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天然存在的磷灰石是细菌和藻类生长的正磷酸盐来源。

Naturally occurring apatite as a source of orthophosphate for growth of bacteria and algae.

机构信息

Department of Biology, University of Waterloo, N2L 3G1, Waterloo, Ontario, Canada.

出版信息

Microb Ecol. 1977 Jun;4(2):105-17. doi: 10.1007/BF02014281.

Abstract

Several naturally occurring calcium-phosphate apatites which varied in crystalline structure and ionic composition were added as crystals of different particle size to P-free (<1μg/liter total P) nutrient media. Sufficient ortho-PO 4 (3-) was released by the partial dissolution of apatite crystals at limnetic pH levels (pH 7.8) to support growth of several unialgal-mixed bacterial cultures. The biomass produced by mixed populations increased as the amount of available apatite was increased and as the pH of the media and the particle size of the apatite crystals were decreased. These findings suggest that although apatite characteristically displays reduced solubility under alkaline conditions, the tons of apatite which are continuously entering aquatic environments as erosion material may be contributing to the P loading of those ecosystems.

摘要

将几种晶体结构和离子组成不同的天然钙磷磷灰石作为不同粒径的晶体添加到无磷(总磷<1μg/l)营养介质中。在敞水(pH 7.8)条件下,磷灰石晶体的部分溶解释放出足够的正磷酸盐(PO 4 3-),以支持几种单藻混合细菌培养物的生长。混合种群产生的生物量随着可用磷灰石量的增加以及培养基的 pH 值和磷灰石晶体的粒径的降低而增加。这些发现表明,尽管磷灰石在碱性条件下通常显示出降低的溶解度,但作为侵蚀物质不断进入水生环境的磷灰石可能会导致这些生态系统的磷负荷增加。

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