该委员会声称随着表层海水继续吸收大气中的二氧化碳，平均来说海洋将变得更加酸性。
The ocean will become more acidic on average as surface waters continue to absorb atmospheric CO2, the committee said.
不同土壤层次氧化甲烷的潜力也有差异，表层土比下层土高。
Different soil layers had various potential of methane oxidation. The surface layers were higher than the low layers.
并应用XPS对烧伤表层氧化膜组份进行了探讨。
The oxide film composition of burnt surface has been discussed by means of XPS.
应用推荐