Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Sediments characterization

Lambert, J. B., S. C. Johnson, and G. O. Poinar, Jr. (1996), Nuclear magnetic resonance sediment characterization of cretaceous amber, Archaeometry 38, 325-335. [Pg.592]

Engler, R.M., Brannon, J.M. and Rose, J. (1977) A practical selective extraction procedure for sediment characterization. In Chemistry of Marine Sediments (ed. Yen, T.F.). Ann Arbor Science Publishers, Ann Arbor, MI, p. 163. [Pg.318]

Engler, R. M., Brammon, J. M., Rose, J. and Bigham, G. A practical selective extraction procedure for sediment characterization, Presented at l68th Amer. Chem. Soc. Meeting, Atlantic City, September 197. ... [Pg.610]

Seme R. J. and Gore V. L. (1996) Strontium-90 Adsorption-Desorption Properties and Sediment Characterization at the 100 N-area. Pacific Northwest National Eaboratory. [Pg.4800]

Major functions of the distal nephron include the regeneration of bicarbonate, the excretion of acid (hydrogen ion), the secretion of potassium, and the reabsorption of water. Damage to this portion of the nephron may present as significant acidemia and either hypo-or hyperkalemia, depending on the mechanism of injury. For example, amphotericin B produces small pores in the luminal membrane of distal tubular cells. These pores allow small molecules such as potassium to leak out the molecules are then wasted in the urine. Consequently, amphotericin B nephrotoxicity is characterized by hypokalemia secondary to renal potassium wasting. ATN is associated with urinary sediment characterized by the presence of tubular cells, coarse granular casts, and rarely, RBC casts. [Pg.786]

DOE. 1996e. Strontium-90 adsorption-desorption properties and sediment characterization at the 100N-area. Richland, WA U.S. Department of Energy. DE-AC06-76RLO 1830. [Pg.335]

The presence of iron minerals and their respective reactivity towards sulfide is of greatest importance for the pore water chemistry and the limitation for pyrite formation. In case of reactive iron rich sediments dissolved iron may build-up in pore water and dissolved sulfide is hardly present although sulfate reduction occurs. In contrast, in sediments characterized by a low content of reactive iron dissolved sulfide can build-up instead of dissolved iron (Canfield 1989). The degree of pyritisation (DOP) was originally defined by Berner (1970) and was later modified by Leventhal and Taylor (1990) and Raiswell et al. (1994). DOP is now defined as ... [Pg.253]

RlOO E. C. Bortoluzzi, M. A. Santanna dos Santos and M. A. ViUetti, Sediment Characterization , in Sedimentology of Aqueous Systems, eds. C. Poleto and S. Charlesworth, John Wiley Sons Ltd., Chichester, UK, 2010, p. 80. [Pg.27]

Sedimentation Characterization Based on Cumulative Monitoring of Sediments from an Initially Homogeneous... [Pg.103]

In the sedimentation characterization based on cumulative monitoring of sediments from an initially homogeneous suspension a record of the weight of sediment at... [Pg.103]


See other pages where Sediments characterization is mentioned: [Pg.531]    [Pg.12]    [Pg.897]    [Pg.203]    [Pg.5139]    [Pg.454]    [Pg.189]    [Pg.154]    [Pg.6]    [Pg.223]    [Pg.857]    [Pg.93]    [Pg.103]    [Pg.604]   
See also in sourсe #XX -- [ Pg.150 ]




SEARCH



© 2024 chempedia.info