Experimental Method and Application of Rapid and Continuous Extraction of Reduced Inorganic Sulfur from Sediments
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摘要:
还原性无机硫是沉积物硫中最活跃的部分，其含量变化控制沉积物中铁、磷及重金属等元素的地球化学行为，在地质过程和环境污染方面都具有至关重要的影响。化学连续提取法是目前沉积物中硫形态提取基本方法，但常用的冷扩散法处理单个样品耗时长，难以实现对大批量样品的快速连续提取。为实现快速、准确地测定沉积物样品各形态还原性无机硫的含量，本文采用热蒸馏法，改进基于前人的三步提取过程，通过优化实验装置预先制备实验所需的二氯化铬溶液，实现了样品还原性无机硫形态的快速连续提取；以过氧化氢为氧化剂，将提取的各形态硫氧化为$\mathrm{SO}_4^{2-}$后采用离子色谱进行检测。选取三峡库区沉积物样品进行重复实验检验，得到提取酸挥发性硫、黄铁矿硫、元素硫的标准偏差(RSD，n=3)分别为5.26%、1.22%和3.09%，重复性较好。进一步对酸挥发性硫、黄铁矿硫、元素硫的加标回收率进行测定，得到这三种硫形态的回收率分别为92.8%、93.6%、94.1%。本实验方法采用的热蒸馏法对单个硫形态提取时间为1.5h，用时较短，玻璃装置连接便捷、操作简单，分析检测准确度好，实现了一套装置对沉积物还原性无机硫形态的连续提取，可适用于大批量样品的硫形态快速提取与检测。
要点(1) 所设计的实验装置实现了对各形态还原性无机硫的连续提取。
(2) 提取出的各形态还原性无机硫采用过氧化氢氧化为SO42-后，实现了离子色谱的统一检测。
(3) 三峡库区沉积物的研究显示，库区硫污染程度较低。
HIGHLIGHTS(1) Continuous extraction of reduced inorganic sulfur from sediments was achieved.
(2) All forms of reduced inorganic sulfur were oxidized to SO42- using H2O2 and then detected by ion chromatography.
(3) Three Gorges Reservoir sediments show low reduced inorganic sulfur content.
Abstract:BACKGROUNDSulfur is an active element with multiple chemical forms, which plays a vital role in the regulation of redox chemistry. Reduced inorganic sulfur (RIS) including acid volatile sulfur (AVS), elemental sulfur (ES) and pyrite sulfur (CRS) is the most active part of sulfur species in sediments and plays an important role in controlling the geochemical behavior of iron, phosphorus and heavy metals in sediments. Separation and determination of reduced inorganic sulfur in anoxic sediments are critical to ecological and geological studies of sulfur cycles.
Both distillation and diffusion methods can be effectively used to separate AVS, ES, and CRS in sediments. However, the current methods for extracting sulfur species are difficult to adapt to the large number of samples in geological and environmental research. Due to the reaction time, requirements of 24h for single sulfur species in the diffusion method limits the number of samples that can be processed on a timely basis. This limitation presents a problem for analyzing fresh anoxic sediment samples which have to be processed immediately to minimize the risk of sulfide re-oxidation. The detection method has the disadvantages of having a cumbersome testing process, long analysis time, and easy loss of sulfur components.
OBJECTIVESTo achieve efficient and continuous determination of reduced inorganic sulfur forms in bulk sediment samples.
METHODSThe method used in this experiment was improved based on the thermal distillation method, which was used to continuously extract the reduced inorganic sulfur from sediments. The reaction flask used in the experiment was a three-head round-bottom flask. A nitrogen flushing pipe, a condenser tube and two injection tubes were connected to each of the small necks. For the AVS procedure, 1.00g sediment sample reacted with 10mL of 6mol/L HCl under nitrogen gas at an elevated temperature (90℃) to convert reduced sulfur species into hydrogen sulfide which was subsequently carried by a nitrogen gas stream into a trap. For the CRS procedure, 20mL of CrCl2 solution was added to the sediment in the distillation flask after the AVS procedure, and 10mL of 6mol/L HCl was immediately placed in the flask at an elevated temperature (90℃), flushed with nitrogen. For the ES procedure, 20mL DMF were poured into the sample flask which contained acid and CrCl2 solutions from the previous procedure. 20mL of CrCl2 solution and 10mL of 6mol/L HCl were injected into the flask, and the reaction was allowed to take place at 90℃ purging with nitrogen. During the entire distillation process, H2S gas was absorbed by NaOH solution, and then oxidized by H2O2 to
$\mathrm{SO}_4^{2-}$ . The concentrations of$\mathrm{SO}_4^{2-}$ were obtained by ion chromatography.RESULTSRepeatability experiments (n=3) were conducted on sediment samples from the Three Gorges Reservoir area and the mean values of acid volatile sulfur, elemental sulfur and pyrite sulfur were obtained as 0.19, 0.37 and 3.10μmol/g, respectively. The relative standard deviations (RSD) of the experimental results were 5.26%, 1.22% and 3.09%, respectively. In order to test the effectiveness of the distillation procedures, Na2S·9H2O, pyrite and S were added in the sediment to reveal the corresponding standard recoveries. An average of 92.8% of the added Na2S·9H2O was recovered by the AVS diffusion method. An average of 93.6% of the added pyrite was recovered by the CRS diffusion method. An average of 94.1% of the added elemental sulfur was recovered by the ES diffusion method. In the literature, recovery of AVS by the improved diffusion method ranged from 82.01% to 108.71%, and recovery of ES ranged from 92.25% to 98.08% (n=3), respectively.
The modified apparatus presented in this paper was an economic version which uses rubber and glass parts. The method provided the advantages of lower sample weighing, and simple operation. Compared with the diffusion method (24h), the extraction time for individual sulfur forms by our distillation method was just 1.5h. The recoveries achieved by the method are comparable to those reported for earlier methods. In addition, the results are more like the data on reduced inorganic sulfur content obtained by Hongbin Yin after measuring sediment samples from Taihu Lake using the modified cold diffusion method, indicating that the method designed in this study has a high degree of confidence.
Geochemical processes of sulfur in river aquatic systems play a crucial role in environmental evolution. In this study, the distributions and seasonal variation of reduced inorganic sulfur (RIS) in the Three Gorges Reservoir area surface sediments were investigated. Surface sediment samples were collected from 8 points in the section from Yunyang to Zigui in the Three Gorges Reservoir area in August and December 2017. The result showed that the AVS and ES contents were higher in summer than in winter, and the trend of RIS in the section from Yunyang to Zigui was roughly decreasing, with obvious seasonal and spatial changes. Low sulfur pollution in the Three Gorges Reservoir area was observed.
CONCLUSIONSThe improved thermal distillation method and apparatus in this study have significant advantages in the extraction efficiency of reduced inorganic sulfur from sediments. The extraction time of this study for individual sulfur form is 1.5h, less than the diffusion method. The established analytical method has good precision and accuracy, which is suitable for investigation studies with large numbers of samples such as environmental research and geological surveys.
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硫(S)是水生生态系统中最重要的生源要素之一，影响生态系统的结构、功能和生产力。硫元素在参与植物氨基酸、叶绿素的合成以及光合作用中的碳水化合物代谢、植物呼吸等过程中发挥重要的作用[1-4]。水体沉积物中硫的化学价态多变(从-2到+6价)，按照其存在形态分为无机硫和有机硫两类[5]。已有研究表明无机硫可占植物硫吸收总量的55%以上[6]。无机硫主要包括：酸挥发性硫化物(AVS)、黄铁矿硫(CRS)和元素硫(ES)，这些都为还原性无机硫。还原性无机硫也是沉积物中硫形态最活跃的部分，不仅影响植物的生长，还对沉积物中的铁、磷及重金属的地球化学行为起到了控制性的作用[7-8]。此外，酸挥发性硫化物分析还被越来越多地应用到沉积物重金属的生物毒性评价中[9-10]。因为S2-能够与绝大多数重金属离子相结合，形成不易被生物利用的难溶性硫化物，从而降低了沉积物中重金属的化学活性和生物有效性，对于控制沉积物重金属生物毒性和生态风险能起到关键作用[11]。
为研究不同形态还原性无机硫的环境行为和生物有效性，沉积物中硫形态的提取和分析方法也在不断地发展和完善。Nriagu等[12]在1985年提出的硫形态连续提取原理为后期研究硫形态奠定了基础。目前，硫形态的提取过程主要采用热蒸馏装置和冷扩散装置[9, 13-14]。热蒸馏装置方法为：将沉积物样品加热至混合试剂的沸点与盐酸反应，通过氮气将生成的硫化氢气体(H2S)吹脱至吸收液中。而冷扩散装置法是在热蒸馏法基础上简化的一种提取方法，主要是将装有吸收液的瓶子放入密闭的反应装置中，通过装置中气体浓度差异将生成的硫化氢气体不断地扩散至吸收液中完全吸收[15]。冷扩散法与热蒸馏法相比，虽然装置较为简单，但单一样品的反应一般需要24h，而热蒸馏法提取单个形态时间一般只需1.5h，能极大地提高提取效率。在硫形态提取过程中生成的硫化氢气体一般采用乙酸锌溶液吸收，使用亚甲基蓝法(比色法)[16]、碘量法等方法检测[17]。但这些方法存在测试过程繁琐、分析时间长、硫成分易损失等缺点。随着现代分析仪器的发展和普及，电感耦合等离子体质谱法(ICP-MS)、离子色谱法等因其分析快速、准确率高、检测限低等优势，被越来越多地应用到硫形态检测中[18-22]。
国内外目前对于沉积物中还原性无机硫的提取多采用冷扩散法，但存在难以适应地质、环境研究中样品数量多、样品长时间保存不便等情况。本文研制了一套沉积物中还原性无机硫的快速提取装置及分析方法，即：采用耗时短的热蒸馏法连续提取沉积物中的还原性无机硫，将其转化为硫化氢气体后，经氢氧化钠溶液吸收、加入过氧化氢(H2O2)氧化为$\mathrm{SO}_4^{2-}$后使用离子色谱进行检测。为进一步验证本实验装置的可靠性和实际应用价值，本文还选取了长江三峡库区沉积物样品进行了还原性无机硫的提取分析，研究结果可为三峡库区的水环境治理提供有益的参考。
1. 还原性无机硫提取装置的研制
1.1 装置组成
本实验基于前人沉积物中还原性无机硫的三步提取方法和装置[13, 23]，设计了新的实验装置如图 1所示。装置由五个部分组成，分别为：氮气源(Ⅰ)、加液系统(Ⅱ)、冷凝系统(Ⅲ)、反应系统(Ⅳ)和吸收系统(Ⅴ)，且所有连通部位均以透明硅胶管作为连接器来进行封闭式连通。
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图 1 沉积物还原性无机硫连续提取装置实验装置部件包含：1—氮气瓶；2—减压阀；3—第一气体流量计；4—第二气体流量计；5—层析柱玻璃弯头；6—层析柱；7—层析柱阀门；8—分液漏斗玻璃弯头；9—分液漏斗；10—分液漏斗阀门；11—冷凝管玻璃弯头；12—冷凝管；13—蠕动泵；14—烧杯；15—烧瓶玻璃弯头；16—四口烧瓶(反应器)；17—加热装置；18—试管玻璃弯头；19—玻璃试管。Figure 1. The device for continuous extracting the reduced inorganic sulfur from sedimentsincluding: 1—nitrogen cylinder, 2—pressure reducing valve, 3—the first gas flowmeter, 4—the second gas flowmeter, 5—glass elbow, 6—chromatography column, 7—valve of chromatography column, 8—glass elbow of dispenser funnel, 9—dispenser funnel, 10—valve of dispenser funnel, 11—glass elbow of condenser tube, 12—condenser tube, 13—peristaltic pump, 14—beaker, 15—glass elbow of flask, 16—four-mouth flask (reactor), 17—heating mantle, 18—glass elbow of tube, 19—glass tube.装置五个部分具体连通流程为：首先，将氮气减压阀2、第一气体流量计3、第二气体流量计4连接；然后将层析柱玻璃弯头5和第一气体流量计3、分液漏斗玻璃弯头8连接，将第二气体流量计4、四口烧瓶、层析柱6、分液漏斗9、冷凝管12相连；再次，将冷凝管12下方出口与蠕动泵13左侧接口连接，蠕动泵13右侧接口通过连接管插入烧杯14中，冷凝管12上方出口的连接管置于烧杯14中；最后将冷凝管玻璃弯头11与玻璃试管弯头18相连。
1.2 实验原理与装置性能特点
本实验采用热蒸馏法连续提取沉积物中的还原性无机硫，将其转化为硫化氢气体，经氢氧化钠溶液吸收，用过氧化氢氧化为$\mathrm{SO}_4^{2-}$后通过离子色谱检测。所设计的提取装置密封性好、操作简单，可实现不同形态还原性无机硫的连续提取，分析检测便捷。装置通过试管玻璃弯头与玻璃试管连接，易于取出更换，可提高更换样品的速度，适用于样品数量较多的地质、环境调查分析。
2. 实验部分
2.1 实验样品采集及特征
长江三峡库区沉积物样品为2017年8月和2017年12月采集的三峡库区云阳至秭归段8个长江干流点位样品(云阳上、云阳下、故陵镇、曲尺乡、巫山县、绿竹筏村、屈原镇、秭归)，共16件。采样使用船载采样器采集水界面下表层5cm深的沉积物，样品用聚乙烯自封袋盛装，低温冷藏保存。返回实验室后，将沉积物样品真空冷冻干燥后(-4℃)，于4℃低温密封保存，并及时进行还原性无机硫的提取分析。
2.2 测试仪器
实验过程中，水溶液的离子测试分析在河海大学地球科学与工程学院使用ThermoFisher Scientific公司Aquion型离子色谱仪进行，仪器流量准确度优于0.1%，流量精确度为±0.1%，检测器分辨率为0.00238nS/cm，测试误差 < 5%。
2.3 实验方法
提取沉积物中的还原性无机硫的具体实验流程如图 2所示。为实现连续提取酸挥发性硫、黄铁矿硫、元素硫目的，本装置设计了预先制备提取黄铁矿硫、元素硫所需的二氯化铬溶液(CrCl2)的实验步骤。
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图 2 连续提取沉积物中还原性无机硫流程图Figure 2. Schematic diagram of continuously extracting the reduced inorganic sulfur from sediments.2.3.1 二氯化铬溶液制备及实验准备
关闭图 1所示的分液漏斗阀门10，在分液漏斗9中加入6mol/L盐酸30mL。因为提取还原性无机硫使用的盐酸需经过氮气吹脱，所以在此预先设置了和制备二氯化铬溶液一起使用氮气吹脱盐酸的过程。
以1mol/L稀盐酸为溶剂配制1mol/L三氯化铬溶液(CrCl3)。关闭层析柱阀门7，将120g锌粒和配制好的40mL三氯化铬溶液加入层析柱6中。依次打开图 1所示的氮气瓶1、减压阀2、第一气体流量计3、第二气体流量计4，调节氮气流速以20mL/min的速率对反应装置和盐酸通氮气20min，使氮气通过整个装置，检查装置密闭性；在还原环境、酸性条件下通过金属锌将三氯化铬溶液还原得到二氯化铬溶液，该过程包括两个反应方程式：
$$ \mathrm{Zn}(\mathrm{s})+2 \mathrm{HCl}(\mathrm{aq})=\mathrm{ZnCl}_2(\mathrm{aq})+\mathrm{H}_2(\mathrm{~g}) $$ (1) $$ 2 \mathrm{CrCl}_3(\mathrm{aq})+\mathrm{Zn}(\mathrm{s})=2 \mathrm{CrCl}_2(\mathrm{aq})+\mathrm{ZnCl}_2(\mathrm{aq}) $$ (2) 当层析柱6中溶液颜色由绿色变成亮蓝色时，二氯化铬溶液即制备完成。打开蠕动泵13，保持冷凝管12持续工作。至此，硫形态提取实验准备工作结束。
2.3.2 还原性无机硫形态的提取及测定
(1) 酸挥发性硫(AVS)
酸挥发性硫主要是二价金属(Cu、Ni、Pb、Zn等)硫化物。加入盐酸后，金属硫化物会与其反应生成硫化氢气体，如CuS+2HCl=H2S+CuCl2。硫化氢气体进入氢氧化钠溶液后会发生以下反应：2NaOH+H2S=Na2S+2H2O。而后加入双氧水，可以将-2价的硫氧化为+6价：Na2S+4H2O2=Na2SO4+4H2O。最后通过离子色谱测定溶液中$\mathrm{SO}_4^{2-}$浓度换算得到酸挥发性硫的含量。具体提取步骤如下。
取1.00g沉积物样品加入四口烧瓶16中，加入图 1所示的磁子和0.1mol/L抗坏血酸1mL，往玻璃试管19中加入10mL浓度为50mmol/L氢氧化钠吸收液，调节氮气速率为20mL/min，除去反应系统和吸收系统中的空气后打开分液漏斗阀门10，根据分液漏斗的刻度标识加入10mL盐酸到四口烧瓶16中。打开数显搅拌电热套17，加热至90℃，调节氮气速率以约5~10mL/min的流速将生成的硫化氢气体缓慢吹脱至玻璃试管19中，反应90min。然后调节氮气流速至20mL/min继续吹脱20min，下一步取出装有溶液的玻璃试管19，加入0.1mL过氧化氢(浓度为30%)摇匀静置10min后待检测。同时快速放入另一个含有10mL氢氧化钠溶液(50mmol/L)的玻璃试管为下一步提取黄铁矿硫作准备，连接好玻璃弯头18后通氮气30s。
(2) 黄铁矿硫(铬还原性硫, CRS)
黄铁矿硫主要化学成分为二硫化亚铁(FeS2)，在酸性条件下通过Cr2+将二硫化亚铁转化为硫化氢气体，反应原理为：4H++2Cr2++FeS2→2H2S+2Cr3++Fe2+。产生的硫化氢气体进入氢氧化钠溶液后加入双氧水，将-2价的硫氧化为+6价$\mathrm{SO}_4^{2-}$。通过离子色谱测定$\mathrm{SO}_4^{2-}$浓度并换算得到黄铁矿硫的含量。具体提取步骤如下。
在提取酸挥发性硫步骤完成后，打开图 1所示的层析柱阀门7，根据层析柱刻度指示加入20mL二氯化铬溶液(在2.3.1节中已加入层析柱中)，打开分液漏斗阀门10，根据分液漏斗的刻度标识加入10mL盐酸到四口烧瓶16中，打开数显搅拌电热套17，加热至90℃，以5~10mL/min的氮气流速将生成的硫化氢气体缓慢吹脱至玻璃试管19中，反应90min后调节氮气流速至20mL/min继续吹脱20min。然后取出装有氢氧化钠溶液的玻璃试管19，加入0.1mL过氧化氢(浓度为30%)摇匀静置10min；同时快速放入另一个含有10mL氢氧化钠溶液(50mmol/L)的玻璃试管为下一步提取元素硫作准备，连接好玻璃弯头18后通氮气30s。
(3) 元素硫(ES)
元素硫主要是中间态的零价硫，难溶于水，但与有机溶剂结合能力较强，因此加入DMF(N, N-二甲基甲酰胺)萃取。在酸性条件下通过Cr2+将零价硫转化为硫化氢气体，反应原理为：2H++2Cr2++S0→H2S+2Cr3+。产生的硫化氢气体进入氢氧化钠溶液后加入过氧化氢，将-2价的硫氧化为+6价$\mathrm{SO}_4^{2-}$，再通过离子色谱测定$\mathrm{SO}_4^{2-}$浓度，从而换算得到元素硫的含量。具体提取步骤如下。
在提取黄铁矿硫步骤完成后，通过图 1所示的玻璃弯头15往反应器16中加入20mL二甲基甲酰胺，由于其对塑料有溶解作用，所以不能从三通阀处直接注入，连接好装置后通氮气30s；打开层析柱阀门7和分液漏斗阀门10，分别从层析柱、分液漏斗加入20mL二氯化铬溶液和6mol/L盐酸10mL，打开数显搅拌电热套17，加热至90℃，以5~10mL/min的氮气流速将生成的硫化氢气体缓慢吹脱至玻璃试管19中，反应90min后调节氮气流速至20mL/min继续吹脱20min。取出装有氢氧化钠溶液的玻璃试管19，加入0.1mL过氧化氢(浓度为30%)，摇匀静置10min后溶液待检测。
3. 实验方法的精密度和准确度
为对本研究改进的热蒸馏法提取还原性无机硫实验方法的准确度和精密度进行验证，进一步开展了重复性和加标对比实验(表 1)。选取沉积物样品(三峡秭归，冬季)开展重复性实验3次(n=3)，得到酸挥发性硫、黄铁矿硫、元素硫的平均值分别为0.19、3.10、0.37μmol/g，实验结果的相对标准偏差(RSD)分别为5.26%、1.22%和3.09%，重复性较优。进一步分别用1mmol/L九水硫化钠(Na2S·9H2O)、黄铁矿(GBW07267)、高纯硫对酸挥发性硫、黄铁矿硫、元素硫的回收率进行测定，实验结果显示这三种硫形态的回收率分别为92.8%、93.6%、94.1%，实验结果的相对标准偏差(RSD)分别为1.14%、2.14%和0.46%，加标回收率较理想。
表 1 重复实验与加标实验结果Table 1. Results of repeated experiment and spike recovery in AVS, CRS, and ES procedures.硫形态 重复实验 加标实验(回收率) 第一次实验(μmol/g) 第二次实验(μmol/g) 第三次实验(μmol/g) 平均值(μmol/g) RSD(%) 第一次实验(%) 第二次实验(%) 第三次实验(%) 平均值(%) RSD(%) 酸挥发性硫(AVS) 0.20 0.19 0.18 0.19 5.26 91.6 93.2 93.6 92.8 1.14 黄铁矿硫(CRS) 3.13 3.06 3.12 3.10 1.22 93.4 95.7 91.7 93.6 2.14 元素硫(ES) 0.38 0.38 0.36 0.37 3.09 94.6 93.8 93.9 94.1 0.46 李肖等[24]采用改进的“冷扩散法”测定沉积物中还原态无机硫含量，实验过程中通过90℃水浴加热将“冷扩散法”提取酸挥发性硫、黄铁矿硫和元素硫的提取反应时间分别缩短为1.5h、2h和2h；其在实验中加入固体硫化锌(ZnS)进行酸挥发性硫的回收实验，回收率为82.01%~108.71%。王小芳等[25]与李肖等[24]采用相同提取方法通过配制标准溶液作为提取剂的方式进行沉积物元素硫的回收实验，回收率为92.25%~98.08%(n=3)。通过以上其他实验对比可以看出，本研究实验的加标回收率相对较优。本文的热蒸馏法沉积物还原性无机硫提取装置和实验方法的分析准确度较高，精密度也较好。
4. 讨论
4.1 实验的操作效率分析
多数沉积物样品赋存于缺氧的沉积环境中，这些新鲜的沉积物样品必须及时处理，减少硫化物再氧化的风险[15]，快速、准确也是相关行业对大批量样品硫含量分析测试的基本要求[22]。本实验所采用的热蒸馏法相比冷扩散法能较大地缩短实验时间。由于冷扩散法装置简单、易操作，传统的硫形态多采用冷扩散法提取[23]、亚甲基蓝法[16, 26]或碘量法[17]检测，其中酸挥发性硫、元素硫的提取需要18~24h，黄铁矿硫则需48h，反应时间较长[27-28]。而本实验系统采用的热蒸馏法对单个形态提取为1.5h，完成3种形态的提取时间大约需要4.5h时，时间大大缩短，已有研究表明加热可有效地缩短硫形态的提取时间[29]。
所设计的试验装置操作简便，装置采用试管玻璃弯头与玻璃试管连接，易于取出更换，可实现沉积物中各形态还原性无机硫的连续提取，能有效地提高热蒸馏法的实验效率。同时，根据研究者自身需要，还可以增加提取组数，通过多通器件与氮气瓶连接，进一步实现多组样品的同时处理。过氧化氢可以短时间将硫化氢氧化成硫酸盐[12]。本实验方法选取过氧化氢作为氧化剂，将各形态实验提取出的硫化氢采用氢氧化钠溶液吸收后氧化为$\mathrm{SO}_4^{2-}$，再通过离子色谱测定$\mathrm{SO}_4^{2-}$浓度，并换算得到各形态硫的含量。由于过氧化氢在常温下是液态，可以直接将硫化氢的输送管插入含有过氧化氢的溶液内。采用过氧化氢不仅可以快速地氧化硫化氢，其产物$\mathrm{SO}_4^{2-}$还可以实现使用离子色谱进行检测，检测方法简单可靠，仪器检测的准确度高。
4.2 三峡库区沉积物测试分析
4.2.1 三峡库区沉积物还原性无机硫特征
采用本研究的实验装置和方法进行了三峡库区表层沉积物样品还原性无机硫的测定。实验所用样品为2017年8月和12月分别于三峡库区云阳至秭归段8个长江干流点位采集的沉积物(图 3)，三峡库区表层沉积物中还原性无机硫的平均含量及组成情况见表 2。
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表 2 三峡沉积物与太湖表层沉积物还原性无机硫的含量Table 2. Composition of AVS, CRS, and ES in sediments of the Three Gorges Reservoir area and Taihu Lake.表 2结果显示测得三峡沉积物样品的酸挥发性硫、元素硫和黄铁矿硫的平均含量分别为0.22、0.50和4.37μmol/g。尹洪斌等[30]采用改进的冷扩散法测试了长江下游太湖北部沉积物还原性无机硫的含量，其样品采集于富营养化污染较为严重的太湖梅梁湾北部与西五里湖。进一步分析可知，本研究的三峡库区沉积物酸挥发性硫、黄铁矿硫和元素硫的平均含量均略低于太湖北部研究结果(表 2，图 3)。三峡库区的酸挥发性硫含量相对较低，未达到污染的程度，有学者指出未受污染的湖泊沉积物中酸挥发性硫含量范围为4~13μmol/g[31]。由于太湖是富营养化型湖泊，有机质含量较高，加快了硫酸盐的还原过程，在极端厌氧的水环境中酸挥发性硫很难与沉积物中的元素硫发生氧化反应，从而导致了积累[32]。
4.2.2 三峡库区还原性无机硫的季节性变化
三峡库区夏季与冬季表层沉积物中还原性无机硫(RIS)组成均以黄铁矿硫为主，占68%~93%(图 4)。三峡库区干流沉积物中RIS含量呈现明显的季节性变化。总体上，三峡库区表层沉积物中RIS各组分含量从高到低为：黄铁矿硫 > 元素硫 > 酸挥发性硫。夏季酸挥发性硫平均含量为0.32μmol/g，冬季为0.13μmol/g，冬季酸挥发性硫含量只有夏季的41%左右，表现为夏季高于冬季，这与其他地区的研究结果较为类似[31, 33]。三峡库区沉积物酸挥发性硫在季节和空间分布上表现出了较大差异(图 4)，这可能是因为酸挥发性硫对环境变化更敏感[34]。
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图 4 三峡库区沉积物还原性无机硫形态季节性组成特征a酸挥发性硫，b元素硫，c黄铁矿硫Figure 4. Spatial and seasonal distribution characteristics of RIS in surface sediments of the Three Gorges Reservoir area(a) acid volatile sulfur, (b) elemental sulfur, (c) pyrite sulfur5. 结论
本文基于热蒸馏法，设计了一套连续提取沉积物还原性无机硫的装置和实验方法，该方法相比冷扩散法可较大地缩短单个还原性无机硫形态的提取时间；装置通过优化，设计了预先制备实验所需的二氯化铬溶液的步骤，实现了样品还原性无机硫形态的连续提取；并以过氧化氢为氧化剂，将提取的各形态硫氧化为$\mathrm{SO}_4^{2-}$后采用离子色谱进行检测，操作简便、准确度高。同时，还应用本实验方法对长江三峡库区沉积物样品开展了还原性无机硫的分析研究，显示三峡库区硫污染程度相对较低。
本研究所设计的装置和方法解决了地质、环境调查研究中大批量样品需要快速、准确分析的问题，适合在相关行业推广应用。如何进一步通过装置和方法的优化，减少氮气吹脱量和提取反应的时间，则需要进一步开展实验研究。
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图 1 沉积物还原性无机硫连续提取装置
实验装置部件包含：1—氮气瓶；2—减压阀；3—第一气体流量计；4—第二气体流量计；5—层析柱玻璃弯头；6—层析柱；7—层析柱阀门；8—分液漏斗玻璃弯头；9—分液漏斗；10—分液漏斗阀门；11—冷凝管玻璃弯头；12—冷凝管；13—蠕动泵；14—烧杯；15—烧瓶玻璃弯头；16—四口烧瓶(反应器)；17—加热装置；18—试管玻璃弯头；19—玻璃试管。
Figure 1. The device for continuous extracting the reduced inorganic sulfur from sediments
including: 1—nitrogen cylinder, 2—pressure reducing valve, 3—the first gas flowmeter, 4—the second gas flowmeter, 5—glass elbow, 6—chromatography column, 7—valve of chromatography column, 8—glass elbow of dispenser funnel, 9—dispenser funnel, 10—valve of dispenser funnel, 11—glass elbow of condenser tube, 12—condenser tube, 13—peristaltic pump, 14—beaker, 15—glass elbow of flask, 16—four-mouth flask (reactor), 17—heating mantle, 18—glass elbow of tube, 19—glass tube.
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图 2 连续提取沉积物中还原性无机硫流程图
Figure 2. Schematic diagram of continuously extracting the reduced inorganic sulfur from sediments.
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图 4 三峡库区沉积物还原性无机硫形态季节性组成特征
a酸挥发性硫，b元素硫，c黄铁矿硫
Figure 4. Spatial and seasonal distribution characteristics of RIS in surface sediments of the Three Gorges Reservoir area
(a) acid volatile sulfur, (b) elemental sulfur, (c) pyrite sulfur
表 1 重复实验与加标实验结果
Table 1 Results of repeated experiment and spike recovery in AVS, CRS, and ES procedures.
硫形态 重复实验 加标实验(回收率) 第一次实验(μmol/g) 第二次实验(μmol/g) 第三次实验(μmol/g) 平均值(μmol/g) RSD(%) 第一次实验(%) 第二次实验(%) 第三次实验(%) 平均值(%) RSD(%) 酸挥发性硫(AVS) 0.20 0.19 0.18 0.19 5.26 91.6 93.2 93.6 92.8 1.14 黄铁矿硫(CRS) 3.13 3.06 3.12 3.10 1.22 93.4 95.7 91.7 93.6 2.14 元素硫(ES) 0.38 0.38 0.36 0.37 3.09 94.6 93.8 93.9 94.1 0.46 
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[1] Wang J, Chen J, Guo J, et al. Speciation and transfor-mation of sulfur in freshwater sediments: A case study in southwest China[J]. Water Air Soil Pollut, 2017, 228(10): 392. doi: 10.1007/s11270-017-3580-5
[2] 毛立, 孙志高, 陈冰冰, 等. 闽江河口互花米草入侵湿地土壤无机硫赋存形态及其影响因素[J]. 生态学报, 2021, 41(12): 4840-4852. https://www.cnki.com.cn/Article/CJFDTOTAL-STXB202112018.htm Mao L, Sun Z G, Chen B B, et al. Variations of inorganic sulfur fractions and main influencing factors in marsh soils with different years of spartina alterniflora invasion in the Min River Estuary[J]. Acta Ecologica Sinica, 2021, 41(12): 4840-4852. https://www.cnki.com.cn/Article/CJFDTOTAL-STXB202112018.htm
[3] Lu Q Q, Bai J H, Yan D H, et al. Sulfur forms in wetland soils with different flooding periods before and after flow-sediment regulation in the Yellow River Delta, China[J]. Journal of Cleaner Production, 2020, 276(8): 122969.
[4] 陈伟锐. 高频红外碳硫仪测定土壤和水系沉积物中的硫实验条件改进[J]. 岩矿测试, 2019, 38(1): 123-128. doi: 10.15898/j.cnki.11-2131/td.201804160045 Chen W R. Improvement of experimental conditions for the determination of sulfur in soil and stream sediments by high frequency infrared carbon and sulfur analyzer[J]. Rock and Mineral Analysis, 2019, 38(1): 123-128. doi: 10.15898/j.cnki.11-2131/td.201804160045
[5] Jiang M, Sheng Y Q, Liu Q Q, et al. Conversion mecha-nisms between organic sulfur and inorganic sulfur in surface sediments in coastal rivers[J]. Science of the Total Environment, 2021, 752: 141829. doi: 10.1016/j.scitotenv.2020.141829
[6] 陈冰冰, 孙志高, 孙文广, 等. 外源氮输入对生长季黄河口碱蓬湿地土壤无机硫形态变化特征的影响[J]. 水土保持学报, 2018, 32(5): 277-286. doi: 10.13870/j.cnki.stbcxb.2018.05.044 Chen B B, Sun Z G, Sun W G, et al. Effects of exogenous nitrogen enrichment on variations of inorganic sulfur fractions in soils of suaeda salsa marsh in the Yellow River Estuary during the growing season[J]. Journal of Soil and Water Conservation, 2018, 32(5): 277-286. doi: 10.13870/j.cnki.stbcxb.2018.05.044
[7] Huerta-Diaz M A, Tessier A, Carignan R. Geochemistry of trace metals associated with reduced sulfur in freshwater sediments[J]. Applied Geochemistry, 1998, 13(2): 213-233. doi: 10.1016/S0883-2927(97)00060-7
[8] 刘崴, 胡俊栋, 杨红霞, 等. 电感耦合等离子体质谱联用技术在元素形态分析中的应用进展[J]. 岩矿测试, 2021, 40(3): 327-339. doi: 10.15898/j.cnki.11-2131/td.202006110089 Liu W, Hu J D, Yang H X, et al. Research progress on elemental speciation analysis by inductively coupled plasma-mass spectrometry hyphenated techniques[J]. Rock and Mineral Analysis, 2021, 40(3): 327-339. doi: 10.15898/j.cnki.11-2131/td.202006110089
[9] 李力, 王小静, 刘季花. 沉积物中酸可挥发性硫化物的分析方法研究[J]. 海洋与湖沼, 2015, 46(1): 96-101. https://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ201501012.htm Li L, Wang X J, Liu J H. Analytical method of acid volatile sulfide in sediment[J]. Oceanologia et Limnologia Sinica, 2015, 46(1): 96-101. https://www.cnki.com.cn/Article/CJFDTOTAL-HYFZ201501012.htm
[10] 徐程, 杨斌, 朱雪菁, 等. 大风江口海域沉积物酸可挥发性硫化物、重金属分布及风险评价[J]. 环境科学研究, 2020, 33(6): 1530-1538. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKX202006026.htm Xu C, Yang B, Zhu X Q, et al. Distribution and risk assessment of acid volatile sulfide and heavy metals in sediments of Dafengjiang River Estuary[J]. Research of Environmental Sciences, 2020, 33(6): 1530-1538. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKX202006026.htm
[11] Souza L R, Knöller K, Ladeira A C Q. Sulfur isotope fractionation and sequential extraction to assess metal contamination on lake and river sediments[J]. Journal of Soils and Sediments, 2016, 16: 1986-1994. doi: 10.1007/s11368-016-1410-9
[12] Nriagu J O, Soon Y K. Distribution and isotopic com-position of sulfur in lake sediments of northern Ontario[J]. Geochimica et Cosmochimica Acta, 1985, 49(3): 823-834. doi: 10.1016/0016-7037(85)90175-9
[13] Duan W, Coleman M L, Pye K. Determination of reduced sulphur species in sediments—An evaluation and modified technique[J]. Chemical Geology, 1997, 141(3): 185-194.
[14] 曹爱丽, 周桂平, 胡姝, 等. 崇明东滩湿地沉积物中还原无机硫的形态特征[J]. 复旦学报(自然科学版), 2010, 49(5): 612-617. https://www.cnki.com.cn/Article/CJFDTOTAL-FDXB201005013.htm Cao A L, Zhou G P, Hu S, et al. Morphological characteristics of reduced inorganic sulfur in sediments of Dongtan Wetland in Chongming[J]. Journal of Fudan University (Natural Science), 2010, 49(5): 612-617. https://www.cnki.com.cn/Article/CJFDTOTAL-FDXB201005013.htm
[15] Hsieh Y P, Yang C H. Diffusion methods for the deter-mination of reduced inorganic sulfur species in sediments[J]. Limnology & Oceanography, 1989, 34(6): 1126-1130.
[16] Neretin L N, Böttcher M E, Jørgensen B B, et al. Pyriti-zation processes and greigite formation in the advancing sulfidization front in the upper Pleistocene sediments of the Black Sea[J]. Geochimica et Cosmochimica Acta, 2004, 68(9): 2081-2093.
[17] Burton E D, Sullivan L A, Bush R T, et al. A simple and inexpensive chromium-reducible sulfur method for acid-sulfate soils[J]. Applied Geochemistry, 2008, 23(9): 2759-2766.
[18] 黄志丁, 王军, 逯海, 等. 电感耦合等离子体质谱法测定硫时不同形态硫的影响[J]. 岩矿测试, 2012, 31(1): 77-82. http://www.ykcs.ac.cn/cn/article/id/ykcs_20120110 Huang Z D, Wang J, Lu H, et al. The effect on sulfur species during determination of sulfur by inductively coupled plasma-mass spectrometry[J]. Rock and Mineral Analysis, 2012, 31(1): 77-82. http://www.ykcs.ac.cn/cn/article/id/ykcs_20120110
[19] 张媛媛, 林学辉, 贺行良, 等. 离子色谱法同时测定海洋沉积物中氯和硫[J]. 分析科学学报, 2015, 31(2): 249-252. https://www.cnki.com.cn/Article/CJFDTOTAL-FXKX201502021.htm Zhang Y Y, Lin X H, He X L, et al. Determination of chlorine and sulfur in marine sediment by ion chromatography[J]. Journal of Analytical Science, 2015, 31(2): 249-252. https://www.cnki.com.cn/Article/CJFDTOTAL-FXKX201502021.htm
[20] Chen Y Q, Ge J W, Huang T, et al. Restriction of sulfate reduction on the bioavailability and toxicity of trace metals in Antarctic lake sediments[J]. Marine Pollution Bulletin, 2020, 151: 110807.
[21] 石友昌, 陈贵仁, 赵萌生, 等. 酸溶-电感耦合等离子体发射光谱法和燃烧-红外吸收法测定不同类型地球化学样品中的硫[J]. 岩矿测试, 2022, 41(4): 663-672. doi: 10.15898/j.cnki.11-2131/td.202108200104 Shi Y C, Chen G R, Zhao M S, et al. Determination of sulfur in different types of geochemical samples by ICP-OES with acid dissolution and combustion-infrared absorption spectrometry[J]. Rock and Mineral Analysis, 2022, 41(4): 663-672. doi: 10.15898/j.cnki.11-2131/td.202108200104
[22] 姜云军, 李星, 姜海伦, 等. 四酸敞口溶解-电感耦合等离子体发射光谱法测定土壤中的硫[J]. 岩矿测试, 2018, 37(2): 152-158. doi: 10.15898/j.cnki.11-2131/td.201704010048 Jiang Y J, Li X, Jiang H L, et al. Determination of sulfurin soil by inductively coupled plasma-optical emission spectrometry with four acids open dissolution[J]. Rock and Mineral Analysis, 2018, 37(2): 152-158. doi: 10.15898/j.cnki.11-2131/td.201704010048
[23] Hsieh Y P, Shieh Y N. Analysis of reduced inorganic sulfur by diffusion methods: Improved apparatus and evaluation for sulfur isotopic studies[J]. Chemical Geology, 1997, 137(3): 255-261.
[24] 李肖, 赵新如, 周芬琦, 等. 安徽庐江钟山尾矿区河流水体硫形态及硫同位素分布特征[J]. 环境化学, 2021, 40(6): 1787-1794. https://www.cnki.com.cn/Article/CJFDTOTAL-HJHX202106016.htm Li X, Zhao X R, Zhou F Q, et al. Distribution characteristics of sulfur species and isotopes in sediments of rivers around Zhongshan tailing at Lujiang County, Anhui Province[J]. Environmental Chemistry, 2021, 40(6): 1787-1794. https://www.cnki.com.cn/Article/CJFDTOTAL-HJHX202106016.htm
[25] 王小芳, 李方晓, 黄涛, 等. 安徽铜陵铜尾矿硫形态及硫同位素分布特征[J]. 中国环境科学, 2019, 39(4): 1664-1671. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ201904045.htm Wang X F, Li F X, Huang T, et al. Distribution characteristics of sulfur species and isotopes in a copper tailing at Tongling, Anhui Province[J]. China Environ-mental Science, 2019, 39(4): 1664-1671. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ201904045.htm
[26] 程思海, 陈道华, 雷知生. 使用元素分析仪测定海洋沉积物中的硫化物[J]. 岩矿测试, 2011, 30(1): 63-66. http://www.ykcs.ac.cn/cn/article/id/ykcs_20110113 Cheng S H, Chen D H, Lei Z S. Determination of sulfide in marine sediments by elemental analyzer[J]. Rock and Mineral Analysis, 2011, 30(1): 63-66. http://www.ykcs.ac.cn/cn/article/id/ykcs_20110113
[27] Sheng Y Q, Sun Q Y, Shi W J, et al. Geochemistry of reduced inorganic sulfur, reactive iron, and organic carbon in fluvial and marine surface sediment in the Laizhou Bay region, China[J]. Environmental Earth Sciences, 2015, 74(2): 1151-1160.
[28] 吴松峻, 汪旋, 季秋忆, 等. 太湖西岸典型区域沉积物的硫铁分布特征及环境意义[J]. 湖泊科学, 2019, 31(4): 950-960. https://www.cnki.com.cn/Article/CJFDTOTAL-FLKX201904006.htm Luo S J, Wang X, Ji Q Y, et al. Iron-sulfur distribution and its environmental significance in three typical areas of western Lake Taihu[J]. Journal of Lake Sciences, 2019, 31(4): 950-960. https://www.cnki.com.cn/Article/CJFDTOTAL-FLKX201904006.htm
[29] Chen Y Q, Shen L L, Huang T, et al. Transformation of sulfur species in lake sediments at Ardley Island and Fildes Peninsula, King George Island, Antarctic Peninsula[J]. Science of tThe Total Environment, 2020, 703: 135591.
[30] 尹洪斌, 范成新, 丁士明, 等. 太湖沉积物中无机硫的化学特性[J]. 中国环境科学, 2008, 28(2): 183-187. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ200802019.htm Yin H B, Fan C X, Ding S M, et al. The chemical characteristics of inorganic sulfur in Taihu Lake sediments[J]. China Environmental Science, 2008, 28(2): 183-187. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ200802019.htm
[31] Leonard E N, Mattson V R, Benoit D A, et al. Seasonal variation of acid volatile sulfide concentration in sediment cores from three northeastern Minnesota Lakes[J]. Hydrobiologia, 1993, 271(2): 87-95.
[32] 朱瑾灿, 吴雨琛, 尹洪斌. 太湖蓝藻聚集区沉积物硫形态的时空变异特征[J]. 中国环境科学, 2017, 37(12): 4690-4700. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ201712040.htm Zhu J C, Wu Y C, Yin H B. Spatial and temporal variation of sulfur speciation in sediments from cyanobacteria accumulation in Taihu Lake, China[J]. China Environmental Science, 2017, 37(12): 4690-4700. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGHJ201712040.htm
[33] Howard D E, Evans R D. Acid-volatile sulfide (AVS) in a seasonally anoxic mesotrophic lake: Seasonal and spatial changes in sediment AVS[J]. Environmental Toxicology and Chemistry: An International Journal, 1993, 12(6): 1051-1057.
[34] Oehm N J, Luben T J, Ostrofsky M L. Spatial distribution of acid-volatile sulfur in the sediments of Canadohta Lake, PA[J]. Hydrobiologia, 1997, 345(1): 79-85.
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1. 唐珂，左嘉. 连续提取沉积物中硫的形态分析方法. 科学技术创新. 2024(24): 83-86 . 
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