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卡德藻自养、异养与兼养培养的比较研究 总被引：2，自引：0，他引：2
本文对卡德藻在自养、异养和兼养培养条件下的比生长速率、细胞密度、细胞色素组成及脂肪酸组成等方面进行了比较研究。兼养卡德藻的细胞密度大于自养条件和异养条件下细胞密度之和。兼养培养的卡德藻比生长速率是自养的 2倍 ,异养的 1.3倍。兼养和异养生长的对数期较自养的长。光合自养培养卡德藻最适光强为 10 0 0 0 lx,而兼养培养最适光强范围为 10 0 0～ 2 0 0 0 lx。在自养和兼养培养时亚油酸的含量很高 ,自养和兼养状态下分别为 16 .6 %和 17.4 9%。 EPA合成的量较低。异养藻的多不饱和脂肪酸的产量较自养藻和兼养藻要低。兼养藻细胞光合色素组成和含量与自养藻细胞的基本一致 ,但在异养条件下藻细胞色素组成发生明显改变。 相似文献
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为揭示木钙对兰州黄土水理性质的影响,基于不同的木钙掺量和养护龄期,通过水滴入渗试验、渗透试验和崩解试验分析木钙土斥水性、渗透性和水稳性,并利用X射线衍射试验、扫描电镜试验探讨木钙土的改良机理。研究结果表明:木钙的掺入可以提升黄土的斥水性、水稳性,低掺量木钙土提升幅度有限,高掺量木钙土整体表现良好,而减弱渗透性的作用有限;木钙土的水理性质发挥具有龄期效应;28 d养护龄期下,木钙土的水理性质参数随木钙掺量的变化存在广义上的峰值,但峰值与木钙掺量的关系存在一定差异;木钙土的水理性质同力学性质保持了一定的正向关联性。木钙土并未产生新的矿物成分,但土颗粒双电层厚度变薄,而且胶结生成物包裹联结颗粒、填充孔隙,从而改善木钙土的水理性质。 相似文献
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为揭示太湖流域降雨和湖水酸根阴离子长期变化特征及环境意义,通过历史数据收集和采样分析,对太湖流域降雨和湖水中的SO42-、NO3-变化特征和来源进行了研究.结果表明：自1990s以来太湖流域降雨中SO42-呈显著下降趋势,年平均下降率为0.28 mg/（L·a）;NO3-浓度却呈显著上升趋势,年平均增长率为0.05 mg/（L·a）,降雨中氮污染呈现加重的趋势.与之相反,湖水中SO42-呈显著上升趋势,年平均增长率为1.24 mg/（L·a）;NO3-浓度却呈显著下降趋势,年平均下降率为0.02 mg/（L·a）.30年以来,太湖水体SO42-/NO3-比值不断升高,远高于降水SO42-/NO3-比值.研究认为：流域SO2排放引起的酸沉降是湖水SO42-浓度增长的最重要原因,但氮氧化物排放并未引起湖水NO3-浓度升高,说明太湖流域对大气沉降的氮氧化物有滞留作用,而太湖水体是流域大气沉降硫酸盐的重要汇.综合治理太湖流域酸性物质排放对防止太湖水体酸化和治理富营养化都具有重要意义. 相似文献
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HUANG Xiaohang LAM Patrick P L LIN Xuezheng LIU Chenlin BIAN Ji GAISANO Herbert 《海洋学报(英文版)》2007,26(1):159-164
1 IntroductionSecretion is a basic function of all living organ-isms. In fish, like in mammals, neurotransmitters,hormones, enzymes and other macromolecules aresecreted in several neuronal, neuroendocrine and ex-ocrine organs and tissues located in brain,… 相似文献
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1 Introduction T he light-harvesting com plex (LH C ) com posedofphotosynthesis pigm ents and associated proteins arelocated on the thylakoid m em brane of chloroplast inhigherplants and algae. T he capture oflightenergy isthe first step in photosynthesis and is largely accom -plished by the pigm entprotein com plexes. To m axi-m ize the capture of light energy under various envi-ronm entalconditions, the LH C s w ith differentchro-m ophore com positions have evolved in differentpho-tosynth… 相似文献
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Zhang Yingbin Xiang Chenlin Yu Pengcheng Zhao Lianheng Zhao John X. Fu Haiying 《Landslides》2022,19(1):187-197
Landslides - A general sliding block model for calculating permanent displacement of slope is presented. Ground shaking can be applied to base or block in a direction horizontal or parallel to the... 相似文献
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Chao Luo Dong Yang Zicheng Peng Zhaofeng Zhang Liu Weiguo Jianfeng He Chenlin Zhou 《中国地球化学学报》2008,27(3):257-264
A 10.35-m-long sediment core from the Luobei depression in Lop-Nut, Xinjiang, Northwest China, pro- vides detailed information about environmental changes during the Late Pleistocene. The samples taken every 5 cm of the core were analyzed for 10 environmental proxies, including magnetic susceptibility, granularity, chroma, car-bonate and loss on ignition （LOI）, and pH value. The chronology data are provided by the uranium/thorium disequi-librium dates. The sediments of the section were deposited during the last 32000 years. The results of analysis of 10 proxies were examined using multivariate statistical analysis, and the principal components were calculated. According to the results, the Late Pleistocene sequence contains four climatic and environmental stages appearing in the cycles of cold-wet and warm-dry changes. During 10-9 ka BP, it was the earliest warm episode in the Holocene. Environmental changes in this district were restricted by global change, as suggested by the analysis of glacial-interglacial cycles. But it was different from the mutative trend of a monsoon region in East China because of its own characteristics, which was the situation of cold-wet and warm-dry climate-environment change. The candidate reason may be the uplift of the Tibet Plateau and the westerly wind circulation. 相似文献
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