Items related to Karst Geomorphology and Hydrology
components dissolve. The alumino silicate minerals are the great example of the incongruent class, releasing Na+, K+, HCO-, etc. ions in reaction with J water but retaining most of their atoms in re-ordered solids such as kaolinite. The karst minerals are all congruent in normal conditions. Incongruent solution of dolomite and precipitation of calcite may occur in some exceptional conditions mentioned later. The sample of congruent minerals in Table 3. 1 contains all the common elements of crustal rocks except Fe, and furnishes a majority of the common dissolved inorganic species. The range of solubility is enormou~. Gibbsite is an example that is insoluble to all intents and purposes; even in the most favourable circumstances encountered on the surface of this planet physical processes will disaggregate it and remove it as colloids or larger grains before there is significant solution damage. Rock salt (halite) is so soluble that it is rapidly destroyed in outcrop except in the driest places; it is principally important for its role in interstratal karstification. Sylvite and mirabilite are rarely encountered and never in great bulk. They occur as minor secondary cave minerals (see section 8. 4). Gypsum and anhydrite are quite common in outcrop. Karst features develop upon them rapidly because of their comparatively high solubility. Limestone and dolomite are common in outcrop. Their maximum solubility varies with environmental conditions but never approaches that of gypsum. Quartzite and siliceous sandstones are equally common in outcrop.
"synopsis" may belong to another edition of this title.
Review:
The book as a whole provides a fascinating account of so many aspects of the subject that it is difficult to put it down...This is the best book on the subject I know. - The Times Higher Education Supplement; Karst Geomorphology and Hydrology is simply the best compilation so far of existing karst work...everything you could want to know about karst is there...the last word in standard texts in karst geomorphology and hydrology - Progress in Physical Geography
"About this title" may belong to another edition of this title.
- PublisherSpringer
- Publication date2012
- ISBN 10 9401177805
- ISBN 13 9789401177801
- BindingPaperback
- Number of pages616
Buy New
Learn more about this copy
US$ 142.01
Shipping:
FREE
Within U.S.A.
Top Search Results from the AbeBooks Marketplace
Seller Image
Karst Geomorphology and Hydrology [Soft Cover ]
Seller:
Rating
Book Description Soft Cover. Condition: new. Seller Inventory # 9789401177801
Buy New
US$ 142.01
Convert currency
Stock Image
Karst Geomorphology and Hydrology
Published by
Springer
(2012)
ISBN 10: 9401177805
ISBN 13: 9789401177801
New
Softcover
Quantity: > 20
Seller:
Rating
Book Description Condition: New. Seller Inventory # ABLIING23Apr0412070058937
Buy New
US$ 147.97
Convert currency
Stock Image
Karst Geomorphology and Hydrology
Published by
Springer
(2012)
ISBN 10: 9401177805
ISBN 13: 9789401177801
New
Softcover
Quantity: > 20
Seller:
Rating
Book Description Condition: New. PRINT ON DEMAND Book; New; Fast Shipping from the UK. No. book. Seller Inventory # ria9789401177801_lsuk
Buy New
US$ 150.44
Convert currency
Seller Image
Karst Geomorphology and Hydrology
Published by
Springer Netherlands Jun 2012
(2012)
ISBN 10: 9401177805
ISBN 13: 9789401177801
New
Taschenbuch
Quantity: 2
Seller:
Rating
Book Description Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -components dissolve. The alumino silicate minerals are the great example of the incongruent class, releasing Na+, K+, HCO-, etc. ions in reaction with J water but retaining most of their atoms in re-ordered solids such as kaolinite. The karst minerals are all congruent in normal conditions. Incongruent solution of dolomite and precipitation of calcite may occur in some exceptional conditions mentioned later. The sample of congruent minerals in Table 3. 1 contains all the common elements of crustal rocks except Fe, and furnishes a majority of the common dissolved inorganic species. The range of solubility is enormou~. Gibbsite is an example that is insoluble to all intents and purposes; even in the most favourable circumstances encountered on the surface of this planet physical processes will disaggregate it and remove it as colloids or larger grains before there is significant solution damage. Rock salt (halite) is so soluble that it is rapidly destroyed in outcrop except in the driest places; it is principally important for its role in interstratal karstification. Sylvite and mirabilite are rarely encountered and never in great bulk. They occur as minor secondary cave minerals (see section 8. 4). Gypsum and anhydrite are quite common in outcrop. Karst features develop upon them rapidly because of their comparatively high solubility. Limestone and dolomite are common in outcrop. Their maximum solubility varies with environmental conditions but never approaches that of gypsum. Quartzite and siliceous sandstones are equally common in outcrop. 620 pp. Englisch. Seller Inventory # 9789401177801
Buy New
US$ 153.39
Convert currency
Stock Image
Karst Geomorphology and Hydrology
Seller:
Rating
Book Description Condition: New. pp. 620. Seller Inventory # 26126777549
Buy New
US$ 177.53
Convert currency
Seller Image
Karst Geomorphology and Hydrology
Published by
Springer Netherlands
(2012)
ISBN 10: 9401177805
ISBN 13: 9789401177801
New
Softcover
Quantity: > 20
Seller:
Rating
Book Description Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. components dissolve. The alumino silicate minerals are the great example of the incongruent class, releasing Na+, K+, HCO-, etc. ions in reaction with J water but retaining most of their atoms in re-ordered solids such as kaolinite. The karst minerals are a. Seller Inventory # 5836086
Buy New
US$ 130.80
Convert currency
Seller Image
Karst Geomorphology and Hydrology
Published by
Springer Netherlands
(2012)
ISBN 10: 9401177805
ISBN 13: 9789401177801
New
Taschenbuch
Quantity: 1
Seller:
Rating
Book Description Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - components dissolve. The alumino silicate minerals are the great example of the incongruent class, releasing Na+, K+, HCO-, etc. ions in reaction with J water but retaining most of their atoms in re-ordered solids such as kaolinite. The karst minerals are all congruent in normal conditions. Incongruent solution of dolomite and precipitation of calcite may occur in some exceptional conditions mentioned later. The sample of congruent minerals in Table 3. 1 contains all the common elements of crustal rocks except Fe, and furnishes a majority of the common dissolved inorganic species. The range of solubility is enormou~. Gibbsite is an example that is insoluble to all intents and purposes; even in the most favourable circumstances encountered on the surface of this planet physical processes will disaggregate it and remove it as colloids or larger grains before there is significant solution damage. Rock salt (halite) is so soluble that it is rapidly destroyed in outcrop except in the driest places; it is principally important for its role in interstratal karstification. Sylvite and mirabilite are rarely encountered and never in great bulk. They occur as minor secondary cave minerals (see section 8. 4). Gypsum and anhydrite are quite common in outcrop. Karst features develop upon them rapidly because of their comparatively high solubility. Limestone and dolomite are common in outcrop. Their maximum solubility varies with environmental conditions but never approaches that of gypsum. Quartzite and siliceous sandstones are equally common in outcrop. Seller Inventory # 9789401177801
Buy New
US$ 157.54
Convert currency
Stock Image
Karst Geomorphology and Hydrology
Print on Demand
Seller:
Rating
Book Description Condition: New. Print on Demand pp. 620 49:B&W 6.14 x 9.21 in or 234 x 156 mm (Royal 8vo) Perfect Bound on White w/Gloss Lam. Seller Inventory # 133809938
Buy New
US$ 195.91
Convert currency