Isbn: 9781119166566 - crustal permeability (wiley works) (12 resultados)

hardcover. Condición: Good. Connecting readers with great books since 1972! Used textbooks may not include companion materials such as access codes, etc. May have some wear or writing/highlighting. We ship orders daily and Customer Service is our top priority.

Condición: As New. Unread book in perfect condition.

Condición: New.

Hardcover. Condición: new. Hardcover. Permeability is the primary control on fluid flow in the Earths crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. The practical importance of permeability and the potential for large, dynamic changes in permeability is highlighted by ongoing issues associated with hydraulic fracturing for hydrocarbon production (fracking), enhanced geothermal systems, and geologic carbon sequestration. Although there are thousands of research papers on crustal permeability, this is the first book-length treatment. This book bridges the historical dichotomy between the hydrogeologic perspective of permeability as a static material property and the perspective of other Earth scientists who have long recognized permeability as a dynamic parameter that changes in response to tectonism, fluid production, and geochemical reactions. Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. Shipping may be from multiple locations in the US or from the UK, depending on stock availability.…

Condición: As New. Unread book in perfect condition.

Condición: New. Brand new! Please provide a physical shipping address.

Condición: New. Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. Editor(s): Gleeson, Tom; Ingebritsen, Steve. Series: Wiley Works. Num Pages: 472 pages. BIC Classification: RBGD; RBKF. Category: (P) Professional & Vocational. Dimension: 282 x 221 x 31. Weight in Grams: 1826. . 2016. 1st Edition. Hardcover. . . . . …

Condición: New.

Condición: New. Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. The practical impor.

Condición: New. Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. Editor(s): Gleeson, Tom; Ingebritsen, Steve. Series: Wiley Works. Num Pages: 472 pages. BIC Classification: RBGD; RBKF. Category: (P) Professional & Vocational. Dimension: 282 x 221 x 31. Weight in Grams: 1826. . 2016. 1st Edition. Hardcover. . . . . Books ship from the US and Ireland. …

Hardcover. Condición: Brand New. 1st edition. 472 pages. 11.25x9.00x1.25 inches. In Stock.

Hardcover. Condición: new. Hardcover. Permeability is the primary control on fluid flow in the Earths crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. The practical importance of permeability and the potential for large, dynamic changes in permeability is highlighted by ongoing issues associated with hydraulic fracturing for hydrocarbon production (fracking), enhanced geothermal systems, and geologic carbon sequestration. Although there are thousands of research papers on crustal permeability, this is the first book-length treatment. This book bridges the historical dichotomy between the hydrogeologic perspective of permeability as a static material property and the perspective of other Earth scientists who have long recognized permeability as a dynamic parameter that changes in response to tectonism, fluid production, and geochemical reactions. Permeability is the primary control on fluid flow in the Earth s crust and is key to a surprisingly wide range of geological processes, because it controls the advection of heat and solutes and the generation of anomalous pore pressures. Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability.…