RARE EARTH ELEMENTS IN SURFACE SEDIMENTS OF WESTERN SOUTH YELLOW SEA AND THEIR PROVENANCE IMPLICATIONS

2012 ◽  
Vol 32 (1) ◽  
pp. 11-18 ◽  
Author(s):  
Gang XU ◽  
Jian LIU ◽  
Xianghuai KONG ◽  
Junqiang ZHANG ◽  
Jiandong QIU
2014 ◽  
Vol 955-959 ◽  
pp. 427-430
Author(s):  
Zhen Ya Dou ◽  
Gang Xu ◽  
Jiao Wang

Analyses of Rare Earth Element were made for the 486 surface samples from the western South Yellow Sea in this paper. It was found that the grain size dominates the distribution of the elements. Their contents rise with the decrease of the mean grain size. Their contents was also effected by the minerals at certain stations. The parameters of the Rare Earth Element denote the surface sediments are mostly from Yellow River in the study area.


2011 ◽  
Vol 31 (3) ◽  
pp. 11-16 ◽  
Author(s):  
Xianhong LAN ◽  
Xianjun ZHANG ◽  
Xinbo LIU ◽  
Rihui LI ◽  
Zhixun ZHANG

2017 ◽  
Vol 114 (2) ◽  
pp. 1103-1109 ◽  
Author(s):  
Jingxi Li ◽  
Chengjun Sun ◽  
Li Zheng ◽  
Xiaofei Yin ◽  
Junhui Chen ◽  
...  

2009 ◽  
Vol 29 (5) ◽  
pp. 291-300 ◽  
Author(s):  
Zhaokai Xu ◽  
Dhongil Lim ◽  
Jinyong Choi ◽  
Shouye Yang ◽  
Hoisoo Jung

2013 ◽  
Vol 448-453 ◽  
pp. 313-316
Author(s):  
Jing Jun Liu ◽  
Hao Yue Xiao ◽  
Ying Liu

The concentrations and fractionation of 14 rare earth elements (REEs) such as La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb and Lu in filtered water, suspended particles and surface sediments at 10 sampling sites from Gansu, Ningxia and Inner Mongolia sections of the Yellow River of China were studied by HR-ICP-MS. The results demonstrated that the total concentrations of REEs (REEs) in filtered water varied from 0.017 to 0.079 μg/L and had high concentration at S3 (0.079), S1 (0.070) and S4 (0.063) in Inner Mongolia section, while in suspended particles and surface sediments, the ranges were 148.9-246.8 mg/kg (mean 176.4) and 109.9-252.0 mg/kg (mean 179.9), respectively, and showed high concentration at S9 (246.8), S7 (252.0), S8 (229.8) in Baiyin (Gansu section) and S1 (209.5) in Baotou (Inner Mongolia section). The ratios of L/H, δEu and δCe in suspended particles and surface sediments implied light-REEs enrichment in the water compared with the background value of Chinese soil. And the chondrite-normalized REEs patterns of the suspended particles and surface sediments also showed light REEs enrichment at S1, S7, S8 and S9. The high concentrations of REEs in the Yellow River were probably due to the weathering of soil and anthropogenic activities near the river.


2014 ◽  
Vol 36 (4) ◽  
pp. 383-394
Author(s):  
Inah Seo ◽  
Sang Joon Pak ◽  
Hyeong Kiseong ◽  
Gee-Soo Kong ◽  
Jonguk Kim

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