Qco remained relatively constant between pH 4-6, ascended slowly between pH 6-8 and then rapidly with further increasing pH. Ionic strength and iron chemistry had little influence on Qco.
Qco在pH4-6时保持相对稳定,pH6-8时缓慢增长,随着pH的进一步增加迅速升高。离子强度和铁对Qco几乎没有影响。
The temperature dependence of Qco can be characterized by the Arrhenius equation with the activation energies of freshwater samples being higher than those of salty samples.
Qco与温度的关系服从线性阿伦尼乌斯行为,低盐度水样的反应活化能高于高盐度水样。
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