The present study investigated quantitatively the significance of HNLC (high-nutrient low-chlorophyll) regions and its grazing control with the improved iron fertilization for climate change. The limitation of iron (F...The present study investigated quantitatively the significance of HNLC (high-nutrient low-chlorophyll) regions and its grazing control with the improved iron fertilization for climate change. The limitation of iron (Fe) for phytoplankton growth in HNLC regions was confirmed by sulfur compounds (S) such as volcanic ash and hydrogen sulfide (H2S) in batch cultures, whose chemical sediment of Fe3S4 showed 4.06 wt%. The technologies developed for iron fertilization since 1993 till now were not practical to provide sufficient amounts of bioavailable iron due to sedimentary iron sulfides induced by undersea volcanic sulfur compounds. The proposed technology for iron fertilization was improved to enhance the bioavailable iron to phytoplankton by keeping minimal sulfur compounds in HNLC regions. The low productivity of phytoplankton by grazing control in HNLC regions was 6% diatoms whose 52% was grazed by copepods and 42% by krill on the basis of data analysis in 2000 EisenEx Experiment at boundary of Antarctic and African tectonic plates. All of the previous iron fertilization experiments were conducted at volcanic sulfur compounds enriched HNLC regions. The present study revealed that the enhanced phytoplankton productivity in batch culture without sedimentary iron sulfides can be possible only if sulfur compounds are minimal, as is in Shag Rocks (53°S, 42°W) of South Georgia in Scotia Sea in the Southern Ocean.展开更多
“High nutrient, low chlorophyll (HNLC)” regions were created by locking iron into sedimentary iron sulfides with hydrogen sulfide available from volcanic eruptions in surrounding oceans. Appropriate locations and de...“High nutrient, low chlorophyll (HNLC)” regions were created by locking iron into sedimentary iron sulfides with hydrogen sulfide available from volcanic eruptions in surrounding oceans. Appropriate locations and deployment methods for the iron fertilization were far from volcanoes, earthquakes and boundaries of tectonic plates to reduce the chance of iron-locking by volcanic sulfur compounds. The appropriate locations for the large-scale iron fertilization are proposed as Shag Rocks in South Georgia and the Bransfield Strait in Drake Passage in the Southern Ocean due to their high momentum flux causing efficient iron deployment. The iron (Fe) replete compounds, consisting of natural clay, volcanic ash, agar, N</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">-fixing mucilaginous cyanobacteria, carbon black, biodegradable plastic foamed polylactic acid, fine wood chip, and iron-reducing marine bacterium, are deployed in the ocean to stay within a surface depth of 100</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-size:12px;font-family:Verdana;"><span style="font-size:12px;font-family:Verdana;"><span style="font-family:Verdana;font-size:12px;">m for phytoplankton digestion. The deployment method of Fe-replete composite with a duration of at least several years for the successful iron fertilization, is configured to be on the streamline of the Antarctic Circumpolar Current (ACC). This will result in high momentum flux for its efficient dispersion on the ocean surface where diatom, copepods, krill and humpback whale stay together (~100</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-size:12px;font-family:Verdana;">m). Humpback whales are proposed as a biomarker for the successful iron fertilization in large-scale since humpback whales feed on krill, which in turn feed on cockpods and diatoms. The successful large-scale iron fertilization may be indicated by the return of the humpback whales if they could not be found for a long period before the iron fertilization. On-line monitoring for the successful iron fertilization focuses on the simultaneous changes of the following two groups;the increase concentration group (chlorophyll, O</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">, Dissolved Oxygen (DO), Di Methyl Sulfide (DMS)) and the decrease concentration group (nitrate, phosphate, silicate, CO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">, Dissolved CO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;"> (DCO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">)). The monitoring of chlorophyll-</span><i><span style="font-size:12px;font-family:Verdana;">a</span></i><span style="font-size:12px;font-family:Verdana;">, nitrate phosphate, and silicate concentrations after deploying the Fe-replete complex is carried out throughout the day and night for the accurate measurement of algal blooms.展开更多
为客观掌握原油加工中硫腐蚀产物(主要指硫铁化合物)氧化自燃的研究进展,对中国知网(CNKI)和Web Of ScienceTM(WOS)核心合集数据库中2006—2016年间国内外硫腐蚀产物氧化自燃的相关研究文献进行高级检索,利用文献计量学方法对国内该领...为客观掌握原油加工中硫腐蚀产物(主要指硫铁化合物)氧化自燃的研究进展,对中国知网(CNKI)和Web Of ScienceTM(WOS)核心合集数据库中2006—2016年间国内外硫腐蚀产物氧化自燃的相关研究文献进行高级检索,利用文献计量学方法对国内该领域相关研究文献的发表年度、学科分布、作者分布、研究机构、基金项目资助等方面进行统计与分析,并采用CitespaceIII软件对硫腐蚀产物氧化自燃相关研究文献的关键词进行分析。结果表明:2006—2016年间国内该领域相关研究文献的发表数量总体呈上升态势;该领域呈现多学科相互交叉的发展趋势,其中石油、天然气工业是发文量最多的学科;文献作者蒋军城、赵声萍、赵彬林、张振华、李萍在该领域的研究成果较多;辽宁石油化工大学、南京工业大学、东北大学是该领域研究比较活跃的机构;该领域研究的基金项目资助主要来自国家自然科学基金;该领域的研究热点主要围绕"硫化亚铁"、"硫铁化合物"、"自燃性"、"硫化氢"、"活化能"、"化学清洗"等关键词展开;指出该领域国际上文献发表数量较少的可能原因。最后评述了硫腐蚀产物氧化自燃研究现状和存在的主要问题,并对未来研究趋势进行了展望。展开更多
硫铁化合物氧化放热是引发煤炭自燃的原因之一,运用XRD、TG-DSC技术分析硫铁化合物的热分解过程和非等温热分解机理。研究表明,硫铁化合物分解包括3个阶段:在179.1~287.75℃内逐步进行物相转化,403.5~493.75℃内开始FeS_2的氧化热解,611...硫铁化合物氧化放热是引发煤炭自燃的原因之一,运用XRD、TG-DSC技术分析硫铁化合物的热分解过程和非等温热分解机理。研究表明,硫铁化合物分解包括3个阶段:在179.1~287.75℃内逐步进行物相转化,403.5~493.75℃内开始FeS_2的氧化热解,611.65~792.25℃内发生硫酸盐(或亚硫酸盐)逐步分解,热解失重达到最大值。运用Friedma法、Kissinger法、Starink法对非等温动力学数据进行分析,3个阶段的表观活化能分别是96,174,230 k J/mol。各阶段样品稳定性逐渐提高,为硫铁化合物自燃的综合判据提供依据。展开更多
文摘The present study investigated quantitatively the significance of HNLC (high-nutrient low-chlorophyll) regions and its grazing control with the improved iron fertilization for climate change. The limitation of iron (Fe) for phytoplankton growth in HNLC regions was confirmed by sulfur compounds (S) such as volcanic ash and hydrogen sulfide (H2S) in batch cultures, whose chemical sediment of Fe3S4 showed 4.06 wt%. The technologies developed for iron fertilization since 1993 till now were not practical to provide sufficient amounts of bioavailable iron due to sedimentary iron sulfides induced by undersea volcanic sulfur compounds. The proposed technology for iron fertilization was improved to enhance the bioavailable iron to phytoplankton by keeping minimal sulfur compounds in HNLC regions. The low productivity of phytoplankton by grazing control in HNLC regions was 6% diatoms whose 52% was grazed by copepods and 42% by krill on the basis of data analysis in 2000 EisenEx Experiment at boundary of Antarctic and African tectonic plates. All of the previous iron fertilization experiments were conducted at volcanic sulfur compounds enriched HNLC regions. The present study revealed that the enhanced phytoplankton productivity in batch culture without sedimentary iron sulfides can be possible only if sulfur compounds are minimal, as is in Shag Rocks (53°S, 42°W) of South Georgia in Scotia Sea in the Southern Ocean.
文摘“High nutrient, low chlorophyll (HNLC)” regions were created by locking iron into sedimentary iron sulfides with hydrogen sulfide available from volcanic eruptions in surrounding oceans. Appropriate locations and deployment methods for the iron fertilization were far from volcanoes, earthquakes and boundaries of tectonic plates to reduce the chance of iron-locking by volcanic sulfur compounds. The appropriate locations for the large-scale iron fertilization are proposed as Shag Rocks in South Georgia and the Bransfield Strait in Drake Passage in the Southern Ocean due to their high momentum flux causing efficient iron deployment. The iron (Fe) replete compounds, consisting of natural clay, volcanic ash, agar, N</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">-fixing mucilaginous cyanobacteria, carbon black, biodegradable plastic foamed polylactic acid, fine wood chip, and iron-reducing marine bacterium, are deployed in the ocean to stay within a surface depth of 100</span></span></span><span><span><span style="font-family:""> </span></span></span><span style="font-size:12px;font-family:Verdana;"><span style="font-size:12px;font-family:Verdana;"><span style="font-family:Verdana;font-size:12px;">m for phytoplankton digestion. The deployment method of Fe-replete composite with a duration of at least several years for the successful iron fertilization, is configured to be on the streamline of the Antarctic Circumpolar Current (ACC). This will result in high momentum flux for its efficient dispersion on the ocean surface where diatom, copepods, krill and humpback whale stay together (~100</span></span></span><span><span><span style="font-family:""> </span></span></span><span><span><span style="font-family:""><span style="font-size:12px;font-family:Verdana;">m). Humpback whales are proposed as a biomarker for the successful iron fertilization in large-scale since humpback whales feed on krill, which in turn feed on cockpods and diatoms. The successful large-scale iron fertilization may be indicated by the return of the humpback whales if they could not be found for a long period before the iron fertilization. On-line monitoring for the successful iron fertilization focuses on the simultaneous changes of the following two groups;the increase concentration group (chlorophyll, O</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">, Dissolved Oxygen (DO), Di Methyl Sulfide (DMS)) and the decrease concentration group (nitrate, phosphate, silicate, CO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">, Dissolved CO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;"> (DCO</span><sub><span style="font-size:12px;font-family:Verdana;">2</span></sub><span style="font-size:12px;font-family:Verdana;">)). The monitoring of chlorophyll-</span><i><span style="font-size:12px;font-family:Verdana;">a</span></i><span style="font-size:12px;font-family:Verdana;">, nitrate phosphate, and silicate concentrations after deploying the Fe-replete complex is carried out throughout the day and night for the accurate measurement of algal blooms.
文摘为客观掌握原油加工中硫腐蚀产物(主要指硫铁化合物)氧化自燃的研究进展,对中国知网(CNKI)和Web Of ScienceTM(WOS)核心合集数据库中2006—2016年间国内外硫腐蚀产物氧化自燃的相关研究文献进行高级检索,利用文献计量学方法对国内该领域相关研究文献的发表年度、学科分布、作者分布、研究机构、基金项目资助等方面进行统计与分析,并采用CitespaceIII软件对硫腐蚀产物氧化自燃相关研究文献的关键词进行分析。结果表明:2006—2016年间国内该领域相关研究文献的发表数量总体呈上升态势;该领域呈现多学科相互交叉的发展趋势,其中石油、天然气工业是发文量最多的学科;文献作者蒋军城、赵声萍、赵彬林、张振华、李萍在该领域的研究成果较多;辽宁石油化工大学、南京工业大学、东北大学是该领域研究比较活跃的机构;该领域研究的基金项目资助主要来自国家自然科学基金;该领域的研究热点主要围绕"硫化亚铁"、"硫铁化合物"、"自燃性"、"硫化氢"、"活化能"、"化学清洗"等关键词展开;指出该领域国际上文献发表数量较少的可能原因。最后评述了硫腐蚀产物氧化自燃研究现状和存在的主要问题,并对未来研究趋势进行了展望。
文摘硫铁化合物氧化放热是引发煤炭自燃的原因之一,运用XRD、TG-DSC技术分析硫铁化合物的热分解过程和非等温热分解机理。研究表明,硫铁化合物分解包括3个阶段:在179.1~287.75℃内逐步进行物相转化,403.5~493.75℃内开始FeS_2的氧化热解,611.65~792.25℃内发生硫酸盐(或亚硫酸盐)逐步分解,热解失重达到最大值。运用Friedma法、Kissinger法、Starink法对非等温动力学数据进行分析,3个阶段的表观活化能分别是96,174,230 k J/mol。各阶段样品稳定性逐渐提高,为硫铁化合物自燃的综合判据提供依据。