1) δ~(18)O
δ18O
1.
In this paper,the variations of δ~(18)O of precipitation and the relationships between δ~(18)O in precipitation and temperature and precipitation amount are analyzed by using the meteorological data observed in the summer of 2004 at Baidi,Wengguo and Duixiang Hydrographic Stations around the Yamzho Lake on the Tibetan Plateau.
根据青藏高原南部羊卓雍错流域白地、翁果和堆乡3个水文站2004年1~10月降水中δ18O的测定结果,分析了该流域降水中δ18O的变化特征及其与温度和降水量之间的关系。
2.
According to the precipitation and δ~(18)O obtained during GAME-Tibet IOP, based on the knowledge that the δ~(18)O in precipitation is lower which is from the ocean air mass and higher from that of the local evaporation, the water vapor sources could be identified from the δ~(18)O value in precipitation.
根据GAME-Tibet加强观测期间取得的降水量和δ18O资料,基于来自海洋性气团的水汽形成的降水中δ18O较低、来自局地蒸发形成的降水中δ18O较高这一认识,尝试性地给出了划分不同来源水汽的标准。
3.
The Nanyong-3 well core from the Yongshu Atoll lagoon in the Nansha Islands is measured by high-precision TIMS U serious dating, and then the δ~(18)O of the benthonical Calcarina hispida[Brady] in the sample is analysized.
通过测试了采自南沙群岛永暑礁湖中的南永3井岩芯的高精度TIMS铀系年龄,分析了样品中底栖有孔虫茸刺距轮虫(Calcarinahispida)δ18O,计算了历史时期表层海水温度和气温,结果自330AD以来可划分为4个凉和4个热的气候期,还细分出37个气候凉热波动亚期。
2) δ 18 O
δ18O
1.
Climate change since the 1920s was rec onstructed based on annual δ 18 O from a 102.
0 7m冰芯记录中δ18O的年变化 ,恢复了青藏高原中部 2 0世纪 2 0年代以来的气候变化 。
3) δ 18O values
δ18O值
4) ice core δ18O
冰芯δ18O
5) Light δ18O and δ13C excursions
δ18O和δ13C轻值
6) δ_1 phase
δ1相
补充资料：(C14-18、C16-18不饱和)脂肪酸乙二醇酯
CAS：2884-59-5
中文名称：(C14-18、C16-18不饱和)脂肪酸乙二醇酯
英文名称：Fatty acids, C14-18 and C16-18 -unsatd., esters with ethylene giycol
中文名称：(C14-18、C16-18不饱和)脂肪酸乙二醇酯
英文名称：Fatty acids, C14-18 and C16-18 -unsatd., esters with ethylene giycol
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条