Academic literature on the topic 'Gadolinium Anomaly'
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Journal articles on the topic "Gadolinium Anomaly":
Yayama, H., and A. Tomokiyo. "Electrical resistivity anomaly and specific heat in gadolinium-hydrogen solid solution." Journal of Alloys and Compounds 192, no. 1-2 (February 1993): 185–87. http://dx.doi.org/10.1016/0925-8388(93)90226-d.
Zhang, Jue, Zhuhong Wang, Qixin Wu, Yanling An, Huipeng Jia, and Yuanyi Shen. "Anthropogenic Rare Earth Elements: Gadolinium in a Small Catchment in Guizhou Province, Southwest China." International Journal of Environmental Research and Public Health 16, no. 20 (October 22, 2019): 4052. http://dx.doi.org/10.3390/ijerph16204052.
Rozemeijer, J., C. Siderius, M. Verheul, and H. Pomarius. "Tracing the spatial propagation of river inlet water into an agricultural polder area using anthropogenic gadolinium." Hydrology and Earth System Sciences Discussions 9, no. 1 (January 30, 2012): 1411–34. http://dx.doi.org/10.5194/hessd-9-1411-2012.
Taha, Birra, Taihui Li, Daniel Boley, Clark C. Chen, and Ju Sun. "Detection of Isocitrate Dehydrogenase Mutated Glioblastomas Through Anomaly Detection Analytics." Neurosurgery 89, no. 2 (April 22, 2021): 323–28. http://dx.doi.org/10.1093/neuros/nyab130.
Shah, M. D., and B. Want. "Dielectric and conducting behavior of gadolinium–terbium fumarate heptahydrate crystals." Journal of Advanced Dielectrics 05, no. 03 (September 2015): 1550020. http://dx.doi.org/10.1142/s2010135x15500204.
Elbaz-Poulichet, Françoise, Jean-Luc Seidel, and Clara Othoniel. "Occurrence of an anthropogenic gadolinium anomaly in river and coastal waters of Southern France." Water Research 36, no. 4 (February 2002): 1102–5. http://dx.doi.org/10.1016/s0043-1354(01)00370-0.
Rozemeijer, J., C. Siderius, M. Verheul, and H. Pomarius. "Tracing the spatial propagation of river inlet water into an agricultural polder area using anthropogenic gadolinium." Hydrology and Earth System Sciences 16, no. 8 (August 2, 2012): 2405–15. http://dx.doi.org/10.5194/hess-16-2405-2012.
Knappe, Andrea, Peter Möller, Peter Dulski, and Asaf Pekdeger. "Positive gadolinium anomaly in surface water and ground water of the urban area Berlin, Germany." Geochemistry 65, no. 2 (May 2005): 167–89. http://dx.doi.org/10.1016/j.chemer.2004.08.004.
Harrowfield, JM, WM Lu, BW Skelton, and AH White. "Structural Systematics of Rare Earth Complexes. III. Structural Characterization of Lanthanoid(III) Picrate Hydrates: Gadolinium Picrate Dodecahydrate—an X-Ray-Induced Phase Modification?—and Some General Aspects of the Structural Chemistry of Lanthanoid Picrates." Australian Journal of Chemistry 47, no. 2 (1994): 349. http://dx.doi.org/10.1071/ch9940349.
Inoue, Kazumasa, Masahiro Fukushi, Akira Furukawa, Sarata Kumar Sahoo, Nimelan Veerasamy, Ken Ichimura, Shogo Kasahara, et al. "Impact on gadolinium anomaly in river waters in Tokyo related to the increased number of MRI devices in use." Marine Pollution Bulletin 154 (May 2020): 111148. http://dx.doi.org/10.1016/j.marpolbul.2020.111148.
Dissertations / Theses on the topic "Gadolinium Anomaly":
Louis, Pauline. "Origine, comportement et devenir des Terres Rares dans les installations de traitements des eaux résiduaires urbaines et les milieux récepteurs associés." Electronic Thesis or Diss., Université de Lorraine, 2021. https://docnum.univ-lorraine.fr/ulprive/DDOC_T_2021_0021_LOUIS.pdf.
Rare Earths Elements (REEs) are naturally present in water due to the erosion of rocks. They are used in human activities (new technologies, energy, agriculture and medicine). These ever-increasing uses eventually disrupted the geochemical and life cycle of REEs and led to the enrichment (positive anomaly) of some REEs in the hydrosphere (La, Ce, Sm and Gd). For anthropogenic Gd, pollution derives from conventional wastewater treatment plants (WWTPs) which are not able to remove the organic complex form of Gd used in MRI analyses. Four areas were therefore studied in order to better understand the behavior of the REEs: the French basin of the Moselle River, the Danube river basin as a whole, the WWTP of Grand Nancy, and the constructed wetland downstream the WWTP of Grand Reims. Along the Moselle River, the presence of positive Gd anomalies and a regular LREEs depletion/ HREEs enrichment pattern on sandstone/limestone substrates were the most distinctive features. In the Danube basin, the positive Gd anomaly ranged from 1.8 to 37.4 in surface water and up to 80.8 in groundwater, showing contamination of alluvial wells. Within the Greater Nancy STEU, the greatest Gd inflows were observed during weekdays (Tuesday and Wednesday), and at the end of the day (7 p.m. to 10 p.m.). Treatment processes did not affect anthropogenic Gd, but increased LREE/HREE fractionation. The waters of the artificial wetland were those with the highest values of positive Gd anomalies (up to 4500). It was shown that the magnitude of Gd anomalies depended on the methodological approach chosen for their calculation. The choice of a threshold value to identify the presence of an anthropogenic Gd anomaly may therefore be basin dependent and may be tricky in areas where anthropogenic pressure is low