青鳞鱼下脚料水解蛋白的制取及其营养评价

以青鳞鱼（Harengula zunast)下脚料为原料，采用碱萃取，蛋白酶水解，浓缩，喷雾干燥等手段，制得水解鱼蛋白。研究了碱萃取，蛋白酶水解条件及不同沉淀方法对水解鱼蛋白沉淀效果的影响，并对水解鱼蛋白制品营养价值进行了评价，结果表明，下脚料水解鱼蛋白制品含粗蛋白72．9％，氨基酸总量67．6％，其中必需氨基酸占44．6％，氨基酸分为96，苏氨酸为其限制性氨基酸（1973年FAO／WHO标准），无机盐钙，镁，铁，锌，铜，磷含量丰富，以有机溶剂（异丙醇，乙醇)为沉淀剂沉淀水解蛋白时，粗蛋白损失率约为30％（干基计）。     

A 15.4-ka paleoclimate record inferred from δ<Superscript>13</Superscript>C and δ<Superscript>15</Superscript>N of organic matter in sediments from the sub-alpine Daping Swamp,western Nanling Mountains,South China

We inferred past climate conditions from the δ¹³C and δ¹⁵N of organic matter (OM) in a sediment core (DP-2011-02) from the sub-alpine Daping Swamp, in the western Nanling Mountains, South China. In the study region, a 1000-m increase in altitude results in a ~0.75‰ decrease in δ¹³C and a ~2.2‰ increase in δ¹⁵N. Organic carbon stable isotope (δ¹³C) values of the dominant modern vegetation species, surface soils, and the core samples taken in the swamp exhibit a strong terrestrial C3 plant signature. Comprehensive analysis of the core indicates both terrestrial and aquatic sources contribute to the OM in sediment. Temperature and precipitation are most likely the critical factors that influence δ¹³C: warm and wet conditions favor lower δ¹³C, whereas a dry and cool climate leads to higher δ¹³C values. Higher δ¹⁵N values may result from greater water depth and increased primary productivity, promoted by large inputs of dissolved inorganic nitrogen, induced by high surface runoff. Lower δ¹⁵N values are associated with lower lake stage and reduced productivity, under drier conditions. Therefore, stratigraphic shifts in these stable isotopes were used to infer past regional climate. Measures of δ¹³C and δ¹⁵N in deglacial deposits, in combination with total organic carbon (TOC) and nitrogen (TN) concentrations, the TOC/TN ratio, coarse silt and sand fractions, dry bulk density and low-frequency mass magnetic susceptibility, reveal two dry and cold events at 15,400–14,500 and 13,000–11,000 cal a BP, which correspond to Heinrich event 1 and the Younger Dryas, respectively. A pronounced warm and wet period that occurred between those dry episodes, from 14,500 to 13,000 cal a BP, corresponds to the Bølling–Allerød. The δ¹³C and δ¹⁵N data, however, do not reflect a warm and wet early Holocene. The Holocene optimum occurred between ~8000 and 6000 cal a BP, which is different from inferences from the nearby Dongge cave stalagmite δ¹⁸O record, but consistent with our previous results. This study contributes to our understanding of climate-related influences on δ¹³C and δ¹⁵N in OM of lake sediments in South China.     

Genome size of <Emphasis Type="Italic">Alexandrium catenella</Emphasis> and <Emphasis Type="Italic">Gracilariopsis lemaneiformis</Emphasis> estimated by flow cytometry

Flow cytometry(FCM) technique has been widely applied to estimating the genome size of various higher plants. However, there is few report about its application in algae. In this study, an optimized procedure of FCM was exploited to estimate the genome size of two eukaryotic algae. For analyzing Alexandrium catenella, an important red tide species, the whole cell instead of isolated nucleus was studied, and chicken erythrocytes were used as an internal reference. The genome size of A. catenella was estimated to be 56.48 ± 4.14 Gb(1C), approximately nineteen times larger than that of human genome. For analyzing Gracilariopsis lemaneiformis, an important economical red alga, the purified nucleus was employed, and Arabidopsis thaliana and Chondrus crispus were used as internal references, respectively. The genome size of Gp. lemaneiformis was 97.35 ± 2.58 Mb(1C) and 112.73 ± 14.00 Mb(1C), respectively, depending on the different internal references. The results of this research will promote the related studies on the genomics and evolution of these two species.     

中国西北地区东部短时强降水时空特征

基于中国西北地区东部136个气象站2001-2011年每6 h地面降水常规观测资料、1 674个自动站2009-2011年逐时降水资料,运用气候统计、线性趋势、归一化、分区域统计以及降水集中度（PCD）和集中期（PCP）分析等方法,研究了西北地区东部短时强降水的时空分布和气候特征。结果表明：该地区短时强降水日数年际变化不大,但区域性的短时强降水过程呈明显增加趋势;短时强降水主要发生在7月上旬至8月下旬,且具有明显的日变化特征;短时强降水总频次的空间分布与地势分布比较一致,高频高值区多位于夏半年环流盛行西南气流的迎风坡附近;在空间上PCD由东南向西北越来越集中,PCP自东向西逐步推迟。     

An improvement of soil temperature simulations on the Tibetan Plateau

The simulation of soil temperature on the Tibetan Plateau (TP) plays a dominant role in the performance of both global climate and numerical weather forecast models. To improve the simulation of soil temperature on the TP, the Johansen soil thermal conductivity parameterization scheme was introduced into Community Land Model 3.5 (CLM3.5) and Regional Climatic Model 4 (RegCM4). The improved CLM3.5 and RegCM4-CLM were utilized to conduct offline and regional simulation experiments on the TP. Comparison of the new and old schemes revealed that CLM3.5 provides high thermal conductivity parameters of mineral soil solid on the TP. The Johansen scheme is more practical for the TP than the soil thermal conductivity parameterization in CLM3.5. The simulation of soil temperature and liquid water content was improved in offline experiment. The improved parameterization scheme can also reduce the simulation error of soil temperature in winter throughout the entire TP.     

Analysis for temperature and pressure fields in process of hydrate dissociation by depressurization

An improved axisymmetric mathematic modeling is proposed for the process of hydrate dissociation by depressurization around vertical well. To reckon in the effect of latent heat of gas hydrate at the decomposition front, the energy balance equation is employed. The semi‐analytic solutions for temperature and pressure fields are obtained by using Boltzmann‐transformation. The location of decomposition front is determined by solving initial value problem for system of ordinary differential equations. The distributions of pressure and temperature along horizontal radiate in the reservoir are calculated. The numeric results indicate that the moving speed of decomposition front is sensitively dependent on the well pressure and the sediment permeability. Copyright © 2010 John Wiley & Sons, Ltd.     

An SMP critical state model for methane hydrate‐bearing sands

Mechanical properties of methane hydrate‐bearing soils are complex. Their behavior undergoes a significant change when hydrates dissociate and become methane gas. On the other hand, methane hydrates are ice‐like compounds and, depending on the hydrate accumulation habits and the degree of hydrate saturation, may cement soil particles into stronger and stiffer soils. A new constitutive model is proposed that is capable of capturing essential characteristics of hydrate‐bearing soils. The core of the model includes the spatial mobilized plane concept; a transformed stress, t_ij; the critical state; and the subloading framework. The proposed model gives soil responses due to stress changes or hydrate saturation changes or both. The performance of the model has been found satisfactory, over a range of hydrate saturation and confining pressures, using triaxial test data from laboratory‐synthesized samples and from field samples extracted from Nankai Trough, Japan. Copyright © 2015 John Wiley & Sons, Ltd.     

http://www.sciencedirect.com/science/article/pii/S1674987111001319

The microbial diversity in Wuli Area,Qinghai-Tibetan Plateau was investigated using 16S rRNA gene phylogenetic analyses.A total of 117 bacterial and 66 archaeal 16S rRNA gene clones were obtained from the Wuli cold springs.The bacterial clones could be classified into Pwteobacteria,Acidobacteria, Deinococci,Sphingobacteria,Flavobacteria.Nitrospirae,Actinobacteria,Gemmatimonadetes, and unclassified-bacteria;and the archaeal clones could be classified into Crenarchaeota and Thaumarchaeota.Among the major groups,Pwteobacteria and Crenarchaeota were dominant in the bacterial and archaeal 16S rRNA gene clone libraries,respectively.The clone sequences obtained in Wuli cold springs were closely related to those from cold habitats,such as snow/ice/soils on high mountains or at high latitude.Especially,the microbial community composition of Wuli Area was more similar to that in Tibetan glaciers than cold environments of other locations.The data presented in this study have implications for a better understanding of microbial diversity in cold springs on the Qinghai-Tibetan Plateau.     

Creep Failure of Roof Stratum Above Mined-Out Area

By taking into account the rheological behavior of the rock mass, the creep failure of a roof stratum seated on pillars in mined-out area is analyzed through a newly developed visco-elastic model. The time-dependent deflection of the roof stratum is obtained by numerical inversion of Laplace transform. The study shows that when creep properties of both the pillars and roof stratum are considered, the expected deflection in the roof stratum increases with time. Consequently, the roof would fail when the critical tensile stress is reached as the result of the increased deflection. To demonstrate the present analytical procedure, the failure time of roof stratum of the Xingtai Gypsum Mine in China was estimated, and the results obtained agreed with the observation. The case study indicates that the analytic approach provides a new way to assess the potential impact of the time-dependence of the roof stratum deformation and is useful in predicting its stability above a mined-out area.