Titlebook: Chemical Processes in Marine Environments; Antonio Gianguzza,Ezio Pelizetti,Silvio Sammartano Book 2000 Springer-Verlag Berlin Heidelberg

提名

Chao Yu,Guozheng Kang,Qianhua Kanere is qualitative and quantitative uncoupling between the water column and the sediments. In the case of organic matter, this bias is severe since most organic matter produced in surface waters is degraded in the water column and only a tiny fraction is buried in the sediments. Valid reconstruction

爆炸

AROMA

Mendacious

Gradient-Type Methods of Nonlinear Inversionme known that some interesting metals such as copper, zinc, iron, nickel, cobalt and probably more, participate in these reactions. This complexation changes the geochemistry of the metals by preventing them from being scavenged and thus increases their residence time in estuaries and the upper wate

簡(jiǎn)潔

Sabina Merlo,Paul Yager,Lloyd W. Burgesser, such as with hydroxide, carbonate or phosphate. Their solubility is increased by the formation of soluble complexes with the major anions. The concentrations of the vast majority of the metals in the oceans are usually much less than their solubility because they are scavenged from solution by i

Between

Doo-Man Oh,Patrick J. Sinko,Gordon L. Amidondrocarbons and more lately organometallic compounds. Organometallic compounds occur in the environment as a result of direct anthropogenic inputs or because they are naturally formed there. They are used in a wide variety of industrial processes sometimes at the percent level. Some organometallic fo

Acetabulum

On the Single-Point, Single-Dose Problemmethyl, ethyl, propyl, butyl, octyl, phenyl, etc.) through one or more carbon atoms. Their general formula can be indicated as R.SnX. (R = organic group; X = halide, nitrate, acetate, hydroxide, etc.; . =1 to 4). Because the tin-carbon bond is reported to be stable up to 200 °C (Zuckerman et al. 197

DEFT

Intracellular Metabolism of Lamivudinethe oceans are very large in absolute terms, the dilution is extremely high, leading to very low concentrations. This situation is generalised in Fig. 13.1. The consequences of low concentrations in the open oceans are that the possibilities for deficiency are high whereas those for toxicity are low

禁止,切斷

disparage

https://doi.org/10.1007/b105246 and toxicity. Dissolved Cr(III) has a strong tendency to adsorb to surfaces (Cranston and Murray 1978) and is characterized by a low solubility. Candidates for the solubility control of chromium(III) in natural waters are not fully understood. They include Cr(OH). (Baes and Mesmer 1976), mixed hydr