C3666
Carbonic Anhydrase Isozyme II from bovine erythrocytes
Isoelectric focusing marker, pI 5.4
Sinonimo/i:
Carbonate Dehydratase, Carbonate Hydrolyase, Carbonic Anhydrase II
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About This Item
Prodotti consigliati
Livello qualitativo
Stato
powder
Confezionamento
vial of ~1 mg protein
pI
5.4
Solubilità
deionized water: soluble, clear to slightly hazy, colorless (Dissolve vial contents in 0.25mL of deionised water.)
Temperatura di conservazione
−20°C
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Nota sulla preparazione
Dissolve in 0.25mL of deionized water. The solution is colorless, clear to slightly hazy.
Avvertenze
Danger
Indicazioni di pericolo
Consigli di prudenza
Classi di pericolo
Resp. Sens. 1
Codice della classe di stoccaggio
11 - Combustible Solids
Classe di pericolosità dell'acqua (WGK)
WGK 3
Punto d’infiammabilità (°F)
Not applicable
Punto d’infiammabilità (°C)
Not applicable
Dispositivi di protezione individuale
Eyeshields, Gloves, type N95 (US)
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I clienti hanno visto anche
J Gao et al.
Biophysical journal, 76(6), 3253-3260 (1999-06-04)
This paper describes the use of electrospray ionization-Fourier transform ion cyclotron mass spectrometry (ESI-FTICR-MS) to study the relative stabilities of noncovalent complexes of carbonic anhydrase II (CAII, EC 4.2.1.1) and benzenesulfonamide inhibitors in the gas phase. Sustained off-resonance irradiation collision-induced
Ryuta Saito et al.
Acta crystallographica. Section D, Biological crystallography, 60(Pt 4), 792-795 (2004-03-25)
Carbonic anhydrase (CA) is a zinc-containing enzyme that catalyzes the reversible hydration of CO2 to HCO3-. In eukaryotes, the enzyme plays a role in various physiological functions, including interconversion between CO2 and HCO3- in intermediary metabolism, facilitated diffusion of CO2
Xiuhong Shan et al.
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Bernardo V Alvarez et al.
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Carbonic anhydrase enzymes (CA) catalyze the reversible hydration of carbon dioxide to bicarbonate in mammalian cells. Trans-membrane transport of CA-produced bicarbonate contributes significantly to cellular pH regulation. A body of evidence implicates pH-regulatory processes in the hypertrophic growth pathway characteristic
Laurie C Hofmann et al.
Journal of experimental botany, 64(4), 899-908 (2013-01-15)
The concentration of CO(2) in global surface ocean waters is increasing due to rising atmospheric CO(2) emissions, resulting in lower pH and a lower saturation state of carbonate ions. Such changes in seawater chemistry are expected to impact calcification in
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