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Rainfalls can " deposit " the co2 in air , making it to take part in the process of karst , to dissolve and corrade carbonate rock . co2 concentration in soil become lower after heavy rainfall and become higher after general rainfall .( 8 ) the value of chemical characteristic of soil water in the high elevation area is lower than that in the low elevation area

降雨可以对coz产生影响,&沉淀&大气中的co :,使其参与到岩溶作用中,溶蚀碳酸盐岩;降雨对土壤空气中coz的影响与雨强、雨量有关,降雨量、雨强较大时,土壤空气中的c02产生受到抑制,降雨量和雨强较小时,土壤空气中的coz浓度升高。

Kreht also investigated homologous areas in brains of a few apes and monkeys and found that the cortices of these animals had areas with similar cytoarchitecture as that found in Broca's area.

Kreht 也调查到在一些人猿与猴子的脑袋中有类似的区域且发现这些动物的皮层都有与Broca' area 相似的区域。

Base on core observation and grain size analysis, and under associated consideration of logging trace characteristics, Chang8 reservoir in study area is classified into three sedimentatal microfacies, subsea river, mouth bar and river flank.3.The mian diagenesis in study area are: mechanical compaction, cementation, metasomasis and denudation in late diagenetic phase.4. In allocation of reservoir macroscopic heterogeneity, more heterogeneticer reservoir, class 1 and class 2, mainly locate in the center of subsea river or crook and divaricate of the river; class 3 and class 4 mainly locate in river flank, and the physical property of these locality are better.5. Diagenesis of reservoir have influence on the pore structure which influences the reservoir microscopic heterogeneity. The better the pore structure is, the slighter the reservoir microscopic heterogeneity is; on the contrary, the reservoir microscopic heterogeneity is serious.

本次研究所取得的主要成果及熟悉有:1、将合水地区长8储层细分为6个小层:长8_1~1、长8_1~2、长8_1~3、长8_2~1、长8_2~2和长8_2~3.2、依据岩心观察和粒度分析,并结合测井曲线特征,研究区长8储层分为水下分流河道、河口坝和河道侧翼四种沉积微相。3、研究区主要经历的成岩作用有:机械压实和压溶作用、胶结作用、交代作用、晚成岩期溶解作用。4、从宏观非均质性平面展布特征来看研究区宏观非均质较强的1类和2类区主要分布于水下分流河道中间或河道拐弯和分又处。3类和4类往则主要分布于水下分流河道侧翼,这些地方储层均质性相对较好。5、储层成岩作用影响储层的孔隙结构,储层的孔隙结构又对储层的微观非均质性有不同程度的影响,孔隙结构越好,则储层的均质性越好,储层的孔隙结构差,则非均质性强。

TyPe II collagen induced arthritisln the rat ank1e joint andoVathumin as antigen induced arthritis WA in the rabbit knee joint wereestab1ish2 Qualitative evaluation of me in skin, muscle, synovium, cedilagearound joint and blood was performed by OMA3 The CIA rats were treated on day 7 after hind paw swelling and erythemaAnimals were injected intravenously with ase at a dose of 10mg/kg,tWenty minuots 1ater, one ankle of the rats random1y assigned was exPosedlaser irradiation at l00J/cm fOr l000 seconds, and another ankle wasM grouP wihout laser The other two groups is unmanipulatedcontrol group and untreated CIA group Bimaleolar ankle widthmeasuremellts were taken in all animals every tWo days using amicrometer The histopathology of the ank1e Joint was assessed at day 21after disease onset4 The pro1iferating cell nuclear antigen WCNA of CIA treated by PDT andthe HMME group without laser was doterdrined by immunohistochemiStry5 The AfA rabbits were treated on day 7 after knee swelling and erythemaThe theraPy invo1ved lntravenous injection of l0mg/kg HMME, fOl1owedby 20 minues period in dim light, and transdermal light treatment with\l00 J/cm2 fOr l000 seconds The inner sides of the treated Anees wereirradiated at first, and then the outer side did 24 hours later, the synovialtissue of the Anees joint were removed and in situ cel1 aPoptosis wasdetCCted With tednal deoxync1eotidyl transferase-mediated dUTP nickend labelingR6suIt8:l The pathologic changes of CIA and AIA include subsynovial inflammation,opovial hyPerplasia, pannus formation, cartilage and bone destructionresemble RA.2 The studies demonstrated that there are different uptake of HMME withinskin, muscle, synovium, cartilage and b1ood, and the synovium cou1draPidly uPtake more ase than skin and cartilage at the firSt 30 minuesaller intravenous injection of HMME3 The bimaleolar anke width had no different among PDT treated group,H group withollt 1aser and untreated CIA group But hlstologicalevaluation showed statiStical1y significallt reductions in synovialhyperplasia, pannus formation and cart1lage reosion, bone destruction andtotal score in PDT treated group4 Image analysis showed that the ratlo bforeen the areas of the coufltedobect to that of the entire area in PDTtreated grOup is lower than that in conirol group, but the integrated oPticaldensity had no different between the two groups5 Imape analysis showed that the ratio between the area of the countedobject to that of the e

治疗组在大鼠出现踝关节红肿后1周,炎症达到高峰时进行PDT治疗。随机治疗大鼠一侧的踝关节,另。2。一一侧作单纯HMME 对照。治疗方法是大鼠麻醉后尾静脉注入 HMME10ngkg,20分钟后踝关节照光,激光波长627.sum,功率密度 100mwcm',照射时间1000秒,能量密度100)/。治疗后避光喂养72 小时。隔日一次测量大鼠的踝关节左右横径,治疗后两周取关节进行病理d 观察。 4。大鼠CIA模型用上述方法进行PDT治疗后,治疗组和单纯HMME 组用兔疫组化SP法检测石蜡切片的核增殖抗原。 5。兔AIA模型在关节炎出现第七天进行PDT治疗,随机治疗一侧膝关节,另一侧作自身对照。兔耳静脉注入I'arrainrelomg/Kg,20分钟后,膝关节用金蒸气激光照射,激光能量密度100)儿旷。24 /J'时后取膝关节滑膜作病理检查,并用脱氧核昔酸末端转移酶介导的缺口末端标记法原位检测凋亡细胞。结果: 1。模型观察:CIA大鼠炎症高峰期滑膜下炎细胞浸润明显,滑膜细胞明显增殖,炎症达到高峰后二周,血管缀形成,并侵蚀和破坏软骨和骨, CIA模型病理改变与人类RA相似。兔AIA模型膝关节滑膜病理可见滑膜细胞增生,滑膜下炎细胞浸润,也与人类RA滑膜改变相似。 2。关节周围组织中光敏剂含量的测定结果表明,各组织对HMME 的吸收速度和吸收量不同,荧光值一时间曲线不同,滑膜组织比皮肤和软骨对 HMME的吸收多,在 2 0分钟时即有明显差异。 3.PDT对CIA模型的治疗结果表明:PDT治疗后关节炎组、单纯 HMME组和治疗组踝关节左右横径统计学检验差异没有显著性,但病理评分PDT治疗组滑膜增生、血管资形成及软骨破坏、骨破坏和总分比关节炎对照组和HMME对照组好,统计学检验差异有显著性。。3_军医进修学院硕士学位论文中文摘要 4.PDT治疗组PCNA阳性细胞较对照组少,图像分析结果表明面密度(阳性染色的面积总和与统计视野面积的比值)治疗组小于对照组,统计学检验差异有显著性。。 5.PDT治疗组凋亡阳性细胞较对照组明显增多,图像分析结果单位视野内阳性细胞数和面密度PDT治疗组高于对照组,统计学检验差异有显著性。凋亡细胞核直径PDT治疗组较小,与对照组相比,统计学检验差异有显著性。结论:二。CIA、AIA的病理改变类似人类RA,可作为研究RA病因、发病机制、检查及治疗方法的模型。 2。各组织对HMME的吸收速度和吸收量不同,滑膜组织比皮。

Based on the seismic data obtained in deepwater area of northern South China Sea in recent years, the development of ancient Miocene reef was analyzed. The seismographic result shows typical reef feature in the Xisha uplift, such as the mound, high amplitude, middle frequency, middle continuity, and chaotic reflection. Some reef-like reflection was found in the Miocene Meishan Formation in Beijiao area of Qiongdongnan Basin.

中文摘要:基于近些年南海北部深水区采集的地震资料,对南海北部深水区中新世生物礁发育特点进行分析、对比和研究,认为西沙隆起地区发育典型的生物礁,具有丘状反射、强振幅、中频、中连和杂乱地震相,发现琼东南盆地北礁地区在中新世梅山组也有似礁相发育。

Ningbo Hongyun Electrical CO., Ltd is located in the west of Ningbo with more than 2,000 sq meters workshop area.We are professional in producing and developing different kinds of potentiometers with high quality, and are full of technology innovation. The company has a trade mark of . There is an excellent team of potentiometer development, production and sale. There are many series of potentiometer products, such as potentiometer with plastic seal, potentiometer with switch, position sensor potentiometer used in the car , control potentiometer with high-power and long life, Spanish potentiometer, inching potentiometer , encoder and so on. We keep ahead in many key technology area (noise、liner typer≤1%、life≥100,000 cycles).

宁波宏韵电子有限公司,坐落于宁波市西郊,厂房面积二千多平米,是一家专业生产、研发各类高品质电位器的技术创新型企业,公司注册商标,公司拥有优秀的专业电位器研发、生产、销售团队,产品有各种塑封电位器,带开关电位器、汽车位置传感电位器,大功率长寿命控制用电位器,西班牙电位器,微调电位器及编码器等多个系列产品,并在电位器多个关键技术(动噪声、静音,线性≤1%,寿命100万次以上…)具领先水平。

Ningbo Hongyun Electrical CO., Ltd is located in the west of Ningbo with more than 2,000 sq meters workshop area.We are professional in producing and developing different kinds of potentiometers with high quality, and are full of technology innovation. The company has a trade mark of . There is an excellent team of potentiometer development, production and sale. There are many series of potentiometer products, such as potentiometer with plastic seal, potentiometer with switch, position sensor potentiometer used in the car , control potentiometer with high-power and long life, Spanish potentiometer, inching potentiometer , encoder and so on. We keep ahead in many key technology area (noise、liner typer≤1%、life≥100,000 cycles).

公司简介:宁波宏韵电子有限公司,坐落于宁波市西郊,厂房面积二千多平米,是一家专业生产、研发各类高品质电位器的技术创新型企业,公司注册商标,公司拥有优秀的专业电位器研发、生产、销售团队,产品有各种塑封电位器,带开关电位器、汽车位置传感电位器,大功率长寿命控制用电位器,西班牙电位器,微调电位器及编码器等多个系列产品,并在电位器多个关键技术(动噪声、静音,线性≤1%,寿命100万次以上…)具领先水平。

In the process of reserve calculation using volumetric method, to confirm oil-bearing area is in fact to calculate polygon area.

在用容积法计算地质储量的过程中,含油面积的确定实际上是计算多边形的面积。

objective to introduce a method for repair of defects of alae nasi.methods transplantation of whole or partial free auricle composite tissue was designed in reconstruction of alae nasi.partial auricle composite tissue transplantation was used in 14 patients,the area of the graft was 1.0cm×1.5cm~1.9cm×2.5cm.whole auricle composite tissue transplantation was used in 6 patients,the area of the graft was 0.5cm×0.5cm~0.8cm×1.2cm.results all grafts survived.the grafts were dark red or light red in color,there were no blisters on them.follow-up of more than six months showed good results.conclusion in many methods for repair of defects of alae nasi,this method is simple,the appearance of alae nasi is good after operation and there is no new scar on face.

目的 修复鼻翼缺损。方法采用全层或部分耳廓复合组织游离移植的方法修复鼻翼缺损20例,其中以鼻翼残存瘢痕组织翻转作衬里,然后进行部分耳廓复合组织游离移植14例,移植物面积最小1.0cm×1.5cm,最大1.9cm×2.5cm;利用耳廓复合组织全层嵌入游离移植修复鼻翼缺损者6例,移植物面积最小0.5cm×0.5cm,最大0.8cm×1.2cm。结果 20例移植组织全部成活。色泽呈暗红至淡红不等,无水泡。随访半年移植物色泽与鼻组织基本近似,供区隐蔽。结论在诸多鼻翼缺损修复方法中,该方法简便易行、术后鼻翼外形好,面部显著部位不增加新的瘢痕,有独到优越性。

The ion concentrations were studied in both four snow pits on Hami Miaoergou FlatTopped Glacier and one snow pit on Haxilegen Glacier No.51 of Kuitun river in eastern Tianshan Mountain, and both snow pits were retrieved in 2004. The results show that the Ca2+, NO-3 and SO2-4, particularly Ca2+, are major ions in the snow of snow pits in both ablation and accumulation area and also in the ice of snow pits in accumulation area on Hami Miaoergou FlatTopped Glacier, where the relationships among major cation concentrations in snow of snow pits can be revealed by ion concentrations in the ice of snow pits, but the correlation between ion concentrations in the snow of snow pits and elevation is not obvious, which probably can be attributed to the narrow span of elevation and sparse snow pits on glacier. However, the good correlation between ion concentrations in the ice of snow pits and elevation indicates that the elution process weakened gradually with the elevation rise and temperature decrease.

对2004年获取的天山奎屯河哈希勒根51号冰川1个雪坑和哈密庙尔沟平顶冰川4个雪坑的离子浓度特征进行了研究,结果表明:Ca2+、NO-3和SO42-是哈密庙尔沟平顶冰川雪坑雪层和积累区雪坑底部冰中的主要离子(尤其是Ca2+),其雪层中的主要阳离子关系可在底部冰中得以较好的反映,但雪层中各离子浓度与海拔的相关性不明显,可能与海拔的跨度较小和挖取的雪坑较疏有关;雪坑底部冰中的离子浓度与海拔间明显的相关性说明淋融作用随着海拔升高、气温降低而逐渐减弱。

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