2.2 Governing Equations.- 2.4 Input / Output.- 2.5 Practical Modeling: Remarks, Explanations and Instructions.- 2.6 Code Verification.- 3 Pre- and Post-Processing with "Processing SHEMAT".- 3.1 What is Processing SHEMAT?.- 3.2 Modeling Environment.- 3.3 Menu System.- 4 Advanced Features.- 4.1 Chemical Equilibrium Speciation for Brines at High Temperatures and Ionic Strength.- 4.2 Fractal Relation Between Porosity and Permeability: Theory and Verification.- 5 Tutorial for "Processing SHEMAT".- 5.1 Introduction.- 5.2 Creating a Fluid Flow, Heat Transfer, and Solute Transport Model.- 5.3 Using the Geochemical Reaction Module.- 5.4 Expanding the Model to Three Dimensions.- 6 Applications.- 6.1 Development of a Preferential Flow Path in an Anhydrite Cemented Sandstone: Numerical Simulation of a Core Flooding Experiment.- 6.2 Modeling Flooding of a Sandstone Core with Reactive Transport and Subsequent Changes in Porosity and Permeability.- 6.3 Injection Well with Reaction Kinetics.- 6.4 Magmatic Intrusions in Long Valley Caldera.- 6.5 Rhine Graben Cross Section.- 6.6 Thermal Transect of Continental Lithosphere in Canada.- 6.7 Waiwera Coastal Geothermal System.- References.