Grundriss Einer Geschichte Der Naturwissenschaften; Zugleich Eine Einfuhrung in Das Studium Der Grundlegenden Naturwissenschaftlichen Litteratur (1)
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Grundriss Einer Geschichte Der Naturwissenschaften Zugleich Eine Einfuhrung in Das Studium Der Grundlegenden Naturwissenschaftlichen Litteratur (1) (2001)
EN PB NWISBN: 9781234537418 bzw. 1234537419, in Englisch, RareBooksClub, Taschenbuch, neu.
Von Händler/Antiquariat, BuySomeBooks [52360437], Las Vegas, NV, U.S.A.
This item is printed on demand. Paperback. 42 pages. Original publisher: Reston, Va. : U. S. Geological Survey, 2009. OCLC Number: (OCoLC)369163139 Subject: Groundwater flow -- New York (State) -- Broome County -- Mathematical models. Excerpt: . . . Methods and Assumptions 5 Water-level elevation, in meters above NGVD 29 260. 0 255. 0 0 2, 000 METERS 250. 0 245. 0 240. 0 River cells Layer 1 Figure 3. Simulated water-table elevation. 2 effect of sorption and precipitation reactions that remove Fefrom the dissolved phase. Finally, sulfate reduction conditions with respect to the electron acceptors. The reformulated equa-yield to methanogenesis when the sulfate concentration falls tions are as follows: below 0. 01 mg L. The transient transport simulations begin with back-r -k DONOR for ODONOR, O2 O2 2 ground conditions for electron acceptors that correspond to the concentrations in recharge and river water. The simulations are run until equilibrium conditions are attained with respect to all r -k DONOR for O 0. 01 mg L and DONOR, NO3 NO3 2 reactants in all model cells. NO3 Redox conditions become stable when the rate at which electron acceptors are supplied by incoming water balances the rate at which they are consumed by redox reactions. r -k DONOR for O 0. 01 mg L, NO DONOR, Fe2 Fe3 2 3 3 0. 01 mg L and FeEquations of the Geochemical Model r -k DONOR for O 0. 01 mg L, NO DONOR, SO4 SO4 2 3 Module 3 of the RT3D code ( Clement, 2001 ) was adapted 3 0. 01 mg L, Fe 0. 01 mg L and SOto model the distribution of reduced ground water. The module 4 simulates kinetic-limited degradation by way of multiple electron acceptors. It was intended originally to model BTEX r -k DONOR for O 0. 01 mg L, NO DONOR, CH4 CO2 2 3 degradation ( Clement and others, 1997 ), but it was used 3 0. 01 mg L, . . . This item ships from La Vergne,TN.
This item is printed on demand. Paperback. 42 pages. Original publisher: Reston, Va. : U. S. Geological Survey, 2009. OCLC Number: (OCoLC)369163139 Subject: Groundwater flow -- New York (State) -- Broome County -- Mathematical models. Excerpt: . . . Methods and Assumptions 5 Water-level elevation, in meters above NGVD 29 260. 0 255. 0 0 2, 000 METERS 250. 0 245. 0 240. 0 River cells Layer 1 Figure 3. Simulated water-table elevation. 2 effect of sorption and precipitation reactions that remove Fefrom the dissolved phase. Finally, sulfate reduction conditions with respect to the electron acceptors. The reformulated equa-yield to methanogenesis when the sulfate concentration falls tions are as follows: below 0. 01 mg L. The transient transport simulations begin with back-r -k DONOR for ODONOR, O2 O2 2 ground conditions for electron acceptors that correspond to the concentrations in recharge and river water. The simulations are run until equilibrium conditions are attained with respect to all r -k DONOR for O 0. 01 mg L and DONOR, NO3 NO3 2 reactants in all model cells. NO3 Redox conditions become stable when the rate at which electron acceptors are supplied by incoming water balances the rate at which they are consumed by redox reactions. r -k DONOR for O 0. 01 mg L, NO DONOR, Fe2 Fe3 2 3 3 0. 01 mg L and FeEquations of the Geochemical Model r -k DONOR for O 0. 01 mg L, NO DONOR, SO4 SO4 2 3 Module 3 of the RT3D code ( Clement, 2001 ) was adapted 3 0. 01 mg L, Fe 0. 01 mg L and SOto model the distribution of reduced ground water. The module 4 simulates kinetic-limited degradation by way of multiple electron acceptors. It was intended originally to model BTEX r -k DONOR for O 0. 01 mg L, NO DONOR, CH4 CO2 2 3 degradation ( Clement and others, 1997 ), but it was used 3 0. 01 mg L, . . . This item ships from La Vergne,TN.
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Hypothetical Modeling of Redox Conditions Within a Complex Ground-Water Flow Field in a Glacial Setting
EN NWISBN: 9781234537418 bzw. 1234537419, in Englisch, General Books LLC, General Books LLC, neu.
Lieferung aus: Vereinigte Staaten von Amerika, zzgl. Versandkosten, Free Shipping on eligible orders over $25, in-stock.
U.S. Government, Paperback, German-language edition, Pub by General Books LLC.
U.S. Government, Paperback, German-language edition, Pub by General Books LLC.
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Grundriss Einer Geschichte Der Naturwissenschaften; Zugleich Eine Einfuhrung in Das Studium Der Grundlegenden Naturwissenschaftlichen Litteratur (1) (2013)
EN PB NWISBN: 9781234537418 bzw. 1234537419, in Englisch, Rarebooksclub.com, Taschenbuch, neu.
Lieferung aus: Vereinigte Staaten von Amerika, zzgl. Versandkosten, Verandgebiet: DOM.
Von Händler/Antiquariat, BuySomeBooks, NV, Las Vegas, [RE:4].
Trade paperback.
Von Händler/Antiquariat, BuySomeBooks, NV, Las Vegas, [RE:4].
Trade paperback.
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