Werner H P, Baer E, Dibelius G, Dittrich H, Ederhof A, Egler W, Ernst G, Roller W, Wurz D
Zentralbl Bakteriol B. 1979 Sep;169(1-2):39-134.
The second in the series "Microbial emission, immission and changes in the germ count in the cooling water of wet cooling towers" describes measuring methods and results of the measurements for determining the emission values and the changes in the germ count in the cooling system. The content of colony-forming units (KBE) in the cooling water varied widely, depending on the germ content of the surface water and the preparation of the cooling water (filtration, chemical conditioning). In summer the KBE values were as a rule higher than the values recorded in winter (factor of about 10). The introduction of cooling tower water into the surface water thus did not result in any noticeable changes in germ content, either in summer or in winter. An emission rate of 8.3 10(7) KBE/s (CSA) measured at the top of the cooling tower was the maximum emission value recorded. This resulted in a total germ content in the plume of 1.2 . 10(4) KBE/m3. In order to place this finding into perspective, it should be noted that fluctuations in the KBE values of the air of considerably more than 1000 KBE/m3 can occur because of biological release and meteorological conditions alone (see IVth communication). The KBE-P values recorded (content of particles with units which are capable of forming colonies) in the plume were of the same order as the KBE values. From this it can be concluded that the drops of cooling water which are swept away with the plume are normally only charged with individual colony-forming units. It is worth noting that the KBE values of the plume are only indirectly dependent on the KBE values of the cooling water used in the cooling tower.
“湿式冷却塔冷却水中微生物排放、沉降及细菌数量变化”系列文章的第二篇描述了用于确定冷却系统中排放值和细菌数量变化的测量方法及测量结果。冷却水中菌落形成单位(KBE)的含量差异很大,这取决于地表水的细菌含量以及冷却水的预处理方式(过滤、化学处理)。夏季的KBE值通常高于冬季记录的值(约为10倍)。因此,无论是夏季还是冬季,将冷却塔水引入地表水均未导致细菌含量出现任何明显变化。在冷却塔顶部测得的排放率为8.3×10⁷ KBE/s(CSA),这是记录到的最大排放值。这导致羽流中的细菌总含量为1.2×10⁴ KBE/m³。为了正确看待这一发现,应当指出,仅由于生物释放和气象条件,空气中KBE值的波动就可能大大超过1000 KBE/m³(见第四次通讯)。在羽流中记录到的KBE - P值(能够形成菌落的颗粒含量)与KBE值处于同一数量级。由此可以得出结论,随羽流带走的冷却水通常仅携带单个菌落形成单位。值得注意的是,羽流中的KBE值仅间接取决于冷却塔中使用的冷却水的KBE值。