白杄花粉管胞吞/胞吐动态及其与细胞壁构建的关系

在有花植物受精过程中，具有顶端极性生长特性的花粉管是雄性生殖单位的载体，同时也是研究细胞生长分子调控机理的理想体系。与被子植物相比，裸子植物花粉具有萌发时间长、花粉管生长缓慢等特点。对于裸子植物花粉萌发和花粉管生长的机理，目前人们尚不十分清楚。本文将以裸子植物白杄（Picea meyeri）花粉为材料，应用不同浓度的分泌系统干扰剂Brefeldin A处理，并通过细胞学和生理生化方法，其中包括普通光学显微镜、荧光显微镜、激光扫描共聚焦显微镜、显微红外光谱（FTIR）和透射电镜（TEM）等技术，对其花粉萌发和花粉管生长过程中胞吞胞吐的调控，以及与细胞壁建成的关系等进行较为系统的研究，旨在为进一步揭示裸子植物花粉管发育的调控机理提供参考。 首先比较观察了各种细胞器在白杄与被子植物花粉管中的分布差异。经FM4-64探针标记结果表明，在正常生长的白杄花粉管顶端存在分泌小泡积累的透明区，但与被子植物比较起来，此透明区在花粉管中所占比例较小，且不呈倒“V”字型。在透射电镜下观察发现，其花粉管顶端透明区内分泌小泡的分布密度远低于被子植物。另外，在白杄花粉管中，线粒体的分布一般靠近细胞壁的地方，高尔基体分布较为分散，而内质网的分布则不具方向性。 其次，研究了BFA对白杄花粉萌发和花粉管生长的影响，特别是对其花粉管生长过程中的胞吐/胞吞作用。通常在正常生长的白杄花粉管中，用FM4-64标记后发现，在其顶端形成与透明区对应的荧光亮区;超微结构显示，在花粉管顶端进行旺盛的胞吐作用，许多分泌小泡正与质膜融合，以及分布有大量显示高分泌活性的壁旁体（PB）等。而经过BFA处理后，花粉的萌发和花粉管的生长均受到严重抑制，花粉管出现了弯曲（波状生长）或顶端膨大等异常形态，同时还干扰了FM4-64在花粉管顶端的标记模式。另外，花粉管顶端分泌小泡数量减少，透明区内充满线粒体、高尔基体和空泡等一些大的细胞器，壁旁体也随之消失，其中高尔基体呈现解体或弯曲的异常形态，在其周围的分泌小泡数量大大减少，内质网出现膨胀和核糖体脱落等;同时胞吐活性标志性酶——酸性磷酸酶的活性也随之降低。通过对FM4-64的染料吸收实验表明，BFA对胞吞有明显的促进作用。由上可见，BFA对白杄花粉管生长过程中的胞吐和胞吞作用起了相反的影响， BFA正是通过扰乱花粉管生长过程中的分泌途径来抑制其花粉管的生长。 最后，检测了白杄花粉管分泌途径紊乱后，管壁物质合成的变化情况。通过FTIR光谱分析表明，BFA处理后花粉管壁化学组分发生了变化，例如蛋白质和多糖含量明显减少，而且与蛋白比较起来，多糖的含量下降更为明显，尤其是在顶端。蛋白和多糖含量的下降导致花粉管壁的组成结构不够致密。由SDS-PAGE的结果显示， BFA抑制后，花粉管壁中糖蛋白的含量下降了60%，同时很多壁蛋白条带在BFA处理后不表达或含量减少。通过对花粉管壁多糖成分的研究表明，BFA处理还导致纤维素含量下降，而胼胝质在花粉管顶端积累。用识别AGPs的LM6和识别酸性果胶的JIM5对花粉管进行标记，发现BFA处理后AGPs的环状分布消失，酸性果胶质在顶端的含量也明显减少，但在胞质内却形成一些小的分隔亮点（compartments）。 综上所述，导致裸子植物白杄花粉管生长缓慢的原因，可能与其顶端透明区较小、分泌小泡数量少等有关。另外，从白杄花粉管的细胞质状态和细胞器分布上看，虽然与被子植物相比差异较大，但在其正常生长中仍能进行旺盛地胞吐和胞吞过程。经BFA处理后引起花粉管内分泌系统的紊乱，致使管壁物质不能正常合成，从而导致花粉管的停滞生长。

施肥对干旱胁迫下夏玉米根系提水的调节作用研究

以耐旱性玉米品种郑单958号为材料,采用两室分根土培装置,通过时域反射计(TDR)对上下土层土壤含水量进行控制和观测,研究施肥对干旱胁迫条件下玉米根系提水作用的影响.结果表明,玉米根系在土层上干下湿条件下(即上下层土壤存在一定水势差时)存在明显提水作用;玉米根系提水量在整个生育期呈单峰变化,并以吐丝期最大;上层土壤施肥可以调节玉米根系提水作用强弱,整个生育期根系总提水量表现为NP配施>单施P>CK>单施N,NP配施处理全生育期单株提水量(1 948.6 g)分别是单施P处理、CK和单施N处理的1.5倍、3.1倍和3.5倍.玉米整个生育期根系总提水量与收获期不同层次根系干重和体积存在极显著正相关关系,也与其地上部分生物量和籽粒产量呈极显著或显著正相关关系.可见,玉米根系的提水作用强弱因生育期和施肥处理而变化,施肥主要通过影响根系生长来调节其提水作用;在一定水分环境条件下,玉米根系提水作用能促进作物生长,提高其籽粒产量.

A stable carbon isotopic approach for understanding the CO2 flux at the Haibei Alpine Meadow Ecosystem - A simple model

Although respiration of organisms and biomass as well as fossil fuel burning industrial production are identified as the major sources, the CO2 flux is still unclear due to the lack of proper measurements. A mass-balance approach that exploits differences in the carbon isotopic signature (delta(13)C) of CO2 Sources and sinks was introduced and may provide a means of reducing uncertainties in the atmospheric budget. delta(13)C measurements of atmospheric CO2 yielded an average of - 10.3 parts per thousand relative to the Peedee Belemnite standard; soil and plants had a narrow range from -25.09 parts per thousand to -26.51 parts per thousand and averaged at -25.80 parts per thousand. Based on the fact of steady fractionation and enrichment during respiration of mitochondria, we obtained the emission Of CO2 of 35.451 mol m(-2) a(-1) and CO2 flux of 0.2149 mu mol m(-2) s(-)1. The positive CO2 flux indicated the Haibei Alpine Meadow Ecosystem a source rather than a sink. The mass-balance model can be applied for other ecosystem even global carbon cycles because it neglects the complicated process of carbon metabolism, however just focuses on stable carbon isotopic compositions in any of compartments of carbon sources and sinks. (C) 2005 Elsevier B.V. All rights reserved.

松辽盆地南部大情字井地区CO2埋存体地质格架及储层建模

Increasing attentions have been paid to the subsurface geological storage for CO2 in view of the huge storage capacity of subsurface reservoirs. The basic requirement for subsurface CO2 storage is that the CO2 should be sequestrated as supercritical fluids (physical trapping), which may also interact with ambient reservoir rocks and formation waters, forming new minerals (chemical trapping). In order to the effective, durable and safe storage for CO2, enough storage space and stable sealing caprock with strong sealing capacity are necessitated, in an appropriate geological framework. Up till now, hydrocarbon reservoirs are to the most valid and appropriate CO2 storage container, which is well proven as the favorable compartment with huge storage capacity and sealing condition. The thesis focuses on two principal issues related to the storage and sealing capacity of storage compartment for the Qingshankou and Yaojia formations in the Daqingzijing block, Southern Songliao Basin, which was selected as the pilot well site for CO2-EOR storage. In the operation area, three facies, including deltaic plain, deltaic front and subdeep-deep lake facies associations, are recognized, in which 11 subfacies such as subaqueous distributary channel, river- mouth bar, interdistributary bay, sheet sandbody, crevasse splay and overflooding plain are further identified. These subfacies are the basic genetic units in the reservoir and sealing rocks. These facies further comprise the retrogradational and progradational depositional cycles, which were formed base- level rise and fall, respectively. During the regressive or lake lowstand stage, various sands including some turbidites and fans occurred mostly at the bottom of the hinged slope. During the progradation stage, these sands became smaller in size and episodically stepped backwards upon the slope, with greatly expanded and deeped lake. However, most of Cretaceous strata in the study area, localized in the basin centre under this stage, are mainly composed of grey or grizzly siltstones and grey or dark grey mudstones intercalated with minor fine sandstones and purple mudstones. On the base of borehole and core data, these siltstones are widespread, thin from 10 to 50 m thick, good grain sorting, and have relative mature sedimentary structures with graded bedding and cross- lamination or crossbeds such as ripples, which reflect strong hydrodynamic causes. Due to late diagenesis, pores are not widespread in the reservoirs, especially the first member of Qingshankou formation. There are two types of pores: primary pore and secondary cores. The primary pores include intergranular pores and micropores, and the secondary pores include emposieus and fracture pores. Throat channels related to pores is also small and the radius of throat in the first, second and third member of Qingshankou formation is only 0.757 μm, 0.802 μm and 0.631 μm respectively. In addition, based on analyzing the probability plot according to frequency of occurrence of porosity and permeability, they appear single- peaked distribution, which reflects strong hetero- geneity. All these facts indicate that the conditions of physical property of reservoirs are not better. One reason may be provided to interpret this question is that physical property of reservoirs in the study area is strong controlled by the depositional microfacies. From the statistics, the average porosity and permeability of microfacies such as subaqueous distributary channel, channel mouth bar, turbidites, is more than 9 percent and 1md respectively. On the contrary, the average porosity and permeability of microfacies including sand sheet, flagstone and crevasse splay are less than 9 percent and 0.2md respectively. Basically, different hydrodynamic environment under different microfacies can decide different physical property. According to the reservoir models of the first member of Qingshankou formation in the No. well Hei47 block, the character of sedimentary according to the facies models is accord to regional disposition evolution. Meantime, the parameter models of physical property of reservoir indicate that low porosity and low permeability reservoirs widespread widely in the study area, but the sand reservoirs located in the channels are better than other places and they are the main sand reservoirs. The distribution and sealing ability of fault- fractures and caprock are the key aspects to evaluate the stable conditions of compartments to store CO2 in the study area. Based on the core observation, the fractures widespread in the study area, especially around the wells, and most of them are located in the first and second member of Qingshankou formation, almost very few in the third member of Qingshankou formation and Yaojia formation instead. In addition, analyzing the sealing ability of eleven faults in the three-dimensional area in the study area demonstrates that most of faults have strong sealing ability, especially in the No. well Hei56 and Qing90-27. To some extent, the sealing ability of faults in the No. well Hei49, Qing4-6 and Qing84-29 are worse than others. Besides, the deposition environment of most of formations in the study area belongs to moderately deep and deep lake facies, which undoubtedly take advantage to caprocks composed of mudstones widespread and large scale under this deposition environment. In the study area, these mudstones distribute widely in the third member of Qingshankou formation, Yaojia and Nenjiang formation. The effective thickness of mudstone is nearly ~550m on an average with few or simple faults and fractures. In addition, there are many reservoir beds with widely- developed insulated interbeds consist of mudstones or silty mudstone, which can be the valid barrier to CO2 upper movement or leakage through diffusion, dispersion and convection. Above all, the closed thick mud caprock with underdeveloped fractures and reservoir beds can be taken regard as the favorable caprocks to provide stable conditions to avoid CO2 leakage.

博兴洼陷西部砂体成因与油气成藏研究

Based on achievements of thirty years of hydrocarbon exploration, this paper uses the modern theories and methods of sedimentology and oil accumulation to study the origin and distribution features of four sandbodies of Gaoqing, Fanjia, Zhenglizhuang and Jinjia from the third member to the lower second member of Shahejie Formation in detail. Various geophysical methods are also used to explain and to predict the spatial distribution of sandbodies, which further shows mechanism and the model of oil accumulation and illuminates the disciplinarians of oil enrichment and its controlling factors in the study area. The most favourable oil pools predicted by this paper have significant economic and social benefits, which has been confirmed by the exploration. The main conclusions and knowledge includes: (1) Resolving the problems, which remain unresolvable for a long time in the western area of Boxing depression, about the original environment and the spatial distribution of sandbodies of Gaoqing, Fanjia, Zhenglizhuang and Jinjia, and illuminating their relationships. It is suggested that two deltas or delta-related sandbody sediments, which include the delta sandbodies of Jinjia and Gaoqing and their frontal turbidite fan sandbody, are developed in the second and third members of Shahejie Formation. The sandbodies of Fanjia, Gaoqing and Zhenglizhuang are components of Gaoqing delta and belong to the sediments of various periods in different part of the delta. Whereas, the sandbody of Jinjia belong to the Jinjia delta or fan-delta created by the uplift of the Western Shandong and in some areas shows the features of juxtaposition, superimposed deposition and fingeration with the sandbodies of Gaoqing and Zhenglizhuang. (2)Proposing that the sandbodies of different origins in the deltas of Gaoqing and Jinjia have obvious different reservoir qualities, among which the delta frontal bedded sandbodies in the second member of Shahejie Formation in Zhenglizhuang are the best ones and the turbidite sandbody of Fanjia is relatively worse. This shows the direction of further reservoir prediction. (3) According to modern petroleum system theory and continental pool-formation theory, the author divided the western area of Boxing depression into the Jinjia—Zhenglizhuang—Fanjia nose structure belt pool-formation system and the Gaoqing fracture belt pool-formation system. The study area is predominantly located in the former belt and subdivided into pool-formation sub-systems of Zhenglizhuang-Fanjia and Jinjia, which have the source rock of mudstone and oil shale from the upper forth member and the third member of Shahejie Formation in Boxing depression. The hydrocarbon migration and accumulation are controlled by Jinjia-Zhenglizhuang-fanjia nose structure and Gaoqing fracture. (4)Proposing that compared with the best developed sandbodies and traps in the west area of Boxing, the source from the Boxing depression is not sufficient, which is the fundamental reason that the hydrocarbon resources in mid-west area is less than in the east of Boxing. (5) Under the direction of the new theory (fluid compartments theory) and new method of modern pool-formation mechanism, two kinds of pool-formation model are established in study, i.e. inner-compartment model and outer-compartment model. The former has abnormal pressure and is the antigenic source seal pool-forming mechanism, whereas the latter has normal pressure and is of the allochthonous source opening pool-formation mechanism. (6)The study shows that the four sandbodies of Gaoqing, Fanjia, Jinjia and Zhenglizhuang sand are all very benefit for pool-formation, among which the Fanjia sandbody is the best favourable one and is likely to form lithological reservoir and fault-lithological reservoir. But the main step of exploration in Gaoqing, Zhenglizhuang sandbodies should be finding out the fault block, reversed roof and stratum-lithological oil reservoir. (7)Established a set of guidelines and techniques for the research and exploration in the large scale of sandbodies. Proposing that the various traps related to reversed fault and basin-ward fault should be found in step slopes and gentle slopes respectively, and the lithological oil reservoir should mainly be found in the sandstone updip pinch out. It is also suggested that Fanjia sandbody is most favourable to form the lithological and fault-lithological and the Gaoqing, Zhenglizhuang and Jinjia sandbodies have the potential of forming fault block, reversed roof and stratum-lithological oil reservoir. (8) Interpretation and prediction the spatial distribution of main sandbodies based on various geophysical methods suggestion that Fanxi, Gao28 south and Gao27 east have better exploration potential.