飞机试飞的自然结冰潜势预测及检验评估          下载免费PDF全文

倪洪波  李佰平  闫文辉  李静  张莹  张华  倪萍 《气象科技》2022,50(2):254-266

自然结冰试飞是运输类飞机合格审定必须实施的高难度、高风险试飞科目，需要在环境温度、云中液态水含量（LWC）和云滴中值体积直径（MVD）满足条件，含有大量过冷水的环境中完成规定的飞行动作。利用2020年3月16日、26日及27日阎良机场国产某大型运输机自然结冰试飞的地面、高空、卫星、雷达和机载探测等多源观测资料，对3次自然结冰试飞气象条件进行了对比分析，并验证了李佰平等改进的自然结冰潜势算法有效性。结果表明：改进的自然结冰潜势算法对于结冰区域的预报较为准确，但在结冰强度预报上需进一步优化。西风系统因水汽条件不足，结冰气象条件较南支系统要差。高空冷空气未到达试飞区域前，云中环境温度偏高，结冰强度较弱；冷暖空气交汇的区域，LWC较高，MVD较为合适，结冰较强。研究结果对未来在阎良机场开展运输类飞机自然结冰试飞的窗口期和空域选择、协同指挥保障均具有参考意义。  相似文献   

高效液相色谱 串联质谱法测定水产品中的4种四环素类药物残留量   总被引：1，自引：0，他引：1       下载免费PDF全文

刘艳萍  冷凯良  王清印  王志杰  孙伟红  王瑜  邢丽红 《海洋科学》2009,33(4):34-39

建立了水产品中四环素(Tetracycline)、土霉素(0xytetracycline)、金霉素(chlortetracyline)和强力霉素(Doxycycline)4种四环素类抗生素残留量的高效液相色谱-串联质谱(HPLC-MS/MS)测定方法.以MTC缓冲液提取水产品中的四环素类残留物,经HLB固相萃取柱净化,采用LC-MS/MS选择反应监测(SRM)正离子模式测定,可一次对水产品中的四环素、土霉素、金霉素和强力霉素进行定性和定量.4种物质定量下限均可达到2.0μg/kg.适用于水产品中四环素类抗生素多残留的同时确证检测.  相似文献   

虾夷扇贝毒素yessotoxins(YTXs),中国沿海贝类中首次发现的一组贝类生物毒素   总被引：6，自引：0，他引：6       下载免费PDF全文

高春蕾  刘仁沿  梁玉波  王宗灵  刘永健  庞敏  张芳  潘宁  许道艳  邵魁双 《海洋学报》2010,32(3):129-137

采用高效液相色谱-串联质谱方法对我国近海贝类中腹泻性贝毒成分进行研究,结果发现采自北黄海大连附近海域的海湾扇贝和虾夷扇贝含有25~41μg/kg的虾夷扇贝毒素(yessotoxin,YTX),在虾夷扇贝体内还含有37.2μg/kg的45-OH-YTX,并在5种贝中发现微量的Homo-YTX毒素组分,这是首次报道在我国贝中检出此类毒素。虾夷扇贝毒素YTXs是一类含有2个磺酰基的脂溶性多环聚醚类化合物,对小鼠的腹腔注射急性致死毒性很高,毒理作用机制尚不清楚。本研究的结果说明我国贝类体内生物毒素成分复杂,亟需进行毒素成分结构、来源生物、生态毒理效应、分布规律及安全限定标准的研究。  相似文献   

Chronology of Early to Mid-Pleistocene sediments in the northern North Sea: New evidence from amino acid and strontium isotope analyses     

《Quaternary Geochronology》2022

Sediments deposited during glacial-interglacial cycles through the Early to Mid-Pleistocene in the North Sea are chronologically poorly constrained. To contribute to the chronology of these units, amino acid racemization (AAR) and strontium (Sr) isotope analyses have been performed on samples from four shallow borings and one oil well along a transect in the northern North Sea. D/L Asp (aspartic acid) values obtained through reverse-phase liquid chromatography in the benthic foraminiferal species Elphidium excavatum is focused on because of consistent results and a good stratigraphic distribution of this benthic species. For the Early Pleistocene, an age model for the well 16/1–8, from the central part of the northern North Sea based on Sr ages allows for dating of the prograding wedges filling the pre-Quaternary central basin. A regional calibration curve for the racemization of Asp in Elphidium excavatum is developed using published ages of radiocarbon-dated samples and samples associated with the previously identified Bruhnes/Matuyama (B/M) paleomagnetic boundary and a Sr age from this study. Based on all the available geochronological evidence, samples were assigned to marine oxygen isotope stages (MIS) with uncertainties on the order of 10–70 ka.Sr ages suggest a hiatus of <2 million years (Ma) possibly due to non-deposition or low sedimentation between the Utsira Formation (Pliocene) and the Early Pleistocene. An increase in sedimentation rates around 1.5 ± 0.07 Ma (∼MIS 51) may partly be due to sediment supply from rivers from the south-east and partly due to the extension of ice sheet around 1.36 ± 0.07 Ma from the Norwegian coast to the central North Sea. A possible basin-wide glaciation occurred around 1.1 Ma (∼ MIS 32) (upper regional unconformity/top of unit Q4 in this study), resulting in erosion and regional unconformity. Two interglacials in the Norwegian Channel have been dated: the Radøy Interglacial to 1.07 ± 0.01 Ma (possibly MIS 31, the ‘super interglacial’), and the Norwegian Trench Interglacial to 0.50 ± 0.02 Ma (possibly MIS 13). A massive till unit identified at the same stratigraphic level in all shallow borings may partly represent an extensive MIS 12 glaciation. This study shows that the combined use of amino acid racemization data and Sr isotope chronology can refine the chronological ambiguities of Quaternary North Sea sediments related partly to the impact of glacial processes.  相似文献   

海水中溶解态铁的伏安极谱法与液芯波导光纤法测定          下载免费PDF全文

龙爱民  党爱翠  程远月  陈绍勇 《海洋学报》2009,31(1):152-158

尽管铁为地壳中丰度位居第4的元素,但它在海水中的浓度却很低,浓度一般为0.05~2.0 nmd/dm3[1]。近年来,国内外的海洋科学家在进行海洋生态系统初级生产力、碳循环等重要生态过程及其对全球气候变化影响的研究中发现,海洋中的铁对浮游植物的生长、初级生产力的水平有着十分重要的影响甚至成为了“限制性因子”,在多个“高营养盐、低叶绿素(HNLC)”海区所实施的富铁实验的结果很好地印证了铁元素在海洋生态系统中的重要作用[2]。最新的研究成果表明近岸海水中的铁可能对浮游植物的种类组成起到决定性的作用,进而对包括氮、磷、硅在内的其他元素的生物地球化学行为产生深远的影响[3]。  相似文献