壳聚糖抑菌性能研究进展

壳聚糖又名甲壳胺,是甲壳素脱乙酰的产物,学名为1,4-2-氨基2-脱氧-β-D葡萄糖。壳聚糖来源于甲壳动物和昆虫的外骨骼,在地球上含量及为丰富。作为一种天然的多阳离子化合物,由于其具有良好的生物降解性、生物相溶性、无毒性和广谱抗菌性等特点,近年来越来越受到人们的重视,尤其在壳聚糖的抑菌方面,关于壳聚糖的抑菌机理抑菌效果和构效关系等方面都进行了大量的研究,由于壳聚糖的水溶性较差,限制了它的应用范围,根据这一特点,人们开始致力于其水溶性衍生物的开发和抑菌方面的研究与应用,取得了不少新的研究进展,为壳聚糖在抗菌方面的应用提供了大量的基础理论。作者就以上几个方面的问题进行了综述。     

Simultaneous estimation of surface soil moisture and soil properties with a dual ensemble Kalman smoother

In this paper, a new state-parameter estimation approach is presented based on the dual ensemble Kalman smoother(DEn KS) and simple biosphere model(Si B2) to sequentially estimate both the soil properties and soil moisture profile by assimilating surface soil moisture observations. The Arou observation station, located in the upper reaches of the Heihe River in northwestern China, was selected to test the proposed method. Three numeric experiments were designed and performed to analyze the influence of uncertainties in model parameters, atmospheric forcing, and the model's physical mechanics on soil moisture estimates. Several assimilation schemes based on the ensemble Kalman filter(En KF), ensemble Kalman smoother(En KS), and dual En KF(DEn KF) were also compared in this study. The results demonstrate that soil moisture and soil properties can be simultaneously estimated by state-parameter estimation methods, which can provide more accurate estimation of soil moisture than traditional filter methods such as En KF and En KS. The estimation accuracy of the model parameters decreased with increasing error sources. DEn KS outperformed DEn KF in estimating soil moisture in most cases, especially where few observations were available. This study demonstrates that the DEn KS approach is a useful and practical way to improve soil moisture estimation.     

利用正弦分段法模拟气温日变化

提出了一种运用正弦分段模拟法模拟气温日变化的新方法,并以山东省德州、菏泽、泰安、烟台、潍坊和青岛6个地面气象站2009年春、夏、秋、冬不同时段内一个月的自动观测逐时气温,与运用正弦分段模拟法模拟的逐时气温进行比较分析。结果表明,模拟气温与观测气温之间呈显著相关;该方法可以实现传统观测气温与自动观测气温的衔接以及满足作物模型对气温输入时间步长的精度要求;无论从空间或时间上,模拟气温与观测气温偏差及其变幅基本能满足应用需要。     

辽东大连金石滩新元古代碳酸盐岩臼齿构造形态及其沉积环境指示意义

辽东大连金石滩新元古代兴民村组上部灰岩段发育了一系列形态复杂多样的臼齿构造(Molar-tooth struc-ture,简称MT)。通过野外及室内综合研究鉴别出条带状、短直杆状、蠕虫状、细丝状、圆斑状(气泡状、瘤状)和碎屑状6种主要类型,其中以条带状最为发育。MT发育段主要由含砂屑或粉屑灰岩、泥晶灰岩、纹层状泥晶灰岩和含泥泥晶灰岩的韵律组成,系多个向上沉积动力减弱、水体变浅的潮下-潮间带沉积旋回序列。兴民村组MT发育的沉积环境具有一定水深和频繁波动的水动力特点,MT形态受宿主岩石性质的影响和控制。MT主要发育在浅潮下带-潮间带下部沉积微相。不同形态的MT及其组合分别宿主于不同的沉积岩相或沉积韵律,表现了MT形态的指相意义。     

蒙东地区与东北三省区域整合研究

在现有的区域整合理论基础上提出了经济、空间和制度等区域整合的三基点,并针对蒙东地区与东北三省区域整合问题构建了理论框架,在三个基点框架内分析了区域整合的基础条件、制约因素和动力机制,最后提出经济整合、空间整合与制度整合等具有可操作性较强的区域整合模式。     

Linear dichroism in ALD layers of TiO2

We prepare TiO₂ film by ALD and study their electronic properties by soft X-ray absorption spectroscopy (XAS) and photoelectron spectroscopy. We focus on XAS and X-ray linear dichroism to indentify band onset and learn about local distortion of the Ti–O octahedral atomic and about defects which cause Ti-based electronic states within the band gap.     

Distribution of <Superscript>226</Superscript>Ra in the Arctic Ocean and the Bering Sea and its hydrologic implications

Radium-226 (²²⁶Ra) activities were measured in the surface water samples collected from the Arctic Ocean and the Bering Sea during the First Chinese National Arctic Research Expedition. The results showed that ²²⁶Ra concentrations in the surface water ranged from 0.28 to 1.56 Bq/m³ with an average of 0.76 Bq/m³ in the Arctic Ocean, and from 0.25 to 1.26 Bq/m³ with an average of 0.71 Bq/m³ in the Bering Sea. The values were obviously lower than those from open oceans in middle and low latitudes, indicating that the study area may be partly influenced by sea ice meltwater. In the Bering Sea, ²²⁶Ra in the surface water decreased northward, probably as a result of the exchange between the ²²⁶Ra-deficient sea ice meltwater and the ²²⁶Ra-rich Pacific water. In the Arctic Ocean, ²²⁶Ra in the surface water increased northward and eastward. This spatial distribution of ²²⁶Ra reflected the variation of the ²²⁶Ra-enriched river component in the water mass of the Arctic Ocean. The vertical profiles of ²²⁶Ra in the Canadian Basin showed a concentration maximum at 200 m, which could be attributed to the inputs of the Pacific water or/and the bottom shelf water with high ²²⁶Ra concentration. This conclusion was consistent with the results from ²H, ¹⁸O tracers.     

On the transplantation and cultivation ofKappaphycus alvarezii in China

A 2-year study onKappaphycus alvarezii (Doty) Doty introduced to Hainan Island from the Philippines in 1985 showed promising results. The average daily growth in weight reached 10% at a favourable temperature of about 26°C. Experimental results showed that timely cutting of the plant was an effective way to obtain new cuttings for cultivation and accelerate growth. New cuttings 0.05 kg in weight are suggested to be used as “seeds” and the old plant should be harvested. At present, artificial cultivation with a type of underwater raft applicable in places where there is strong wind will expand cultivation to more regions in Hainan Province. This paper was originally published in Chinese inOceanologia et Limnologia Sinica 19(5): 410–418, 1988. The plant under discussion wasEucheuma alvarezii Doty which was previously calledE. striatum in the article, and which now becomesKappaphycus alvarezii (Doty) Doty. To the original title, “in China” was added. Only the essence of the original article was presented.     

藏北申扎地区上二叠统木纠错组的建立及皱纹珊瑚组合

在申扎县城东南木纠错南东岸附近发现一套巨厚的以白云岩、白云质灰岩为主组成的岩系,厚达2348m。该岩系整合覆于下二叠统下拉组之上,并于其底部发现中国南方晚二叠世早期珊瑚动物群中的重要分子WaagenophyllumindicumcrassiseptatumWu和LiangshanophyllumstreptoseptatumWang两种,与其共生的还有Lobatophyllumzakan-genseWu和WaagenophyllummegacolumetumWu,它们共同组成一个晚二叠世早期特有的皱纹珊瑚动物组合,命名为Waagenophyllum-Liangshanophyllum-Lobatophyllum组合。将含有这一珊瑚化石组合的以白云岩、白云质灰岩为主的岩系另建立新组———木纠错组,该组在层位上相当于中国南方上二叠统的吴家坪组。