摘要
选择分解有机磷能力较强的 3株细菌和溶解磷矿粉较强的 4株细菌 ,砂培 4周后 ,用不同的方法测定水浸提液中磷的含量。发现不同的细菌解磷能力差异很大 ,细菌在分解磷化合物的同时 ,一部分磷被细菌同化 ,一部分以无机磷酸盐状态贮藏在细菌细胞内。直接测定浸提液中无机磷酸盐的含量 ,将大大低估细菌的解磷能力 ,必须将浸提液消煮 ,才能比较正确地反映细菌分解磷的能力。
Three bacteria of decomposing lecithin and 4 bacteria of dissolving aptite were incubated for 4 weeks with sand media respectively. Phosphorus in the sand was extracted with distilled water and measured by different methods. It was found that the bacteria have a quite different ability to release P from the materials. Part of the P released became organic phosphorus compounds in microbial tissue. However, a large amount of the P was reserved in microbial cells in a form of phosphates. The direct measurement of P in the extract by molybdenum blue method would underestimate the capacity of the bacteria to release P from the materials. The correct approach was that the sand was fumigated with chloroform and then digested with acid before the measurement by molybdenum blue method.
出处
《微生物学通报》
CAS
CSCD
北大核心
2001年第1期1-4,共4页
Microbiology China
基金
北京市自然科学基金重点资助项目!(No.6 9710 0 3)