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Our previous studies were mainly carried out on amended soils and it is well established that the availability of metals in such soils is far higher than it is in real soils (e.g. [63,64]).
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We found that the adsorption was very high in all the soils, and it was particularly influenced by the soil clay content and CEC and negatively related to pH and phosphorus.
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The spores can survive for years in the soil and it is through spores that the disease is spread.
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Kaolin is used as the model clayey soil, and it is amended with various amounts of Ca-bentonite (7.8–8.4%) and zeolite (10 40%) to prepare zeolite-amended kaolin bentonite backfills.
Kaolin is used as the control clayey soil and it is amended with different contents of Ca-bentonite, 0 (kaolin alone), 5, 10, and 15% (by dry weight basis), to prepare the clayey soil/Ca-bentonite backfills.
The condition of the soil microbial growth is affected by various environmental factors in the soil, and it is one of the most sensitive indicators for the change of the soil quality at the same time (Chen et al. 2007), whose number and distribution can reflect the subtle change of soil ecological system.
Kaolin is used as the base clayey soil, and it is amended with Ca-bentonite at three content levels (5, 10 and 15% by dry weight) to prepare the backfill samples.
The method is compared to standard methods for measuring pH in soil, and it is demonstrated that such standard methods in extreme cases can give differences of up to 2 pH units compared to the in situ pH.
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