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21.
以紫露划4430^#为材料,用300×10^-6,150×10^-6,30×10^-6三种不同浓度的人工污染HgCl2溶液在多个不同时间(3,6,24h)对其处理,观察紫露草雄蕊毛污染突变的情况。结果表明:处理3h实验组能在正常的恢复时产生突变高峰,而6,24h则不能。3h实验组随着污染程度的增加,突变率呈现明显增加趋势。用实验组与对照组的突变率进行统计分析,紫露草4430^#在300×10^-6 相似文献
22.
江蓠原生质体分离和培养的初步研究 总被引:2,自引:0,他引:2
以江蓠Gracilariaverrucosa(Huds.)Papenfuss为材料,用微生物发酵法提取的琼胶酶成功地分离到江蓠的原生质体,经初步培养,原生质体发育为愈伤组织,为江芳江生物工程研究和育苗利用提供了可能。 相似文献
23.
结合地震、测井及微体古生物等资料,研究了珠江口盆地白云凹陷北斜坡区第四纪的沉积体系、层序地层及控制因素。研究区第四系发育以巨厚的高角度前积层为特征的大陆斜坡沉积体系,可将其划分为4个三级层序。层序的构成包括低位、海进及高位域,沉积体系包括下切谷、北东向单向迁移斜坡水道、陆架边缘三角洲、斜坡扇及高角度陆架边缘前积体系等。随着海平面下降及物源供应,三角洲体系推进至陆架坡折形成巨厚的陆架边缘三角洲和斜坡扇体系。更新世大陆斜坡沉积体系不断从番禺隆起向白云凹陷推进,陆架坡折带向海迁移;陆架区下切谷向上不断发育,在SB3和SB2界面上最密集;而冰后期至今的全新世高位三角洲被局限在内陆架地区。大陆斜坡沉积体系的演化主要受海平面变化、构造作用、气候变化以及沉积供给变化的共同控制。 相似文献
24.
The northeastern shelf margin of the South China Sea(SCS) is characterized by the development of large scale foresets complexes since Quaternary. Based on integral analysis of the seismic, well logging and paleontological data, successions since ~3.0 Ma can be defined as one composite sequence, consist of a set of regional transgressive to regressive sequences. They can be further divided into six 3 rd order sequences(SQ0–SQ5) based on the Exxon sequence stratigraphic model. Since ~1.6 Ma, five sets of deltaic systems characterized by development of wedge-shaped foresets complexes or clinoforms had been identified. High-resolution seismic data and the thick foresets allowed further divided of sub-depositional sequences(4 th order) of regression to transgression, which is basically consistent with published stacked benthic foram O-isotope records. Depositional systems identified in the study area include deltaic deposits(inner-shelf deltas and shelf-edge deltas), incised valleys, and slope slumping massive deposits. Since ~1.6 Ma, clinoforms prograded from the southern Panyu Lower Uplift toward the northern Baiyun Depression, shelf slope break migrated seaward, whereas the shelf edge of SQ0 migrated landward. The development of incised valleys in the continental shelf increased upward,especially intensive on the SB3 and SB2. The slumping massive deposits increased abruptly since SB2, which corresponds to the development of incised valleys. The evolution of depositional systems of continental slope mainly controlled by the combined influence of sea level changes, tectonic movements, sediment supply and climate changes. Since ~3.0 Ma, relative sea level of the northern SCS had been experienced transgression(~3.0 Ma BP) to regression(~1.6 Ma BP). The regional regression and maximum transgressions of the composite sequences were apparently enhanced by uplift or subsidence related to tectono-thermal events. In addition,climatic variations including monsoon intensification and the mid-Pleistocene transition may have enhanced sediment supply by increasing erosion rate and have an indispensable influence on the development of the incised valleys and 5 sets of deltaic systems since ~1.6 Ma. 相似文献
25.
在大洋环流模型中对应于惯性内波破碎的垂直混合的一个参数化方案 总被引:1,自引:0,他引:1
Based on the theoretical spectral model of inertial internal wave breaking(fine structure) proposed previously, in which the effects of the horizontal Coriolis frequency component f-tilde on a potential isopycnal are taken into account, a parameterization scheme of vertical mixing in the stably stratified interior below the surface mixed layer in the ocean general circulation model(OGCM) is put forward preliminarily in this paper. Besides turbulence, the impact of sub-mesoscale oceanic processes(including inertial internal wave breaking product) on oceanic interior mixing is emphasized. We suggest that adding the inertial internal wave breaking mixing scheme(F-scheme for short) put forward in this paper to the turbulence mixing scheme of Canuto et al.( T-scheme for short) in the OGCM, except the region from 15°S to 15°N. The numerical results of F-scheme by using WOA09 data and an OGCM(LICOM, LASG/IAP climate system ocean model) over the global ocean are given. A notable improvement in the simulation of salinity and temperature over the global ocean is attained by using T-scheme adding F-scheme, especially in the mid- and high-latitude regions in the simulation of the intermediate water and deep water. We conjecture that the inertial internal wave breaking mixing and inertial forcing of wind might be one of important mechanisms maintaining the ventilation process. The modeling strength of the Atlantic meridional overturning circulation(AMOC) by using T-scheme adding F-scheme may be more reasonable than that by using T-scheme alone, though the physical processes need to be further studied, and the overflow parameterization needs to be incorporated. A shortcoming in F-scheme is that in this paper the error of simulated salinity and temperature by using T-scheme adding F-scheme is larger than that by using T-scheme alone in the subsurface layer. 相似文献
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29.
依据在作者的前文(1998)中对于考虑旋转向量水平分量(f~)的大洋内波方程求出的渐近解,文中对S场(考虑f~条件下的总的内波场),SI场(不计f~影响的内波场)和SF场(S场中与f~相关联的部分)导出了能量谱和相干谱。此理论谱与Muler等(1978)的IWEX实验的观测结果相比较表明,SF场的水平动能谱和铅直位移谱基本上与水平流细结构和铅直位移细结构的观测谱一致。作者推测SF场对应于中纬度大洋可逆细结构。但是对于相干谱的观测结果,在不考虑内波非线性相互作用和破碎过程的条件下,仅考虑SF场的影响还不能给予满意的解释。 相似文献
30.
旋转向量水平分量对大洋内波方程的影响 总被引:7,自引:1,他引:7
在物理海洋学问题中,一般地采用固结在所研究海区中的直角笛卡尔坐标系(f-平面或β户平面近似),即原点在无扰动海面,z,y,x轴分别为向东、向北和向上. 相似文献