Karst hydrology and physical speleology
著者
書誌事項
Karst hydrology and physical speleology
Springer-Verlag, 1980
- タイトル別名
-
Karsthydrographie und physische Speläologie
- 統一タイトル
-
Karsthydrographie und physische Speläologie
大学図書館所蔵 全9件
  青森
  岩手
  宮城
  秋田
  山形
  福島
  茨城
  栃木
  群馬
  埼玉
  千葉
  東京
  神奈川
  新潟
  富山
  石川
  福井
  山梨
  長野
  岐阜
  静岡
  愛知
  三重
  滋賀
  京都
  大阪
  兵庫
  奈良
  和歌山
  鳥取
  島根
  岡山
  広島
  山口
  徳島
  香川
  愛媛
  高知
  福岡
  佐賀
  長崎
  熊本
  大分
  宮崎
  鹿児島
  沖縄
  韓国
  中国
  タイ
  イギリス
  ドイツ
  スイス
  フランス
  ベルギー
  オランダ
  スウェーデン
  ノルウェー
  アメリカ
注記
Translation of: Karsthydrographie und physische Speläologie
Bibliography: p. [244]-260
Includes index
内容説明・目次
内容説明
The present publication on karst hydrology and physical speleology combines two subjects which have up to now been treated separately. The two fields of knowledge have gone their separate ways, less as a result of differences in subject matter than of varying approaches. The focal point in karst hydrology lies in the description of subter- ranean water with its physical and chemical properties, whereas physical speleology de- scribes subterranean cavities with their contents (air, water, and sediments), which gen- erally have been created by water. Such cavities can be correctly interpreted only by means of a knowledge of karst hydrology, yet they in turn yield indications of the pro- perties of karst water. Karst hydrology and physical speleology are thus two aspects of the subterranean karst phenomenon and should be viewed congruently. This book addresses geologists, hydrologists, geomorphologists, geographers, and karstologists, above all speleologists, as well as all friends of caves, especially the cavers among them.
Its contents must therefore appeal to two groups: on one hand to the academically trained, whether university faculty, graduates, or students, who as a rule have the necessary basic knowledge to be able to understand the theoretical com- ments; on the other hand to the laymen, who have fust-hand experience from their own observations in caves, but who often do not dispose over the scientific foundation necessary for an understanding of the phenomena. Therefore occasionally more attention will be given to problems of a simpler nature and to questions of technical terminology.
目次
- 1. Karstifiable Rocks.- 1.1 Introduction.- 1.2 Evaporites.- 1.2.1 Anhydrite and Gypsum.- 1.2.2 Rock Salt Halite.- 1.3 Carbonate Rocks: Limestone and Dolomite.- 1.3.1 Limestone and Dolomite.- 1.3.2 Differences between Limestone and Dolomite.- 1.3.3 Limestones.- 1.3.4 Structure of Limestones.- 1.3.5 Permeabuity of Limestone Rock.- 1.3.6 Reefs.- 2. Processes of Dissolution of Karstifiable Rocks, Corrosion.- 2.1 Dissolution of Gypsum and Rock Salt.- 2.2 Dissolution of Carbonate Rocks.- 2.2.1 CO2 on Either Side of the Interface Air/Solution.- 2.2.2 The Kinetics of CO2.- 2.2.3 Dissolution of CaCO3.- 2.2.4 Influence of Other Ions.- 2.2.5 Mixing Corrosion.- 2.2.6 Cooling Corrosion and Thermal Mixing Corrosion.- 2.2.7 Pressure Dependence of Limestone Solutions.- 2.2.8 Comparison and Evaluation of the Types of Corrosion.- 2.2.9 Further Possibilities of Corrosion in the Phreatic Zone.- 2.3 Karst Denudation.- 3. A General View of Exokarst.- 3.1 Karren, the Small Solution Feature.- 3.1.1 Introduction.- 3.1.2 The Genetic System of Karren Forms.- 3.1.3 Karren and Karst Hydrology.- 3.1.4 Pseudokarren.- 3.2 Small, Closed Hollows in Karst.- 3.2.1 Dolines.- 3.2.2 On the Morphology of Dolines.- 3.2.3 Cenotes.- 3.2.4 Karst Window and Karst Gulfs.- 3.2.5 Cockpits.- 3.2.6 Uvalas (Slovenic).- 3.3 Corrosion Plains.- 3.4 Fluvial Karst Forms: Karst Valleys, Dry Valleys.- 3.5 Glacial Karst.- 3.6 Poljes.- 4. Endokarst and Karst Hydrology.- 4.1 Introduction.- 4.2 The Origin of the Water in Endokarst.- 5. Physical Behavior of Karst Water.- 5.1 Hydrological Perviousness - Karst Hydro logical Activity - Velocity of Flow.- 5.2 Catchment Area - Local Base Level.- 5.3 Shallow and Deep Karst.- 5.4 Pressure Flow - Gravitational Flow
- the Cave River.- 5.5 Piezometric Surface.- 5.5.1 Introduction.- 5.5.2 Static Karst Water-Body, Local Base Level.- 5.5.3 The Bernoulli Effect (Equation of Continuity).- 5.5.4 Torricelli's Theory (Law of Outflow).- 5.5.5 Loss of Pressure in Flowing Water.- 5.5.6 Losses Through Friction, Losses of Pressure.- 5.5.7 Analysis of an Inaccessible Water-Course.- 5.5.8 Cavitation.- 5.6 Poljes as Karst-Hydrological Regulating Factors.- 6. The Karst Hydrological Zones.- 6.1 Introduction.- 6.2 Vadose Zone.- 6.2.1 Inactive Vadose Zone.- 6.2.2 Feeders.- 6.2.3 High-Water-Zone.- 6.3 Phreatic Zone.- 7. Karst Water - Groundwater.- 7.1 Introduction.- 7.2 Underground Water.- 7.3 "Karst Barre".- 7.4 Blocked Karst.- 8. Underground Karst Levels.- 8.1 Introduction.- 8.2 The Cave Level of the Piezometric-Surface Type - Evolution Level.- 8.3 Cave Levels According to the Type of River-Bed.- 9. Karst Springs.- 9.1 Introduction.- 9.2 Classification of Karst Springs.- 9.3 Vauclusian Springs and Other Large Karst Springs.- 9.4 Periodic Springs - Ebb and Flow Springs (Intermittent Springs).- 9.4.1 Periodic Springs.- 9.4.2 Intermittent Springs, Ebb and Flow Springs.- 9.4.3 Episodic Springs.- 9.5 Subaqueous Springs.- 9.5.1 Sublacustrine Springs.- 9.5.2 Submarine Springs - Vrulje.- 9.5.3 The Sea Mills of Argostoli.- 9.6 Physicochemical Properties of the Water of a Karst Spring.- 9.6.1 Discharge.- 9.6.2 Variations in Temperature.- 9.6.3 Chemistry of Spring Water.- 10. Tracers.- 10.1 Tracers.- 10.2 The Tracer-Diagram.- 11. Incasion, Breakdown.- 12. Speleomorphology, the World of Forms Created by the Subterranean Removal of Matter.- 12.1 Introduction.- 12.2 Large Forms.- 12.2.1 Passages - Passages Cross-Sections.- 12.2.2 Ceiling Half-Tube Passage.- 12.2.3 Dome - Bell-Shaped Dome - Chamber.- 12.2.4 Shafts.- 12.3 Small Forms.- 12.3.1 Cave Karren.- 12.3.2 Potholes, Inverse Solution Pockets.- 12.3.3 Scallops and Ceiling Dents.- 13. Cave Sediments.- 13.1 Clastic Sediments.- 13.1.1 Coarse Clastic Sediments.- 13.1.2 Fine Clastic Sediments.- 13.1.3 Conditions of Sedimentation.- 13.1.4 Interpretation of a Sediment Profile.- 13.1.5 Clay Minerals - Heavy Minerals.- 13.1.6 Small Forms of Fine Clastic Sediments.- 13.2 Organic Sediments.- 13.2.1 Phytogenic Sediments.- 13.2.2 Coprogenic Sediments.- 13.2.3 Cave Phosphates.- 13.3 Chemical Sediments.- 13.3.1 Limestone Deposits.- 13.3.2 Cave Sulphates, Gypsum.- 13.3.3 Cave Minerals.- 14. Speleogenetics.- 14.1 The Role of Joints and Bedding Interstices in Speleogenetics.- 14.2 The Development from Interstice to Cave Passage Under Phreatic Conditions.- 14.3 The Development to a Cave Level.- 14.4 Primary and Secondary Vadose Cave Formation.- 14.5 Widening of Interstices.- 14.6 Phases in the Development of Cavities.- 15. Speleometerology - Speleoclimatology.- 15.1 Movement of Air in Caves.- 15.1.1 Exogenous Factors of Pressure Differences.- 15.1.2 Endogenous Causes of Pressure Differences.- 15.1.3 Cave Winds as a Result of Temperature Contrast Between Open Atmosphere and Underground Cavities.- 15.1.4 Air Movements Caused by Flowing Water.- 15.2 Cave Temperatures.- 15.3 Humidity of the Air.- 16. Ice Caves.- 17. Classification of Underground Cavities.- 17.1 Definition of Cave.- 17.2 Genetic Classification.- 17.2.1 Primary Caves.- 17.2.2 Secondary Caves.- 17.3 Geological-Petrographical Classification.- 17.4. Classification According to Size.- 17.5. Classification According to Prominent Characteristics.- Appendix (A) Conventional Cave Signs.- References.- Plates.
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