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1)  variably saturated soils
变饱和带
2)  unsaturated zone
非饱和带
1.
It mainly includes the transportation and transformation on contaminant in soil, unsaturated zone, underground water and clay impermeable layer, and numerical models stimulated the contaminant transportation.
系统地评述了近年来国内外对污染物在土壤、非饱和带、地下水和粘土防渗层中迁移转化规律研究的最新进展,以及模拟污染物迁移的数值模型,并提出了需要进一步解决的关键性问题,为环境污染的治理、控制污染和水资源管理与评价的研究提供了可靠依据。
2.
The utilization of soil water in the unsaturated zone is of significance for agriculture,forestry,stock raising and the local eco-system.
如何保持和利用非饱和带中的土壤水对农、林、牧生态系统具有重要意义。
3)  thermo-saturation zone
热饱和带
4)  saturation strips
饱和条带
1.
Effect of saturation strips at the crack-tips was taken into account.
研究了无限压电体内共线周期裂纹间的相互作用的问题,并且考虑了裂纹尖端的饱和条带作用。
5)  oil-saturated zone
油饱和带
1.
All secondary enlargement of quartz and albitization of potash feldspar in water-saturated zone (water layer) are stronger than those in oil-saturated zone.
油饱和带 (油层 )中石英次生加大和钾长石颗粒的钠长石化程度均低于水饱和带 (水层 ) ,石英次生加大边中的流体包裹体显微测温 (6 0~ 14 0℃ )表明 ,油饱和带与水饱和带中包裹体的温度相近 ,这说明油饱和带中石英次生加大在石油侵入后继续发育 ,但与水饱和带相比这种作用受到抑制。
6)  water-saturated zone
水饱和带
1.
All secondary enlargement of quartz and albitization of potash feldspar in water-saturated zone (water layer) are stronger than those in oil-saturated zone.
油饱和带 (油层 )中石英次生加大和钾长石颗粒的钠长石化程度均低于水饱和带 (水层 ) ,石英次生加大边中的流体包裹体显微测温 (6 0~ 14 0℃ )表明 ,油饱和带与水饱和带中包裹体的温度相近 ,这说明油饱和带中石英次生加大在石油侵入后继续发育 ,但与水饱和带相比这种作用受到抑制。
补充资料:(C14-18-饱和、C16-18-不饱和)脂肪酸钾盐
CAS:68002-80-2
分子式:C14-18 and C16-18-Unsaturated alkylcarboxylic acid potassium salts

中文名称:(C14-18-饱和、C16-18-不饱和)脂肪酸钾盐;牛油脂肪酸钾皂

英文名称:Fatty acids, C14-18 and C16-18-unsatd., potassium salts
C14-18 and C16-18-Unsaturated alkylcarboxylic acid, potassiumsalt
fatty acids, c14-18 and c16-18-unsatd., potassiumsalts
Fatty acids,C14-18 and C16-18-unsatd.,potassium salts
C14-18 and C16-18-Unsaturated alkylcarboxylic acid,potassiumsalt
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