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991.
The diatom genus Pseudo-nitzschia blooms throughout New Zealand's coastal waters. More than a decade of monitoring data were analysed in this study and seasonality was a significant factor in the appearance of Pseudo-nitzschia blooms. Austral spring and summer were the main bloom periods, although there were regional differences. Between January 2000 and August 2011, 8.4% of 29,000 seawater samples analysed for Pseudo-nitzschia exceeded the voluntary trigger level for biotoxin testing (10×104 cells l?1), and these were analysed by fluorescent in situ hybridisation (FISH) assays. Pseudo-nitzschia fraudulenta and P. pseudodelicatissima (low domoic acid [DA] producers) were the dominant bloom formers throughout New Zealand (each contributing 25%) followed by the highly toxic P. australis (10%). Shellfish flesh testing for DA was triggered on 8477 occasions between 2000 and 2011, but no samples exceeded the regulatory limit (20 mg/kg); the maximum concentration was 13 mg/kg (Marlborough Sounds, mid-winter 2010). 相似文献
992.
993.
???????????????????????????????????????嶫?????????GPS????????????????????????????????λ??ó?????????β???????仯???????????2001???????8.1???????????β?????????д?????μ?仯????????仯?????????ж??????????С????????????????????????????????????????8.1????????????????????????????????о????????????????β???????п??????????????????? 相似文献
994.
THE CORRESPONDING ANALYSIS OF HEAVY-METAL POLLUTION OF SOIL IN ZHUZHOU CITY ShangJincheng(尚金城);LongAimin(龙爱民)LiBin(李斌);JiangJ... 相似文献
995.
996.
In this study, sea surface salinity(SSS) Level 3(L3) daily product derived from soil moisture active passive(SMAP)during the year 2016, was validated and compared with SSS daily products derived from soil Moisture and ocean salinity(SMOS) and in-situ measurements. Generally, the root mean square error(RMSE) of the daily SSS products is larger along the coastal areas and at high latitudes and is smaller in the tropical regions and open oceans. Comparisons between the two types of daily satellite SSS product revealed that the RMSE was higher in the daily SMOS product than in the SMAP, whereas the bias of the daily SMOS was observed to be less than that of the SMAP when compared with Argo floats data. In addition, the latitude-dependent bias and RMSE of the SMAP SSS were found to be primarily influenced by the precipitation and the sea surface temperature(SST). Then, a regression analysis method which has adopted the precipitation and SST data was used to correct the larger bias of the daily SMAP product. It was confirmed that the corrected daily SMAP product could be used for assimilation in high-resolution forecast models, due to the fact that it was demonstrated to be unbiased and much closer to the in-situ measurements than the original uncorrected SMAP product. 相似文献
997.
浮游生物主要由浮游植物和浮游动物组成,是湖泊生态系统的重要组分.嵌套性结构及物种间的互作关系对群落的分布格局、功能乃至稳定性都具有重要意义,然而到目前为止,我们对此仍知之甚少.为此,本研究以东太湖为研究区域,在2019-2020年期间进行了春、夏、秋、冬季的观测调查,根据浮游生物群落的组成和多样性特征,结合群落分布矩阵和二分网模型研究浮游生物的嵌套性格局及其互作关系,并探讨其驱动机制.结果显示:(1)在时间上,春、秋、冬季水体的理化特征较为相似,但与夏季的水质差异显著.在空间上,西南部区域的综合污染指数显著高于东北部;(2)环境异质性使得浮游植物呈现出明显的嵌套性分布,即秋、冬季群落是春、夏季群落的子集.然而,浮游动物并未呈现该分布特征;(3)浮游生物的互作关系具有明显的季节特征:冬季的互作网络组成最简单,物种竞争最激烈,物种的特异性关系、物种脆弱性和一般性最小,说明浮游生物群落的稳定性在冬季最弱.综上所述,水环境的时空差异性造成的生态位分离可能是造成浮游生物嵌套性及其互作网络季节性变化的主要机制. 相似文献
998.
This paper presents a simplified nonlinear solution for piled raft foundations in layered soils under vertical loading. Based on the elastic–plastic analysis of a single pile in a layered soil, the shielding effect between a receiver pile and the soil is taken into account to modify the conventional interaction factor between two piles. An approximate approach with the concept of the interaction factor is employed to study the nonlinear behavior of pile groups with a rigid cap. Considering the variation of soil properties, the solution to multilayered elastic materials is used to calculate the settlement of the soil. The interactions between pile–soil–raft are taken into account to determine the stiffness matrix of the piled raft. By solving the stiffness matrix equations, the settlement and the load shared by the piles and raft could be obtained. Compared with results of the available published literatures, the proposed solution provides reasonable results. 相似文献
999.
Haiying Hu Lidong Dai Heping Li Jianjun Jiang Keshi Hui 《Mineralogy and Petrology》2014,108(5):609-618
Electrical conductivity measurements on dry polycrystalline K-feldspar were performed at 1.0 to 3.0 GPa and 873 to 1,173 K with a multi-anvil high-pressure apparatus and the Solartron-1260 Impedance/Gain Phase Analyzer in the frequency range of 10?1 to 106 Hz. At each temperature the complex impedance displays a perfect semi-circular arc that represents the grain-interior conduction. Under the experimental conditions, electrical conductivity exponentially increases with increasing temperature and slightly decreases with increasing pressure; however, the effect of pressure on the conductivity is less pronounced than that of temperature. The activation enthalpy decreases slightly from 0.99 to 1.02 eV with increasing pressure, and the activation energy and activation volume for K-feldspar are 0.98 eV and 1.46?±?0.17 cm3/mol, respectively. According to these Arrhenius parameters, ionic conduction is proposed to be the dominant conduction mechanism in K-feldspar at high temperatures and pressures, and potassium ions are the charge carriers transporting by an interstitial mechanism. The diffusion coefficient of potassium at high temperatures was calculated from our conductivity data on K-feldspar using Nernst–Einstein equation, and the results were compared with the previous experimental results. 相似文献
1000.
甘肃拾金坡金矿床是北山造山带南部的一处重要中型金矿床。矿体以石英脉和蚀变岩形式产出,受东西向断裂控制,赋矿围岩为早泥盆世拾金坡二长花岗岩。矿石中主要金属硫化物为黄铁矿及少量方铅矿、闪锌矿和磁黄铁矿。石英脉两侧花岗岩发生强烈的硅化、黄铁绢英岩化和绿泥石化。热液蚀变绢云母40 Ar/39 Ar坪年龄为(364.6±3)Ma,表明成矿作用发生在晚泥盆世。矿石石英中流体包裹体可分为早晚两期:早期流体包裹体群包含不同气液比水溶液包裹体和含CO2包裹体,指示成矿过程存在流体沸腾作用,其均一温度集中在280~325℃,盐度(w(NaCl))为7.86%~9.21%;晚期流体包裹体群只发育水溶液包裹体,均一温度集中于160~230℃,盐度为9.47%~11.10%。成矿流体属中温低盐度、富CO2流体。流体从早阶段演化到晚阶段,温度降低约100℃,压力由约113 MPa骤减到约11 MPa。流体包裹体的δ18 OH2O值为1.39‰~3.39‰,δD值为-71‰~-99‰。氢氧投图中,石英脉和蚀变岩样品构成良好的线性关系,暗示初始成矿流体主要来自变质热液,晚期有强烈大气降水加入。矿石金属硫化物δ34S值变化范围为4.44‰~11.33‰,峰值为8‰~9‰,呈塔式分布。与区域S同位素资料对比分析表明,石英脉型矿石S主要来自前寒武系基底,蚀变岩型矿石S更多地继承了花岗岩围岩S。综合分析认为,拾金坡金矿床属于造山型金矿,形成于造山晚期挤压—伸展转换环境。 相似文献