厦门大学学报(自然科学版)
廈門大學學報(自然科學版)
하문대학학보(자연과학판)
JOURNAL OF XIAMEN UNIVERSITY (NATURAL SCIENCE)
2010年
2期
238-241
,共4页
海水%溶解态磷酸盐氧同位素组成%富集%分离%纯化
海水%溶解態燐痠鹽氧同位素組成%富集%分離%純化
해수%용해태린산염양동위소조성%부집%분리%순화
seawater%dissolved phosphate oxygen isotope composition%preconcentration%separation%purification
海水中溶解态磷酸盐的氧同位素组成(δ~(18) O_p)是海洋磷循环研究的有效示踪剂之一.海水中溶解态磷酸盐的富集、分离与纯化研究是测定海水磷酸盐氧同位素组成的基础.通过对国内外海水中磷酸盐氧同位素组成的测定方法进行查阅,选择改进后的MAGIC-CePO_4沉淀-阳离子交换树脂法对海水中溶解态磷酸盐进行富集、分离与纯化,并对实验条件进行了探讨.实验结果表明,所采用的方法对于3种不同溶液体系3个步骤的磷酸盐平均回收率分别为92.8%, 88.2%和98.3%,全流程磷酸盐回收率达到80%以上,因此可作为海水磷酸盐氧同位素测定的重要前提.
海水中溶解態燐痠鹽的氧同位素組成(δ~(18) O_p)是海洋燐循環研究的有效示蹤劑之一.海水中溶解態燐痠鹽的富集、分離與純化研究是測定海水燐痠鹽氧同位素組成的基礎.通過對國內外海水中燐痠鹽氧同位素組成的測定方法進行查閱,選擇改進後的MAGIC-CePO_4沉澱-暘離子交換樹脂法對海水中溶解態燐痠鹽進行富集、分離與純化,併對實驗條件進行瞭探討.實驗結果錶明,所採用的方法對于3種不同溶液體繫3箇步驟的燐痠鹽平均迴收率分彆為92.8%, 88.2%和98.3%,全流程燐痠鹽迴收率達到80%以上,因此可作為海水燐痠鹽氧同位素測定的重要前提.
해수중용해태린산염적양동위소조성(δ~(18) O_p)시해양린순배연구적유효시종제지일.해수중용해태린산염적부집、분리여순화연구시측정해수린산염양동위소조성적기출.통과대국내외해수중린산염양동위소조성적측정방법진행사열,선택개진후적MAGIC-CePO_4침정-양리자교환수지법대해수중용해태린산염진행부집、분리여순화,병대실험조건진행료탐토.실험결과표명,소채용적방법대우3충불동용액체계3개보취적린산염평균회수솔분별위92.8%, 88.2%화98.3%,전류정린산염회수솔체도80%이상,인차가작위해수린산염양동위소측정적중요전제.
Dissolved phosphate oxygen isotope composition(δ~(18) O_p) was an effective tracer of ocean phosphate cycle.The preconcentration,separation and purification of phosphate was the foundation of seawater phosphate δ~(18) O analysis.Some popular seawater phosphate δ~(18) O analysis methods were reviewed.Then MAGIC-CePO_4 coprecipitation-cation exchange resin separation method was choosed to preconcentrate,separate and purify the phosphate.Some basic experiment conditions were also discussed.The results indicate that the mean phosphate recoveries of three procedures for three systems are 92.8%,88.2%,98.3%,and the total recovery of phosphate is more than 80%,so this method can be served as a basic precondition to determine the oxygen isotope composition of dissolved phosphate in seawater.