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By field investigation and water chemical monitoring, the groundwater environment of the shallow buried paleochannel zones and alluvial diluvial fans on the south coast plain of Laizhou Bay can be divided into 3 area: the salt groundwater district in the north, the transition district in the middle and the fresh groundwater district in the south.

通过野外实地调查和水化学监测,将莱州湾南岸平原浅埋古河道带及冲洪积扇浅层地下水水化学环境分为3大区域,即北部的全咸水区、中部的咸淡水过渡区和南部的全淡水区。

By using geological and geochemical data, the genetic type of the Silurian asphaltic sandstones in Tarim Basin is investigated and divided as the following:(1)Oxidized asphalt on surface or in shallow-layer is the heavy asphalt crude and solid oxidized asphalt or gilsonite formed by volatilization, oxidization, water washing and biodegradation in oil-layer outcrop area or near earth surface.

通过对地质、地球化学等资料的研究,认为塔里木盆地志留系沥青砂岩有5种成因类型:①表生—浅层氧化沥青是指在油层露头区或油层位于近地表处,由于挥发、氧化、水洗和生物降解等作用而形成的一些焦油状沥青质重油以及固体浅层氧化沥青或硬质沥青。

All the patients of shallow I degree and some patients of shallow II degree could be cured with nonsurgical therapy such as mydriasis, pressure bandage on drainage area and appropriate medicine.

浅Ⅰ度和部分浅Ⅱ度的病例可以通过散瞳、滤过区加压包扎及合理用药等保守治疗得以康复。

According to the analysis result,the condition of the Chengbei Sea ground settlement were summarized:1 The stratum of the study area above 30m is Quaternary Holocene deltaic deposit and neritic facies deposit,and the geologic structure is silty soil,muddy-silty clay,silty clay and silt.

根据分析结果,对埕北海域的地面沉降情况进行了总结:1研究区埋深30m以浅地层为第四纪全新世三角洲沉积和浅海相沉积地层,其结构是粉土、淤泥质粉质粘土、粉质粘土和粉砂。

A full term male infant, whose mother had been consuming alcohol during the pregnancy, was small for gestational age, had cardiac defect, jaundice, microcephaly, craniofacial dysmorphism, a dimple over sacral area, and poor activity and sucking power.

一个足月男婴,他的母亲在怀孕期间有酒精滥用的情形。这个案例表现出低出生体重、心脏缺损、黄疸、小头症、脸型特徵为:低发际、短眼睑、浅人中、薄上唇、背荐区有一浅凹、活力及吸吞力皆差。

Methods Twelve patients with open maxillary or frontal sinus defects have been repaired with this type of flap. The homolateral superficial temporal vessels were used as nutritional vein to form the temporal fascia island flap of the top superficial temporal artery and the island skin flap of the frontal superficial temporal artery.

对上颌窦、额窦开放性缺损12例患者,利用同侧颞浅动脉、静脉作为供养血管,形成颞浅动脉顶支颞筋膜岛状组织瓣和额支额部岛状皮瓣,通过皮下组织隧道将组织块移植到缺损的副鼻窦区,进行副鼻窦窦腔的充填和皮肤缺损的修复。

Special staining methods, such as Masson and the Van Gieson staining were used to study the distribution of collogen fibers and elastic fibers. ResultsBy HE staining, the subepithelial connective tissues and vessels in the pterygium were more prominent than normal conjunctival tissues. An amorphous subepithelial superficial hyalinized zone and coarse eosinophilic granular materials were observed in the pterygia, but they were not found in normal conjunctival specimens. Coarse fibers were visible only in the deeper subepithelial connective tissues of pterygial samples. With Masson′s staining, the dense staining of collagen fibers was also more prominent in the pterygium than in the subepithelial connective tissues of normal conjunctiva. Abnormal collagen fibers were visible in the deeper sub-epithelial connective tissues of pterygial samples. With Van Gieson staining, abnormal collagen fibers were visible in the deeper subepithelial connective tissues. Dark coarse elastic fibers were found in the abnormal fibers only in the subepithelial deep connective tissues of pinguecula in the pterygia but not in the conjunctiva. With immunohistochemistry staining, MMP-3 was strong in the pterygial epithelium, moderate in fibroblast and absent from pterygial vascular walls. LN was strongly expressed in the blood vessel wall, moderately in the epithelial basement membrane and absent from the entire stroma.

结果HE染色:翼状胬肉组织上皮下基质中存在结缔组织的增生和血管形成;基质浅层存在一无定形物质透明区及粗糙的颗粒样嗜酸性物质,在翼状胬肉体部深层基质中存在粗糙的纤维组织;正常球结膜组织细胞排列整齐;基质为疏松结缔组织,胶原纤维平行排列,其间可见成纤维细胞,散在少量中性粒细胞、毛细血管;Masson染色:翼状胬肉浅层基质中存在致密的胶原纤维染色,深层基质中的胶原纤维存在变性样改变;VG染色:翼状胬肉组织深层基质中存在大量变性的胶原纤维,其间夹杂黑色的弹性纤维;免疫组化染色法:MMP-3在翼状胬肉上皮细胞中呈强表达,成纤维细胞中呈中等强度表达,血管内皮细胞中未见表达;LN在血管壁中呈强表达,在上皮细胞基底膜中呈中等强度表达,在整个基质中未见明显表达;col Ⅲ在整个翼状胬肉基质中呈强表达。

Firstly, with the analysis of electric characteristics of a condensate gas reservoir, we find that there are some differences between Tri\|porosity logging amplitude, Deep Investigation Laterolog, Shallow Investigation Laterolog, and Microlaterolog, etc; secondly, in view of the feature of the condensate gas reservoir, the log interpretation model is built on the basis of the correlation of four reservoir parameters, and the reservoir grade scale is completed using conventional logging techniques combined with cross plot technique and the result of well testing; finally, according to the feature of Qiketai Formation and Sanjianfang Formation in the Hongtai oil field, we set up the reservoir classification criteria and divide the reservoir parameters into four types.

以吐哈盆地红台地区为例,对凝析气层的电性特征进行了分析,认为凝析气层在三孔隙度测井曲线幅度和深、浅、微电阻率等方面存在差异。针对研究区凝析气藏特点,在关键井&四性&关系研究的基础上,建立了储层参数测井解释模型,采用交汇图技术和实际试油、试气资料相结合的方法,对研究区目的层常规测井储集层的分类标准进行了分析,并结合红台气田七克台组和三间房组凝析气藏特点,建立了研究区储层参数分类评价标准,依据该标准将红台地区储集层划分为4类。

The strike of Huanghai block and Huaihai block in the east mainly tends towards north-east, while the strike of Shanxi block and the eastern edge of Ordos block in the west mainly tends towards north-west.(3) According to the feature of Moho, the crust of the research zone can be divided into six parts in the Shanxi block, Moho looks like a nearly north-south sunk belt, and the crust is thick; at the southern edge of the Inner Mongolia block and in the south of Yanshan block, Moho presents the structural features of fold belt, tending nearly towards east-west; at the eastern edge of Ordos block, the structure of Moho is relatively complex with nearly northwest folds.

3根据莫霍面的形态特征,研究区地壳可大致划分为6个区块;在山西地块范围内,莫霍面呈近南北向的凹陷带,地壳厚度大;内蒙古地块南缘和燕山地块南部,莫霍面表现出褶皱带的构造特征,其延展趋势为近东西方向;鄂尔多斯地块东缘,莫霍面构造相对复杂,呈近北西向凸、凹相伴的褶皱;黄淮海地块为莫霍面隆坳区,隆、坳相间排列,构造较复杂,但从整体上看,这是全区莫霍面最浅的隆起区段;鲁西台背斜主要为莫霍面断陷区,其断陷带沿枣庄-曲阜一线向北西方向延伸。

The results show that, the nitrate-N concentration in groundwater in the reed area was 0.2~0.8mg/L and significantly lower than that in surrounding wells (more than 20mg/L), and the reed wetland can remove nitrate pollution in shallow groundwater. The distribution of denitrifying bacteria showed obvious rhizosphere effect, and the higher biodenitrification in natural reed wetland was related to the distribution of denitrifying bacteria. There was a negative relationship between the nitrate-N concentration and the number of denitrifying bacteria in groundwater.

结果表明:芦苇区浅层地下水中硝酸盐氮仅为0.2~0.8mg/L,远低于湿地周围井水中硝酸盐氮质量浓度(大于20mg/L),芦苇湿地能够去除浅层地下水中硝酸盐污染;反硝化细菌在土壤中的分布呈现明显的根际效应;野生芦苇湿地较强的生物脱氮作用与反硝化细菌分布有关,地下水中硝酸盐氮含量与反硝化细菌分布呈负相关。

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