CAJ | 학술논문

在2011年7月利用35 SO2－4培养示踪法测定九龙江河口两个站位（A 站位位于咸淡混合区，盐度3～5；B 站位位于海相区，盐度20～25）沉积柱中硫酸盐还原速率的垂直分布。结果显示 A 站位沉积柱中硫酸盐还原速率变化范围为54～2345 nmol／（cm3·d），从表层到底部先增大后减小，最大值出现在20 cm 深度附近；B 站位硫酸盐还原速率在24～987 nmol／（cm3·d）之间，分别在10 cm 和78 cm深度附近出现两个峰值，分别为876和987 nmol／（cm3·d）。综合分析两个站位孔隙水中 SO2－4、甲烷浓度和沉积物中总有机碳、温度和氧化还原电位的垂直变化趋势与其硫酸盐还原速率的分布规律，表明 A 站位沉积物中硫酸盐还原以有机矿化为主；B 站位受到有机质矿化和甲烷厌氧氧化的共同作用；两个站位硫酸盐还原速率及垂直分布趋势受孔隙水中 SO2－4浓度、有机质活性和温度的共同影响；根据各个层位硫酸盐还原速率估算两个站位硫酸盐还原通量（以硫计）分别为527．9和357．1 mmol／（m2·d），表明硫酸盐还原是九龙江河口有机质厌氧矿化的重要路径。
재2011년7월이용35 SO2－4배양시종법측정구룡강하구량개참위（A 참위위우함담혼합구，염도3～5；B 참위위우해상구，염도20～25）침적주중류산염환원속솔적수직분포。결과현시 A 참위침적주중류산염환원속솔변화범위위54～2345 nmol／（cm3·d），종표층도저부선증대후감소，최대치출현재20 cm 심도부근；B 참위류산염환원속솔재24～987 nmol／（cm3·d）지간，분별재10 cm 화78 cm심도부근출현량개봉치，분별위876화987 nmol／（cm3·d）。종합분석량개참위공극수중 SO2－4、갑완농도화침적물중총유궤탄、온도화양화환원전위적수직변화추세여기류산염환원속솔적분포규률，표명 A 참위침적물중류산염환원이유궤광화위주；B 참위수도유궤질광화화갑완염양양화적공동작용；량개참위류산염환원속솔급수직분포추세수공극수중 SO2－4농도、유궤질활성화온도적공동영향；근거각개층위류산염환원속솔고산량개참위류산염환원통량（이류계）분별위527．9화357．1 mmol／（m2·d），표명류산염환원시구룡강하구유궤질염양광화적중요로경。
Sulfate reduction rates were measured experimentally with 35 SO2-4 in sediment of A and B cores in coastal of Jiulong River Estuary in July of 2011.A and B cores were situated in the upper estuarine coast and seaward boundary respectively,with low salinity (3-5)and high salinity (20-25).Sulfate reduction rates volume-based values ranged from 54 to 2 345 nmol/(cm3 ·d)in vertical profile of A core,and the highest sulfate reduction rates occurred at 20 cm depth.Sulfate reduction rates varied from 24 to 987 nmol/(cm3 ·d)in B core,two peaks in sul-fate reduction rates profiles obviously appeared on the top 10 cm and at 78cm depth,with significantly high value of 876 nmol/(cm3 ·d)and 987 nmol/(cm3 ·d),respectively.Based on trends on the vertical profile of SO2-4 ,meth-ane concentration in pore water and total organic carbon,temperature and oxidation reduction potential in sediments of two cores,sulfate reduction is mainly dominated by organic mineralization in A Core,however sulfate reduction is controlled by the combination of organic matter mineralization and anaerobic methane oxidation in B Core.Mean-while sulfate reduction rates and the vertical distribution trends of it were affected by the availability of active or-ganic matter,temperature and SO2-4 concentration in the pore water in two cores.The depth-integrated sulfate re-duction rates were 527.9 mmol/(m2 ·d)and 357.1 mmol/(m2 ·d)within sulfate reduction zone in A Core and B Core respectively.Sulfate reduction is one of the major processes contributing to the mineralization of organic mat-ter in this estuary.