| 1. | Review of high - salinity organic wastewater treatment
高盐度有机废水处理研究进展 |
| 2. | Experimental results show that desorption of particulate trace metals by waters of high salinity is limited due to dynamical processes . 6
另一方面，因受到受到动力学因素控制，高盐度水对固相中金属的解吸作用是有限的。 |
| 3. | For environmental concerns , a proper design of the brine outfall is essential to enable the end discharge mix rapidly with the ambient coastal waters
出于环境保护考虑，保证海水淡化后产生的高盐度尾液能够迅速与受纳海水掺混的排放口设计显得尤为重要。 |
| 4. | ( 2 ) there was a combined effect of salinity and alkalinity in mixed salt - alkaline stress , and this effect was more great than either simple saline stress or alkaline stress
( 2 )混合盐碱胁迫中的盐度和碱度( ph )间具有协同效应，即高盐度与高ph加合后对高粱幼苗的危害作用明显大于各因素的单独作用。 |
| 5. | During the periods of 12ka , 60ka , 118 - 130ka , the decreasement of summer monsoon resulted in the decreasement of sw monsoon , then correspondingly , the less high salinity water mass make this area low salinity
在12ka 、 60ka 、 118 - 130ka 、 240 - 250ka几个时期由于夏季季风的减弱，引起西南季风流减少，从西边过来的高盐度水团的减少使该区盐度降低。 |
| 6. | There are three main genetic types : ( 1 ) biogas generated in high - latitude and low - temperature permafrost zone : ( 2 ) biogas generated in high salinity environment in high elevation ; ( 3 ) biogas in shallow pay generated in recent sediment
其主要成因类型有3种：高纬度低温，永久冻土带下形成生物气；高海拔、高盐度环境下形成生物气；现代沉积物形成浅层生物气。 |
| 7. | The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ) , micritic limestone , grainstone and micritic dolostone which were laid down in the shallow - water to bathyal , high - salinity and enclosed to semi - enclosed lake systems
五道梁群湖相碳酸盐岩分为生物粘结灰岩（叠层石） 、泥晶灰岩、颗粒灰岩与泥晶白云岩四大类，反映出沉积环境为一个具有浅水半深水、高盐度、半封闭封闭特点的综合湖泊系统。 |
| 8. | The charac teristics of homogenization temperature and salinity data also reports that this high - salinity inclusions were not generated by aqueous fluid immiscibility or boiling in ore - forming processes , but generated directly from a water - saturated crystallizing magmatic melt and that the main mechanism of ore deposition is the mixing of magmatic fluid and underwater not boiling of hydrothermal solution
均一温度和盐度特征还表明，高盐度包裹体不是由热水溶液的不混溶作用或沸腾作用形成的，而是由岩浆熔体直接分离的卤水形成的；沸腾作用对矿质沉淀的作用不大，而流体的混合作用是银山矿床矿质沉淀的主要机制。 |
| 9. | On the basis of this , the paper specially discusses the ore precipitating mechanism and the ore origin . fluid - inclusion observations and microthermometric data suggest that the ore - forming fluid is middle - low temperature hydrothermal solution , it also reports the presence of high - salinity inclusions containing hilite in porphyry rock and ore - hosted quartz vein
流体包裹体岩相学和显微测温学研究表明，银山矿床成矿流体属于中低温热液范畴，在石英斑岩和多金属矿脉中都发现有含石盐子矿物的高盐度流体包裹体。 |
| 10. | Ammonifiers in suzhou creek can not use inorganic nitrogen and carbamide as nitrogen source ; additional carbon source and garbage lixivium have little influence on ammonifiers growth ; high content of salt and low temperature restrain ammonifiers growth ; alkalescent condition has little influence on ammonifiers , but acidic condition restrain ammonifiers growth ; the biomass of ammonifiers are not necessary correlated with the function of ammonifiers , adding glucose with 1g / l content into the water sample obviously promote the growth and function of ammonifiers . physiological groups of bacteria play significant role in the translation and
苏州河的氨化菌无法利用无机氮和尿素作为氮源；在营养条件充足时添加额外c源和富含有机物的垃圾浸出液对氨化菌的生长基本无影响；高盐度和低温抑制氨化菌生长；碱性条件对氨化菌的生长影响不大，酸性条件对氨化菌生长具有抑制作用；氨化菌生物量的消长与转氨活性之间不存在必然联系， 1g / l的葡萄糖对苏州河水样中氨化菌的数量和转氨功能具有明显的促进作用。 |
