uto/dbfile/file?db=121121&rid=140&fid=100000115" style="height: 220px; width: 150px;perspective-origin: 75px 110px; transform-origin: 75px 110px; font: 12px 微软雅黑; " />

uto/dbfile/file?db=121121&rid=140&fid=100000115198px; width: 770px; perspective-origin: 385px 99px; transform-origin: 385px 99px; font: 12px 微软雅黑; margin: 10px 0px 0px; padding: 0px; " id="UL_12">
• 标题：Major, trace, and rare earth element geochemistry of the Ayder and İkizdere (Rize, NE Turkey) geothermal waters: Constraints for water–rock
• 关键词：Geothermal water,Hydrogeochemistry,Rare earth elements,Rize geothermal fields,Turkey
• 作者：Esra Hatipoğlu Temizel, Fatma Gültekin, Arzu Fırat Ersoy

uto/dbfile/file?db=121121&rid=140&fid=116" title="全文下载" style="background-position: 0px -188px; color: rgb(40, 139, 222); display: block; float: left; height: 24px; text-align: center; text-decoration: none solid rgb(40, 139, 222); text-size-adjust: 100%; width: 60px; column-rule-color: rgb(40, 139, 222); perspective-origin: 30px 12px; transform-origin: 30px 12px; caret-color: rgb(40, 139, 222); background: rgba(0, 0, 0, 0) url(https://www1.pconline.com.cn/2015/dl/common/images/bg.png) no-repeat scroll 0px -188px / auto padding-box border-box; border: 0px none rgb(40, 139, 222); border-radius: 3px; font: 12px / 24px \"Microsoft Yahei", tahoma, HELVETICA; list-style: outside none none; margin: 20px 10px 10px; outline: rgb(40, 139, 222) none 0px; " id="A_1">全文下载

This study aims to determine the sources of rare earth elements (REEs) in the geothermal and cold waters of the Ayder and İkizdere (Rize) geothermal fifields (NE Turkey). The difffferentiation stages of REEs in water–rock interactions as well as the migration processes of aqueous complexes of rare earth elements (REEs) in the waters were evaluated. Based on results for major ions, the İkizdere geothermal water with a temperature of 61 °C can be classifified as Na-Ca-HCO3 type water, whereas the Ayder geothermal water with a temperature of 54 °C can be classifified as Na-Ca-CO3−SO4 type water. ∑REE concentrations were between 0.64–2.13 μg/L in the İkizdere geothermal fifield and between 0.01–0.32 μg/L in the Ayder geothermal fifield. As well as lower pH values, the waters in the İkizdere geothermal fifield were found to have higher REE concentrations than those of the Ayder geothermal fifield. Geochemical characteristics of REEs from the host rocks and water samples indicate that the REEs are derived from granite and granodiorite host rocks. Normalized REE plots for the host rocks and waters showed similar patterns, and in particular, the waters interacting with granitic rocks display a pronounced positive Eu anomaly and a less clear Ce anomaly. The positive Eu anomaly in the altered surrounding rocks is associated with argillization of feldspars in the granitic host rocks that the waters have passed through. Application of a speciation model showed that amorphous iron oxy-hydroxide complexes of REEs were signifificant for a pH value of nearly 9 in the Ayder geothermal waters whereas flfluoride complexes are dominant in