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)
2009年
4期
570-575
,共6页
pH微电极%金属氧化物电极%沉积物%铱%钨
pH微電極%金屬氧化物電極%沉積物%銥%鎢
pH미전겁%금속양화물전겁%침적물%의%오
pH microelectrode%metal oxide electrode%sediments%iridium%tungsten
用改进的高温熔融碳酸盐法制备了铱和钨氧化物pH微电极,表征了金属氧化物电极的各项性能.所制备电极对pH有较好的线性响应,斜率在40~60 mV/pH ,接近理想能斯特响应.实验表明,铱氧化物微电极在长时间工作稳定性方面优于钨氧化物微电极,90%响应时间为5 s.铱氧化物微电极受盐度和氧气浓度影响很小,且经Nafion修饰后不受沉积物间隙水中还原性S2-的影响.把铱氧化物微电极应用于测量厦门西海域和九龙江河口的沉积物pH垂直剖面,发现pH在沉积物有氧和无氧深度界面(4~5 mm)达到最小,20 mm以深趋于稳定,符合沉积物生物地球化学规律.
用改進的高溫鎔融碳痠鹽法製備瞭銥和鎢氧化物pH微電極,錶徵瞭金屬氧化物電極的各項性能.所製備電極對pH有較好的線性響應,斜率在40~60 mV/pH ,接近理想能斯特響應.實驗錶明,銥氧化物微電極在長時間工作穩定性方麵優于鎢氧化物微電極,90%響應時間為5 s.銥氧化物微電極受鹽度和氧氣濃度影響很小,且經Nafion脩飾後不受沉積物間隙水中還原性S2-的影響.把銥氧化物微電極應用于測量廈門西海域和九龍江河口的沉積物pH垂直剖麵,髮現pH在沉積物有氧和無氧深度界麵(4~5 mm)達到最小,20 mm以深趨于穩定,符閤沉積物生物地毬化學規律.
용개진적고온용융탄산염법제비료의화오양화물pH미전겁,표정료금속양화물전겁적각항성능.소제비전겁대pH유교호적선성향응,사솔재40~60 mV/pH ,접근이상능사특향응.실험표명,의양화물미전겁재장시간공작은정성방면우우오양화물미전겁,90%향응시간위5 s.의양화물미전겁수염도화양기농도영향흔소,차경Nafion수식후불수침적물간극수중환원성S2-적영향.파의양화물미전겁응용우측량하문서해역화구룡강하구적침적물pH수직부면,발현pH재침적물유양화무양심도계면(4~5 mm)체도최소,20 mm이심추우은정,부합침적물생물지구화학규률.
Iridium oxide and tungsten oxide pH microelectrodes were fabricated by oxidizing the metal wires in sodium carbonate or lithium carbonate molten at high temperature.Experiments were carried out to characterize their working performance.The microelectrodes show good linear response to pH in buffer solution with a slope between 40 and 60 mV/pH,close to Nernst slope.Experimental results indicate that iridium oxide microelectrode has better performance than tungsten oxide microelectrode in long-time working stability.Iridium oxide microelectrode has a 90% response time of about 5 s,shorter than that of tungsten oxide microelectrode.Iridium oxide microelectrode is little affected by oxygen concentration,salinity,and the reducing agent of S2- ions in the pore water of sediments after being coated with a Nafion film.Iridium oxide microelectrodes were applied to measure pH profiles of sediment cores sampled from Xiamen Western Bay and Jiulong River Estuary.It was found that pH reach minimum values at oxic-anoxic interface of 4~5 mm depths within the sediments and tended to be stable at depths deeper than 20 mm.These results agree with the prediction of biogeochemistry in coastal sediments.