泥岩与页岩地化特征对比——以鄂尔多斯盆地安塞地区延长组7段为例

鄂尔多斯盆地安塞地区,延长组7段(长7段)发育优质的页岩与泥岩烃源岩。开展泥岩与页岩的区别研究,有助于评价页岩与泥岩的品质,识别它们对油气资源的贡献。基于25口重点探井开展了岩心描述工作,同时选取泥岩及页岩样品共计81块开展地球化学测试与分析,以获得泥岩与页岩的地化特征并开展差异性对比。结果表明,长7段泥岩与页岩均处于热成熟生油的热演化范围、有机质丰度均达到好烃源岩标准、页岩有机质类型以Ⅰ型与Ⅱ1型为主,而泥岩有机质类型以Ⅱ1与Ⅱ2型为主。在页岩与泥岩的地化特征对比上发现,页岩有机质丰度显著高于泥岩,其中最主要的影响因素是有机碳含量大于4%的页岩样品数量较多;页岩有机质类型更偏于生油,其中最主要的影响因素是高氢指数的腐泥质组分相对丰富;页岩的游离烃、热解烃以及生烃潜量均优于泥岩,但页岩中孔隙及微裂缝对游离烃的统计影响更大;由于页岩孔隙及微裂缝更容易发育,泥岩对烃类的滞留能力可能更强,而页岩中烃类的排运相对容易;泥岩与页岩的生标参数并无显著差异。

Comparison of the Activity Differences in Two Terminal Oxidases between Upland Cotton and Sea-island Cotton

[Objective] This study was to reveal the differences in two terminal oxdiases,so as to provide theoretical basis for the selection of upland and sea-land hybrid materials. [Methods] Using 7 shares of upland cotton cultivars and 4 shares of sea-land cultivars as experimental materials,the change differences in AAO and PPO activities during whole growth period of the materials tested were studied. [Results] Two terminal oxdiases both in upland and sea-land cotton cultivars assumed similar change laws during whole growth period. AAO activity assumed a low-high trend,and there is a peak at the early stage. PPO activity presented two peaks,and that at the early stage was higher than at the late stage; the first peak is obviously higher than the second for sea-land cultivars,and two peaks are not remarkably different for upland cultivars. [Conclusion] The differences in AAO and PPO activities of sea-land and upland cotton cultivars observed on Jul.4th and Aug.6th,may provide guidance for the selection of upland and sea-land hybrids.

录井资料在王集油田西南缘油气层综合解释中的应用

由于沉积相变、复杂的断块构造以及油质多样等因素的影响,王集油田西南缘储层岩电关系、油水关系、油气产层的电性特征及录井资料响应特征极为复杂。通过统计分析工区内已有的录井、试油等基础资料,在分析该区油气水层的录井资料(常规地质录井、气测录井、地化录井)响应特征的基础上,总结出了本区产层的气测、地化录井参数下限,提出了利用气测全烃曲线形态和气测、地化资料的差异性进行本区录井油气层综合解释,经实践应用取得了较好的效果。

Spatial Differentiation of Elements in Soils on Red-Earthy Hill Landscape of Central China

Samples of 21 soil profiles and 165 top soils from an area of approximate 1.5km^2 on red-earthy hill landscape were collected and analysed.The content of Ca,Mg,K,P,Fe,Mn,Zn and Cu in soils relate with the kind of parent material and the position of topography,however,there is great variation due to the local difference of the form of soil utilization.From the difference in spatial distribution of elements content,it is believed that eight kinds of elements are lost by chemical leaching and physical translocation,meanwhile some are added (such as Ca,P,K,Mg) and some mobilized (such as Fe,Mn,Zn,Cu and P) through cultivation,fertilization and irrigation in the soils on the landscape investigated.The sectional differentiation in abundance or deficiency of elements in top soils on the landscape investigated is distinct,which is important for carrying out agricultural management and reasonable fertilization according to local conditions.

Variability of Surface Sensible Heat Flux over Northwest China

The present study documents the variability of surface sensible heat flux over Northwest China using station observations for the period 1961 2000.It is found that the afternoon and nighttime sensible heat flux variations are remarkably different.The variability of the instant flux in the afternoon is much larger than in the nighttime.The afternoon and nighttime flux anomalies tend to be opposite.The diurnal and seasonal dependence of sensible heat flux variations is closely related to the diurnal cycle of mean land-air temperature difference.The relationship of sensible heat flux with land-air temperature difference based on the instant value differs from that based on the daily mean.The present study indicates the importance for the models to properly simulate mean land-air temperature difference and its diurnal and seasonal variations in order to capture surface sensible heat flux variability over Northwest China and predicts its plausible impacts on climate.

Sino-Western Regional Differences and Translation

Cultuare difference always exists in many aspects. Due to the national characters, regionalism, and times, translation can not be in a position when we try to translate without considering the language culture. Cultural difference between English and Chinese, determines the different features between English and Chinese.

A Study on the Cultural Meanings of Qiang’s Traditional Dress and Adornment

Since 2008 when the Wenchuan earthquake occurred, media from different countries and regions across the world reported the earthquake so that a less well-known ethnic group of China, the Qiang ethnic minority, has attracted attention around the world. The Qiang ethnic minority could be dated back to the Shang Dynasty （ca. 1600-1046BC）. The long-standing Qiang culture is an important part of those brilliant Chinese cultures. The Qiang’s traditional dress and adornment is an integral part of the Qiang culture, appreciating unique ethnic characteristics and cultural meanings. Being against the backdrop of promoting cultural diversity nowadays, this paper makes a brief introduction to the Qiang’s traditional dress and adornment and gives an explanation of their rich unique cultural meanings so as to present the Qiang’s traditional dress and adornment to the world, facilitate their going out to the world and communication with other cultures in the world, and enrich the world’s ethnic cultures.

What Influences Cooperative Motivation of Foreign Brides From Southeast Asian Countries in Taiwan？

Because women in Taiwan have had more and more opportunities to receive higher education and engage in different kinds of work, they have had developed increasingly higher standards for their marriage partners. Men who are in the lower socioeconomic working classes such as those who work in agriculture, or fishing, or who are disabled can no longer compete in local marriage market. As a result, these men have begun to look for their brides from other countries to continue the family line, do the housework, and take care of their parents-in-law. In addition to the fact that these foreign brides are often young and from rural areas, language barriers and cultural differences make it difficult for them to raise and educate their children in Taiwan. The inability of these brides often leads to a higher percentage of children who are developmentally delayed, have poor pronunciation, behavior problems, and low academic achievement. Governmental agencies and schools recognize these issues and have tried to help foreign-born mothers take better care of their children. However, there are several influential factors that can limit the cooperative motivation of these foreign-born mothers, including language barriers, parenting stresses, low socioeconomic status, and cultural limitations. Therefore, governmental agencies and related professionals must take these factors into consideration to provide comprehensive services and a better learning environment.

Regional Diferences in the Efect of Climate and Soil Texture on Soil Organic Carbon

The agricultural soil carbon pool plays an important role in mitigating greenhouse gas emission ana unaerstanamg the son orgamc carbon-climate-soil texture relationship is of great significance for estimating cropland soil carbon pool responses to climate change. Using data from 900 soil profiles, obtained from the Second National Soil Survey of China, we investigated the soil organic carbon （SOC） depth distribution in relation to climate and soil texture under various climate regimes of the cold northeast region （NER） and the warmer Huang-Huai-Hai region （HHHR） of China. The results demonstrated that the SOC content was higher in NER than in HHHR. For both regions, the SOC content at all soil depths had significant negative relationships with mean annual temperature （MAT）, but was related to mean annual precipitation （MAP） just at the surface 0-20 cm. The climate effect on SOC content was more pronounced in NER than in HHHR. Regional differences in the effect of soil texture on SOC content were not found. However, the dominant texture factors were different. The effect of sand content on SOC was more pronounced than that of clay content in NER. Conversely, the effect of clay on SOC was more pronounced than sand in HHHR. Climate and soil texture jointly explained the greatest SOC variability of 49.0% （0-20 cm） and 33.5% （20-30 cm） in NER and HHHR, respectively. Moreover, regional differences occurred in the importance of climate vs. soil texture in explaining SOC variability. In NER, the SOC content of the shallow layers （0-30 cm） was mainly determined by climate factor, specifically MAT, but the SOC content of the deeper soil layers （30-100 cm） was more affected by texture factor, specifically sand content. In HHHR, all the SOC variability in all soil layers was predominantly best explained by clay content. Therefore, when temperature was colder, the climate effect became stronger and this trend was restricted by soil depth. The regional differences and soil depth influence underscored the importance of explicitly considering them in modeling long-term soil responses to climate change and predicting potential soil carbon sequestration.