南海神狐海域天然气水合物开采数值模拟

实地钻探结果表明我国南海北部神狐海域存在大量天然气水合物,其作为未来我国潜在的可开发能源的调查和资源评价工作正在展开.利用国际上先进的多相多组分沉积物渗流模拟计算软件TOUGH+HYDRATE,以2007年5月国土资源部广州地质调查局在南海北部神狐海域SH2,SH3和SH7站位的钻探、测井数据为基础,建立实际水合物藏分层地质模型,利用不同的开采井设计方式进行单井降压和降压+注热开采模拟.结果表明,开采过程中水合物分解区域主要集中在开采井周边区域、水合物层与含水层界面处以及水合物层顶部靠近上盖层的区域.由于水合物分解吸热,水合物层的温度降低,使得热量从上盖层向水合物层传递,形成地温梯度的逆转,促进水合物层顶部逐渐产生分解界面.降压开采进行到后期开采井周围会形成渗透率很低的"二次水合物",影响开采的进行,所以利用降压+注热开采方法消除"二次水合物",使开采过程顺利进行.     

氮气笼型水合物的激光拉曼光谱

在253K和16MPa的压力下,于实验室内合成了氮气水合物,用显微共焦拉曼光谱对其N-N和O-H键伸缩振动的光谱特征进行了研究．结果表明,氮气水合物中的N-N和O—H键的拉曼峰分别为2322．4和3092．1cm^-1,与天然的空气水合物中的数据十分接近．另外,还测定了液氮和溶解于水中的氮分子中N—N键的拉曼峰值,分别为2326．6和2325．0cm^-1．氮气笼型水合物分解的拉曼谱图表明,氮分子同时进入水合物的大笼和小笼中,但由于氮分子在大、小笼中的环境氛围十分接近,其拉曼位移相差不大,故拉曼谱图只能显示N—N键伸缩振动一个峰．     

~(12)CO_2/~(13)CO_2体系中碳同位素的显微激光拉曼光谱研究

采用自行设计的装置制备了一系列不同比例的12CO2/13 CO2混合物,对混合物样品进行显微激光拉曼测试,获得CO2气体碳同位素分子的拉曼特征峰。对实验数据分析发现,12CO2的摩尔分数[x(12CO2)]与12CO2/13 CO2混合物中拉曼特征峰峰面积比之间存在数学关系式。根据拟合的关系式,利用显微激光拉曼光谱可以预测CO2气体碳同位素的组成,并为以后预测单个流体包裹体中12CO2的摩尔分数奠定了理论基础。     

Li+-CaxPb1-xTiO3湿敏纳米薄膜的激光拉曼光谱、晶格畸变和激光显微组织--应用"软模理论"解谱

测定了标题物Li^ -CaxPb1-xTiO3（缩写为Li-CPT,其中x=0．35,Li/Ti=1．0％,mol／mol,850℃／h)的激光拉曼光谱(LRS)和激光显微组织,并与湿敏性能极差的纯钛酸铅PbTiO3(缩写为PT)以及不同钙掺杂量的钛酸铅CaxPb1-xTiO3(缩写为CPT,x=0．08,0．16,0．24,0.32,0．40)的LRS进行比较,Li-CPT以及CPT的LRS与PT的LRS相比有很大差别,仅在75,125,190,273和585cm^-1出现五个谱峰．应用“软模理论”将其分别归属于PT四方晶相的五个特征单模E（ITO),A1(ITO),E(2TO),B1 E和A1(3TO)的红移及宽化,PT的其它五个特征单模在Li-CPT及CPT的谱图中完全消失或被淹没,对于这种拉曼活性的降低,可以根据“软模理论”与晶格畸变作用的关联加以解释,Pauling离子半径较小的Ca^2 的掺杂,等价取代了半径较大的Pb^2 的晶格位置,降低了四方晶相畸变度δ=c／a和不对称性导致的各向异性,不单消除了薄膜冷却时位移型相变可能引起的破裂,而且改变了晶格中氧八面体“TiO6”及十二面体“PbO12”的几何结构和电荷分布,改变了晶格c轴上M-O(M-Ti,Pb)键的化学环境,直接阻尼了M-O键的伸缩振动软模,减小了电偶矩及其自发极化,使Li-CPT的振动模的拉曼活性大大降低,因此LRS提供了一种表征晶格畸变的有效方法。反过来也佐证了“软模理论”可以用来解释拉曼光谱。     

Li＋-CaxPb1－xTiO3湿敏纳米薄膜的激光拉曼光谱、晶格畸变和激光显微组织——应用“软模理论”解谱

测定了标题物Li^＋-Ca_xPb_1－xTiO₃ (缩写为Li-CPT, 其中x＝0.35, Li/Ti＝1.0%, mol/mol, 850 ℃/h)的激光拉曼光谱(LRS)和激光显微组织, 并与湿敏性能极差的纯钛酸铅PbTiO₃ (缩写为PT)以及不同钙掺杂量的钛酸铅Ca_xPb_1－xTiO₃ (缩写为CPT, x＝0.08, 0.16, 0.24, 0.32, 0.40)的LRS进行比较, Li-CPT以及CPT的LRS与PT的LRS相比有很大差别,仅在75, 125, 190, 273和585 cm^－1出现五个谱峰. 应用“软模理论”将其分别归属于PT四方晶相的五个特征单模E(1TO), A₁(1TO), E(2TO), B₁＋E和A₁(3TO)的红移及宽化, PT的其它五个特征单模在Li-CPT及CPT的谱图中完全消失或被淹没. 对于这种拉曼活性的降低, 可以根据“软模理论”与晶格畸变作用的关联加以解释. Pauling离子半径较小的Ca^2＋的掺杂, 等价取代了半径较大的Pb^2＋的晶格位置, 降低了四方晶相畸变度δ＝c/a和不对称性导致的各向异性, 不单消除了薄膜冷却时位移型相变可能引起的破裂, 而且改变了晶格中氧八面体“TiO₆”及十二面体“PbO₁₂”的几何结构和电荷分布, 改变了晶格c轴上M-O (M＝Ti, Pb)键的化学环境, 直接阻尼了M—O键的伸缩振动软模, 减小了电偶矩及其自发极化, 使Li-CPT的振动模的拉曼活性大大降低, 因此LRS提供了一种表征晶格畸变的有效方法, 反过来也佐证了“软模理论”可以用来解释拉曼光谱.     

Geochemical Characteristics and Significance of Organic Matter in Hydrate-Bearing Sediments from Shenhu Area,South China Sea

Rock-Eval pyrolysis and the biomarker composition of organic matter were systematically studied in hydrate-bearing sediments from the Shenhu area, South China Sea. The n-alkane distribution patterns revealed that the organic matter in the sediments appeared to originate from mixed sources of marine autochthonous input, terrestrial higher plants, and ancient reworked organic matter. The low total organic carbon contents (average < 0.5%) and the low hydrogen index (HI, <80 mg HC/g TOC) suggested the poor hydrocarbon-generation potential of the deposited organic matter at a surrounding temperature of <20 °C in unconsolidated sediments. The abnormally high production index and the fossil-originated unresolved complex mixture (UCM) accompanied by sterane and hopane of high maturity indicated the contribution of deep hydrocarbon reservoirs. Preliminary oil-to-source correlation for the extracts implied that the allochthonous hydrocarbons in the W01B and W02B sediments might have originated from the terrestrial source rocks of mature Enping and Wenchang formations, while those of W03B seem to be derived from more reduced and immature marine source rocks such as the Zhuhai formation. The results of the organic extracts supported the previous identification of source rocks based on the isotopic composition of C₂₊ hydrate-bound gases. The biomarker of methanogens, squalane, was recognized in the sediments of this study, possibly suggesting the generation of secondary microbial gases which are coupled with the biodegradation of the deep allochthonous hydrocarbons.     

GC–IRMS测定白色块状天然气水合物气体中的碳氢同位素

研究了GC–IRMS联用技术测定烃类气体碳氢稳定同位素的方法。利用气相色谱仪将烃类气体各组分分开,通过高温燃烧/裂解转化为CO2和H2,然后导入MAT–253稳定同位素质谱仪进行测试。用该方法测试的标准甲烷气体碳、氢同位素值和其标定值一致,测定结果的相对标准偏差分别为0.222‰和0.950‰。用该法测定了广东沿海珠江口盆地东部海域首次钻获的高纯度天然气水合物样品所释放的烃类气体碳氢稳定同位素值,其中δ13C为–69.78‰(VPDB),δD为–184.4‰(VSMOW)。GC–IRMS法精确度高,可用范围广,适用于海洋天然气水合物样品所释放烃类气体碳氢同位素的测定。     

基于量子化学计算方法的天然气水合物稳定性研究进展

天然气水合物以资源丰富、优质、洁净等特点,被视为21世纪新能源。天然气水合物稳定性的研究对天然气水合物资源勘探开发具有重要意义。本文简述了微观、介观、宏观、矿藏四个尺度天然气水合物稳定性的研究,重点从微观量子尺度介绍了量子化学计算方法对水合物晶体结构及其稳定性以及水合物宏观物理特性微观表征的计算研究。应用量子化学计算方法可以对天然气水合物的晶体结构、电子轨道分布、振动光谱、成键特性及主客体相互作用进行计算研究,其结果能够为天然气水合物在油气储运、水合物成藏、开采及其综合利用等方面的研究提供理论支持。目前,量子化学计算方法的优化与分子动力学模拟、分子力学模拟等方法的结合将有助于水合物形成和分解微观机理研究的发展,提升计算精度和扩大研究体系,为矿场尺度的天然气水合物资源开采利用提供理论支持。     

P-T stability conditions of methane hydrate in sediment from South China Sea

For reasonable assessment and safe exploitation of marine gas hydrate resource, it is important to determine the stability conditions of gas hydrates in marine sediment. In this paper, the seafloor water sample and sediment sample (saturated with pore water) from Shenhu Area of South China Sea were used to synthesize methane hydrates, and the stability conditions of methane hydrates were investigated by multi-step heating dissociation method. Preliminary experimental results show that the dissociation temperature of methane hydrate both in seafloor water and marine sediment, under any given pressure, is depressed by approximately -1.4 K relative to the pure water system. This phenomenon indicates that hydrate stability in marine sediment is mainly affected by pore water ions.     

Analysis of Volatile Compounds in Sea Bass (Lateolabrax japonicus) Resulting from Different Slaughter Methods Using Electronic-Nose (E-Nose) and Gas Chromatography-Ion Mobility Spectrometry

Sea bass (Lateolabrax japonicus) is known for its unique flavor and high nutritional value. In this study, the influence of slaughter methods on the volatile compounds (VOCs) in sea bass was investigated using electronic nose (E-nose) technology and gas chromatography-ion mobility spectrometry (GC-IMS). VOCs in raw and cooked sea bass resulting from different slaughter methods were effectively distinguished using both techniques. Aldehydes, ketones, and alcohols were associated with the basic flavor of sea bass, whereas esters, organic acids, and furans enriched the aroma. In raw sea bass, the fishy odor was the strongest in the HSD group (head shot control death), followed by that in the IFD (ice faint to death) and BDS (bloodletting to death) groups. The VOC content increased and stabilized after steaming, enhancing pleasant odors such as fatty and fruity aromas. In cooked sea bass, the content of diacetyl and ethanol was the highest in the EAD group (eugenol anesthesia to death), which may be a residue of eugenol, imparting a distinct irritating chemical odor. Furthermore, abundant (E)-2-octenal, 2-heptanone, benzaldehyde, and esters in the BDS group imparted a strong, pleasant aroma. The findings indicate that heart puncture and bloodletting is the preferred slaughter method to maintain sea bass quality, providing new insights into the volatile changes in sea bass induced by different slaughter methods.