| 1. | Bentonite is an expandable three-layer clay mineral .
皂土是一种可膨胀的土层粘土矿物。 |
| 2. | They are stabilized through absorption by clay minerals .
它们通过粘土矿物的吸收作用而得到稳定。 |
| 3. | Two basic types of clay minerals are present in most soils .
大多数土壤中出现了两类主要的粘土矿物。 |
| 4. | The ability of clay minerals to catalyse decarboxylation has long been recognised .
粘土矿物能催化脱羧基作用是早已认识到的问题。 |
| 5. | It occurs as an exchangeable base in the clay mineral and organic fractions of soils .
钙是以交换性盐基在粘土矿物及土壤的有机部分出现的。 |
| 6. | The surface area of crystalline clay minerals is highly dependent on the extent of lattice expansion .
结晶粘土矿物的表面积主要依赖于晶格膨胀的程度。 |
| 7. | The smectites are the most effective of the clay minerals as catalysts of these organic reactions .
对这些有机反应，蒙脱石是粘土矿物中最有效的催化剂。 |
| 8. | Specific evidence for coordination complexes between pesticides and clay minerals is quite limited .
关于农药和粘土矿物之间的配位络合的明确证据是十分有限的。 |
| 9. | These changes reflect the effects of burial diagenesis on the originally deposited clay mineral assemblage .
这种变化反映了埋藏成岩作用对原来沉积的粘土矿物组合的影响。 |
| 10. | Essentially the catalytic properties of clay minerals arise because of their ability to donate protons or accept electrons in reaction mechanisms .
从本质上看，粘土矿物具有催化性质，这是因为粘土矿物在反应过程中能放出质子或接受电子。 |
