COOL AND FRESHWATER SKIN OF THE OCEAN DURING RAINFALL

Rainfall over the sea modifies the molecular boundary layers of the upper ocean through a variety of different effects. These cover the freshwater flux stabilizing the near-surface layer, additional heat flux established due to rain versus surface temperature differences, modification of physical parameters by temperature and salinity changes, enhancement of the surface roughness, damping of short gravity waves, surface mixing by rain, and transfer of additional momentum from air to sea. They are separately described and included in our surface renewal model to investigate the rain's influence on the cool skin of the ocean and the creation of a haline molecular diffusion layer. Simulations with the upgraded model show that the most important effect on the conductive layer is that of reduced renewal periods followed by additional surface cooling due to rain on the order of 0.1 K. At rain rates below 50 mm h-1 rainfall is not able to completely destroy the mean temperature difference across the cool skin. A freshwater skin is created that exhibits a salinity difference exceeding 4 under strong rainfall. Comparisons with field data of the cool skin taken during the Coupled Ocean Atmosphere Response Experiment confirm the upgraded renewal model. Surface salinity measurements taken during the same field campaign are consistent with the calculated salinity differences across the freshwater skin. The enhancement of surface roughness by natural rain is less pronounced than described in earlier laboratory studies of rain with large drop sizes only.     

绿鳍马面鲀(Navodon septentrionalis)鱼皮胶原蛋白的分离纯化及理化性质研究

利用酸溶法和酶溶法分离纯化绿鳍马面鲀(Navodon septentrionalis)鱼皮酸溶性胶原蛋白(ASC)和酶溶性胶原蛋白(PSC),并对所得的ASC和PSC的氨基酸组成、亚基组成、红外光谱(FTIR)、黏度和热变性温度,以及溶解度等性质进行系统分析。研究结果表明:马面鲀鱼皮酸溶性胶原蛋白(ASC)和酶溶性胶原蛋白(PSC)的得率分别为0.87%±0.15%和9.52%±0.41%(按鱼皮干重计算)。ASC和PSC中含有的主要氨基酸为甘氨酸(Gly),含量分别为323.3残基/1000残基和321.7残基/1000残基;二者中所含的亚氨基酸含量分别为191.1/1000残基和183.4/1000残基。氨基酸组成分析、SDS-PAGE和FTIR证实马面鲀鱼皮酸溶性胶原蛋白(ASC)为I型胶原蛋白,且其SDS-PAGE图中的亚基组成(α1-肽链和α2-肽链)、氨基酸序列,以及胶原蛋白构型与PSC明显不同。ASC和PSC的热变性温度(Td)分别为21.5℃和18.9℃,显著低于哺乳动物来源的胶原蛋白。ASC和PSC的最大溶解度出现在p H 2—3时,当Na Cl的浓度低于2%时,二者的溶解度就开始急剧下降。此外,冻干的胶原蛋白显示出疏松多孔的超微结构。综上,相对于哺乳动物类胶原蛋白,马面鲀鱼皮ASC和PSC的亚氨基酸含量和热变性温度较低,结构稳定性差,易于降解,可作为胶原蛋白肽的制备原料进行开发利用。     

烧伤病人中应用CHIMEHERB人工皮的临床研究

1989年4月～1990年10月期间,由全国组成的临床研究组10个烧伤单位对CHIMEHERB人工皮进行全面临床研究.研究目的是:(1)探索应用方法.(2)明确适应症.(3)评价疗效.在260例烧伤病人中,共应用365个不同类型创面,有效率为90.5％,其中优良率为79.7％.研究指出,CHIMEHERB人工皮的性能适合于作为暂时性创面覆盖物,对上皮生长具有有利影响,未发现占位和排斥现象,以及过敏和其他不良反应.主要适用于(1)供皮区,(2)Ⅱ°烧伤创面.(3)深Ⅲ°烧伤脱痂和削痂创面.(4)网状植皮和小皮片(或条状)植皮创面。(5)残余肉芽创面.亦可用于切痂创面.但不适于深Ⅱ°新鲜创面和切痂嵌皮.感染创面应用CHIMEHERB人工皮应结合抗感染措施.应用人工皮创面需良好包扎与固定.人工皮下渗出物多需引流.     

人工皮在烧伤创面的应用

16例烧伤病人应用CHIMEHERB人工皮覆盖26个创面,其中浅Ⅱ°及部分深Ⅱ°创面11个,深Ⅲ°削痂创面10个,切削痂覆盖自体网状皮创面5个,与辐照猪皮对照观察,临床获得较好效果.认为在有效的清创及正确的创面处理下覆盖人工皮能减少创面渗出,有利创面愈合.作为一种新型的生物性敷料,无同种异体皮或异种皮移植时的排异现象,但其本身不具抗菌能力.     

CHIMEHERB人工皮在皮肤微粒移植中的临床应用

在皮肤微粒播散移植中应用CHIMEHERB人工皮覆盖6例,8个部位取得了较满意的效果,显示CHIMEHERB人工皮覆盖部位比新鲜猪皮覆盖部位平均提前愈合8.5天,人工皮可作为微粒皮移植后覆盖物.     

考虑表皮效应的径向溶质迁移模型以及半解析解

径向示踪试验是一种非常有效的获取含水层弥散参数的试验方法,但传统径向示踪试验很少考虑抽水井附近的表皮效应(由于钻井施工工艺所导致抽水井附近一定区域水力性质发生变化).建立了考虑表皮效应的单井注入示踪试验模型,并利用Lapalce变换以及数值逆变换获得了该模型的半解析解.系统分析了表皮区域水力性质对示踪试验穿透曲线的影响规律.研究结果表明:表皮区域的弥散度越大,穿透曲线早期的浓度越高,且峰值越高;表皮孔隙度越大,穿透曲线早期浓度越低,后期浓度越高;此外,散度差异也会导致浓度分布曲线在表皮区域与含水层界面处发生突变.总之,表皮效应对径向溶质迁移产生了较大的影响,有必要将表皮效应考虑到径向示踪试验中去.     

Magnetostratigraphy of the Plio‐Pleistocene carbonate section of the Great Australian Bight

ODP Leg 182 drilled two north‐south transects in the western Great Australian Bight close to longitude 128°E. These transects penetrated a remarkably thick section of uppermost Pliocene and Pleistocene carbonate sediments, which are separated from Miocene sections by a major hiatus. In the eastern transect, at sites 1129, 1131 and 1127, the Brunhes‐Matuyama boundary (onset of C1n) was found at 343 m, between 280 and 300 m, and at 343 m below the sea floor, respectively. In the western transect, at sites 1132 and 1130, it was found between 170 and 181 m, and at 200 m, respectively. Within the Brunhes chron, inclination and intensity fluctuations and correlations between susceptibility and standard δ¹⁸O records were used to give age‐depth relations. These age relations from the palaeomagnetics are broadly consistent with the biostratigraphy and the δ¹⁸O results from Leg 182, but do not provide an entirely independent dataset. Rock magnetism stratigraphy at site 1131 revealed the principal bryozoan buildup to be at the time of the last glacial lowstand, as suggested by previous workers. At all sites the sedimentation rate increases from the basal unconformity up into the thick Upper Pleistocene section. In the western transect there appears to be a partial record of most of the Late Pliocene and Early Pleistocene chron boundaries (C1r1n to C2An3n) in a condensed section, but in the eastern transect only the Jaramillo (C1r1n) is observed.     

响应面法优化鱿鱼(Ommastrephes bartrami)皮胶原蛋白提取液脱色工艺研究*

提要 鱿鱼(Ommastrephes bartrami)皮胶原蛋白提取液为红棕色,不利于在食品中广泛地应用。为了进一步利用鱿鱼皮胶原蛋白,本文采用活性炭吸附法脱除鱿鱼皮胶原蛋白提取液中色素,优化脱色条件。在确定该色素特征吸收波长为420 nm条件下,分别研究了活性炭添加量、脱色时间、溶液pH值和吸附温度对鱿鱼皮胶原蛋白液色素脱除效果影响。在单因素实验基础上,选择吸附时间30 min,进行活性炭添加量、溶液pH值、吸附温度三因素三水平Box-Behnken中心组合响应面分析试验。结果表明：活性炭吸附鱿鱼皮胶原蛋白液色素最佳条件为活性炭添加量4.2%,溶液pH值2.27,脱色温度35 ℃,该条件下鱿鱼皮胶原蛋白液的脱色率为45.6%,蛋白质和氨基酸损耗率分别为19.65%和22.93%。脱色后鱿鱼皮胶原蛋白的甘氨酸含量最高(136.02 mg/g,相对含量23.05%),谷氨酸、精氨酸和脯氨酸含量也较高,而半胱氨酸和蛋氨酸总量不到1%,符合水产蛋白氨基酸和I型胶原蛋白氨基酸特点。     

近46a黑龙江水稻障碍型冷害及其与气候生产力的关系

利用黑龙江省稻作区46 a（1961—2006年）每年7—8月逐日平均气温、5—9月逐旬平均气温、降水量资料,采用气候统计方法分析了自然低温下障碍型冷害发生的规律和时空变化特征,基于logistic曲线方程模拟粳稻气候生产力,建立起5个区域粳稻气候生产力与障碍型冷害期间平均温度和冷害持续时间的关系模型。结果表明,近46 a间,20世纪70年代是障碍型冷害高发期,20世纪80年代是障碍型冷害发生频率由多至少的转折期,21世纪初为低发期。黑龙江省北部稻作区、东部稻作区和中部稻作区为障碍型冷害重发区,南部稻作区为中等发生区,西部稻作区为轻发区。5个区域障碍型冷害发生期间的平均温度与粳稻气候生产力相关性均不显著,而冷害持续时间对粳稻气候生产力影响显著,并具有明显的地域差异,北部、东部和南部极显著（通过0.01信度的显著性检验）,冷害持续时间每延长1 d,北部、东部和南部粳稻气候生产力分别下降119.89 kg/hm^2、213.60 kg/hm^2、133.84 kg/hm^2,西部和中部影响不显著。     

某建筑工程黄土地基处理方案比较分析

西安某建筑工程结构复杂,平面不规整,荷载要求差异大,为自重Ⅲ级湿陷性黄土地基。根据岩土工程资料和上部荷载要求,分析本地常用的地基处理方案,并进行经济性、安全性和可行性比较,提出要根据不同的地基土参数和上部荷载要求,安全、经济、灵活地选择地基处理方案。考虑到统一工艺和施工的方便性,最终采用灰土挤密桩复合地基和桩基础方案。同时,对工程实施过程中具体的参数选择、注意事项也进行了阐述,为同类地基处理提供了参考。