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1.
李绪焜 《中国海洋大学学报(自然科学版)》1989,(Z3)
CHIMEHERB人工皮是由海洋生物材料制成的烧伤创面覆盖材料,主要成分是甲壳胺(chi-tosan).经山东省13所医院在不同类型的烧伤创面,历时3年的临床应用496例表明:CHIMEHERB人工皮对烧伤创面有良好地促进愈合作用,适用于新鲜Ⅲ°创面、供皮区创面、深Ⅱ°削痂创面、脱痂创面以及部分切痂植皮创面.不适于感染严重的烧伤创面.该人工皮不致敏,无刺激,无吸收中毒之虞,虽然弹性与粘附性还不理想,但不失为我国目前较完好的一种创面覆盖物. 相似文献
2.
从1989年4月～1990年10月,我科在69例病人中使用CHIMEHERB人工皮,覆盖治疗了供皮区,Ⅱ°烧伤创面、脱痂创面的残余肉芽创面.临床应用表明:CHIMEHERB人工皮能加快创面的愈合,是目前较好的一种创面覆盖物,用人工皮覆盖创面2～3天后,人工皮干燥,不需再换药,可减轻病人的痛苦. 相似文献
3.
全国临床研究组 《中国海洋大学学报(自然科学版)》1989,(Z3)
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. 相似文献
4.
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. 相似文献
5.
本研究初步评价CHIMEHERB人工皮的治疗效果.74例,105个创面应用人工皮:供皮区47个创面,愈合时间平均为9±1.94d(天),油纱布对照为11.7±1.93d(P<0.01);14个浅Ⅱ°新鲜创面,70％在3～5d内逐渐干燥与创面紧密粘附,平均愈合时间为9.8±3.09d;11个存留上皮组织的削痂深Ⅱ°创面,平均5.7±1.7d干燥,平均愈合时间为10.55±3.09d,不需植自体皮;8个削痂刨面至脂肪组织或切痂创面4～9d更植自体皮,其存活率近乎100％,2个创面因残留坏死组织而失败;人工皮应用于16个自体皮间隙创面,除三个网状植皮和一个条状植皮创面失败外,所植自体皮都在人工皮下扩展融合,未观察到占位现象;对后期残余小创面有良好的效果.本研究结果提示人工皮对创面愈合具有有利影响.主要适用于供皮区、浅Ⅱ°新鲜创面、深Ⅱ°脱痂和削痂后存留上皮组织较多的创面、自体皮间隙创面和后期残余小创面,不适宜于深Ⅲ°新鲜创面. 相似文献
6.
用青岛海洋大学生物材料研究所研制、海威生物材料有限公司生产的CHIMEHERB人工皮治疗烧伤50例.其中用于切、削痂创面10例,Ⅲ°创面20例,肉芽创面12例,供皮区创面3例.削痂创面一次覆盖面积最大23％,切痂创面13％.人工皮下可移植点状小皮片,亦可移植微粒皮,是一种较好的覆盖创面的生物材料.治疗浅Ⅱ°烧伤可使创面愈合时间提前2～4d(天);用于深Ⅱ°创面愈合时间为19～21d.人工皮治疗Ⅱ°创面,最大贴敷面积为60％.它对烧伤肉芽创面有促进周围上皮生长加速创面愈合的作用. 相似文献
7.
应用CHIMEHERB人工皮治疗烧伤病人125例.疗效观察表明,该人工皮具有与创面粘附牢固,减少创面水、电解质和蛋白质的丢失,减轻疼痛,促进上皮生长等功能.无排斥反应,存用方便和成本低廉.临床与生化检验证实,CHIMEHERB人工皮对肝肾功能无不良影响.适用于浅度烧伤创面、供皮区创面,及中、小面积深度烧伤的切、削痂创面. 相似文献
8.
使用甲壳胺人工皮复盖Ⅱ°烧伤新鲜创面,深Ⅱ°及Ⅲ°削切痂创面,供皮区创面共20例、25个创面,发现有减少创面渗出,减少疼痛,减少换药次数,节省敷料,防止加深,比传统方法提前2～3d(天)治愈的优点. 相似文献
9.
刘润文 《中国海洋大学学报(自然科学版)》1989,(Z3)
22例临床应用研究的结果表明,人工皮最佳适应证是浅Ⅱ°烧伤、供皮区创面,亦能用于烧伤残余肉穿小创面.一旦克服早期粘附性差,抗感染能力差后,将可能大面积Ⅲ°烧伤切痂后的良好覆盖物,目前尚不适宜在混合移植中替代异体皮或异种猪皮. 相似文献
10.
应用CHIMEHERB人工皮覆盖烧伤切(削)痂后自体网状植皮创面30例、44个创面,每例平均应用体表面积为5.22％,网状皮扩展比例为1:3.结果有明显积液者5个创面(11.36);感染3个创面(6.82％);需要补植皮创面4个(9.1％).人工皮具有良好的透气性和透湿性,可给创面造成无菌的内环境,未观察到过敏反应和排异现象,贮藏不需特殊设备,使用方便,具有人工皮所要求的基本特性,作为自体网状植皮表层覆盖物,可取得良好效果,值得临床推广应用. 相似文献
11.
Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding. 相似文献
12.
Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors. 相似文献
13.
Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake. 相似文献
14.
This study tests the hypothesis that the in situ void ratio of surficial marine sediments may be predicted from shear wave velocity-depth data with a reliability equal to that of other methods currently available. Shear wave velocity is fundamentally controlled by the number of grain-to-grain contacts per unit volume of material and by the effective stress across those contacts. In this study, three previously established empirical formulae are used to predict void ratio from velocity-depth data. Field data were acquired along a transect off the northern Californian coast across which water depth increased from 35 to 70 m and seafloor sediment type varied from sand to silty-sand, respectively. A towed seafloor sled device was used to collect shear wave refraction data, and a marked, systematic decrease in velocity was observed along the line, ranging from 35-70 m/s for the coarse, near-shore material to 25-40 m/s for the finer, offshore deposits. Void ratios predicted from these velocities were compared with data measured directly from box-core samples. Of the formulae used for prediction, two agree remarkably well with the control data. Both predicted and control values increase from 0.6-0.8 for the sandy material to 1.1-1.5 for the silty-sand. Thus, this study does not disprove the hypothesis set and demonstrates the potential of field shear wave velocity-depth data as a means of delineating spatial variation in void ratio for surficial marine sediments in a remote, nondestructive manner. 相似文献
15.
Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease (0.84% ～ 1.88%) of organic carbon content from the upper reaches to the estuary.δ13C values of particulate organic carbon was in the range of -24.9×10-3 to -26.6×10-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ13C and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs (soil organic matter) among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream. 相似文献
16.
Andrzej Chybicki 《Marine Geodesy》2018,41(1):1-23
Current trends of development of satellite derived bathymetry (SDB) models rely on applying calibration techniques including analytical approaches, neuro-fuzzy systems, regression optimization and others. In most of the cases, the SDB models are calibrated and verified for test sites, that provide favorable conditions for the remote derivation of bathymetry such as high water clarity, homogenous bottom type, low amount of sediment in the water and other factors. In this paper, a novel 3-dimensional geographical weighted regression (3GWR) SDB technique is presented, it binds together methods already presented in other studies, the geographically weighted local regression (GWR) model, with depth dependent inverse optimization. The proposed SDB model was calibrated and verified on a relatively difficult test site of the South Baltic near-shore areas with the use of multispectral observations acquired by a recently launched Sentinel-2 satellite observation system. By conducted experiments, it was shown that the proposed SDB model is capable of obtaining satisfactory results of RMSE ranging from 0.88 to 1.23[m] depending on the observation and can derive bathymetry for depths up to 12m. It was also shown, that the proposed approach may be used operationally, for instance, in the continuous assessment of temporal bathymetry changes, for areas important in the context of ensuring local maritime safety. 相似文献
17.
N. H. Khadge 《Marine Georesources & Geotechnology》2000,18(3):251-258
As a part of the environmental impact assessment studies, geotechnical properties of sediments were determined in the Central Indian Basin. The undrained shear strength and index properties of the siliceous sediments were determined on 20 box cores of uniform dimension collected from various locations in five preselected sites. The maximum core length encountered was 41 cm and most of the sediments were siliceous oozes consisting of radiolarian or diatomaceous tests. The shear strength measurements revealed that surface sediments deposited in recent times (0-10 cm) have a shear strength of 0-1 kPa; this value increases with depth, reaching 10 kPa at 40 cm deep. Older sediments have greater strength because of compaction. Water content varies in the wide range of 312-577% and decreases with depth. The clay minerals such as smectite and illite are dominant and show some control over water content. Wet density, specific gravity, and porosity do not indicate any notable variation with depth, thereby indicating a uniform, slow rate of sedimentation. The average porosity of sediments is 90.2%, specific gravity 2.18, and wet bulk density 1.12 g/cm 3 . Sediments exhibit medium to high plasticity characteristics, with the average plasticity index varying between 105% and 136%. Preliminary studies on postdisturbance samples showed an increase in natural water content and a decrease in undrained shear strength of sediments in the top 10- to 15-cm layer. 相似文献
18.
J. N. Pattan Ch. M. Rao A. A. Migdisov S. Colley N. C. Higgs L. Demidenko 《Marine Georesources & Geotechnology》2001,19(3):155-165
The rare earth element (REE) distribution in nine deep-sea ferromanganese nodules and their associated siliceous sediments from the Central Indian Ocean Basin (CIOB) have been studied to elucidate the REE relationship among them. Total REE concentration varies from 398-928 ppm in the nodules and 137-235 ppm in the associated sediments, suggesting two- to four-fold enrichment in the nodules compared to associated sediments. REE of nodules and their associated sediments show a positive correlation, suggesting REE are supplied from a common source such as seawater. The positive correlation between REE of nodules and sediments from the CIOB is contrary to the competitive scavenging of REE between nodules and sediment in the equatorial Pacific Ocean. REEs in the nodules are carried by Fe, P, and Ti, whereas in the sediment they are carried by P and Mn phases. A similar REE fractionation pattern with middle REE enrichment over heavy and light REE in both the nodules and their associated sediment suggest fractionation is independent of REE abundance and their carrier phases. 相似文献
19.
Lori E. Fenstermacher Gregory B. Crawford Jeffry C. Borgeld Tristan Britt Douglas A. George Meredith A. Klein Neal W. Driscoll Larry A. Mayer 《Marine Georesources & Geotechnology》2001,19(2):135-145
Detailed acoustic surveys of benthic sediments were conducted in July 1995 and September 1998 in the vicinity of Humboldt Bay, California. During these surveys, a band of enhanced acoustic backscatter was observed offshore from the bay entrance, approximately parallel to the isobaths, in water depths ranging from 16-24 m. In order to assess the cause of the increase in backscatter levels, a more comprehensive study was conducted in August and September 1999 using 100 kHz side-scan sonar, bottom grab sampling and underwater video recording. New observations indicated that a dense population of sand dollars ( Dendraster excentricus ) coincided with the enhanced backscatter band. Compared to the two previous acoustic studies, the central section of the band expanded westward by 180 m and the southern section of the band shifted eastward by 160 m, possibly resulting from a change in the biological or physical factors which influence the location and breadth of sand dollars. The relationship between high sand dollar abundance and enhanced acoustic backscatter was further verified in the nearshore region off Samoa Beach California, where a dense, banded population of sand dollars was previously observed. Video footage confirmed the presence of a band of sand dollars, also nominally parallel to the isobaths, in water depths of 8-15 m. A band of enhanced backscatter coincided with the dense sand dollar population. The identification of dense aggregations of sand dollars through enhanced acoustic backscatter could lead to the use of acoustic techniques to study sand dollar distributions and abundance. 相似文献
20.
Vast reserves of marine minerals are known to occur within the Mexican Exclusive Economic Zone. These reserves include: (1) heavy mineral placers rich in titanium and iron along the coast of San Antonio del Mar, Baja California and the southern States of Oaxaca and Guerrero; (2) phosphorites, which represent the only source for superphosphate fertilizers along the Pacific coast off the Baja California peninsula and the Gulf of Tehuantepec; and (3) manganese oxide deposits in nodule and crusts located adjacent to the Clarion-Clipperton Zone and containing high concentrations of Cu + Ni + Co (up to 1.9%), which are essential for the steel and super-alloy industries. Few but important efforts toward surveying these deposits have been carried out by Mexican and international researchers. Relevant data generated by these investigations are reviewed here and put together in a single document. Adequate knowledge of Mexican mineral resources is essential for the development of management strategies when offshore mining starts during this century. Thus, the review discusses the economics inherent to ocean mining in Mexico, setting baselines for future exploration and development activities in the Mexican Exclusive Economic Zone. 相似文献