汶川8级地震前加卸载响应比的大尺度异常

孕震初期加卸载响应比(LURR)通常在1左右涨落,然后逐渐上升至峰值点。但强地震并不在峰值点上发生,而要滞后一段时间(T2)。T2与震级有关,震级越大,T2越长。对于8级地震,T2的计算值为28±8个月,汶川8级地震实际的T2是23个月。对于大地震,T2很长,峰值点后LURR通常迅速下降,在大地震前夕LURR常常降得很低,而预测的地震又迟迟没有发生,这种情况下很容易误导人们怀疑,甚至放弃原来的预测,殊不知,这时大地震正在迫近。这正是汶川8级地震给予人们血的教训。大地震不仅孕育时间长,孕震区面积也很大。大地震的前兆在时空上都是大尺度。基于这种认识,根据LURR的演化,中国大陆西南地区可能正在孕育一个特大地震。

农杆菌介导的双价抗盐基因转化番茄的研究

近年来，植物耐盐生物技术研究取得了可喜的进展，特别是通过抗盐基因转化在一定程度上使植物的耐盐性得到了提高。然而，植物的耐盐性是一个多基因控制的复杂性状，依赖于多个基因之间的相互作用。因此，只是将单个基因导入植物获得的抗逆性还是远不能达到满意的效果。一般认为，将多个与耐盐相关的基因转入到同一个植物（即所谓的“复合基因转化”）将会大大提高转基因植物的耐盐能力。 渗透调节是植物抵御盐胁迫的主要方式。植物渗透调节的方式分为两类：一是在细胞中吸收和积累无机盐，如通过离子通道、Na+/H+逆向运输蛋白和ATP酶/H+泵;二是在细胞中合成有机溶质，如脯氨酸和甘氨酸甜菜碱。 我们通过农杆菌介导法向转AtNHX1（拟南芥Na+/H+逆向运输蛋白编码基因）的番茄（Lycopersicum esculentum L. ‘Moneymaker’）株系X1OEA1自交二代植株（T2）中转入山菠菜甜菜碱醛脱氢酶基因（BADH）。PCR、Southern、RT-PCR和甜菜碱含量分析结果证明，BADH已经整合到目标植物基因组，并在转基因植株中转录和翻译表达。叶绿素荧光（Fv/Fm）、相对电导率（Rc/Rc’）、叶绿素含量（Chla+b）、叶绿素a/b比（Chla/b）和光合速率（Pn）测定结果表明，在200 mM NaCl 胁迫下，二次转化的番茄植株各项生理指标均优于转单基因AtNHX1的番茄。初步证明“复合基因转化”有助于进一步提高植物的耐盐性。同时对番茄的转化系统进行了优化，结果表明使用抗生素‘特美汀’作为抑制农杆菌的抗生素的转化效率明显高于使用头孢霉素。

水稻中一个编码富含脯氨酸蛋白基因家族的表达和功能研究

OsPRP1是水稻中特有的，编码一类富含脯氨酸蛋白（proline-rich protein, PRP）的基因家族，该家族有4个成员。在GenBank中，仅找到了一个结构相对接近的玉米PRP蛋白，但是对它的研究仅限于序列上的某些描述，而且在序列上，仍然与这4个OsPRP1蛋白有明显的差别。OsPRP1蛋白明显有别于前人（1999）所描述的4类PRP蛋白。它们是植物中一类新的小分子量的PRP蛋白，仅有一个保守结构域而属于DUF1210蛋白超家族的成员。 四个OsPRP1基因在基因组中紧密串联排列，而且编码区高度保守，基因结构也高度一致，证明它们来源于同一个祖先基因，是通过基因复制的方式产生的。PAML分析也证明它们在进化时间上的相互距离并不远。而在进化过程中由于执行生理功能上的某种重要性，在编码区表现出很的保守性，因而很难在RNA水平和蛋白水平上研究四个OsPRP1基因的表达差异。但是它们在表达调节区（如启动子区）显示出明显的差异。在克隆启动子的基础上，用GUS报告基因的策略，没有检测到它们在拟南芥中的表达活性，说明它们具有一定的种属特异性。而在水稻中，这四个基因的表达显示出了明显的时序和空间差异，既表现出在组织器官及其发育阶段上的特异性和变化，又在一定程度上表现出交叉，出现了功能上的分化和重叠。根据启动子区上的顺式元件，检测了这些基因对6种植物生长调节物质和3种非生物胁迫因子的应答反应，证明它们的表达调节也表现出显著的差异和分化。因此，四个基因的进化出现了功能退化、亚功能化和产生新功能等多种命运，比理论模型预期的要复杂得多，可能在执行生理功能和对环境反应上具有各自的生物学意义。 植物细胞壁是多种碳水化合物和蛋白质相互交织在一起的亲水性网络。在保护和支撑原生质、细胞通信、细胞分化、细胞对生物的和非生物胁迫的抗性等方面发挥着重要作用。目前已知的大多数植物PRP蛋白被描述成细胞壁结构性蛋白。OsPRP1基因家族编码的蛋白质都有一个N-端信号肽，暗示它们可能是一类分泌蛋白。我们用OsPRP1.1::GFP融合蛋白进行了亚细胞定位，证明了OsPRP1蛋白的确也是细胞壁相关蛋白。用原核表达体系表达了GST-融合蛋白，制备抗体，通过免疫印迹证明这些蛋白不溶于温和的提取缓冲溶液中，但可以被高盐和强碱溶液溶解，且分子量增加了三倍。证明在体内可能出现修饰、与细胞壁其它组分相交联的现象。 在这四个基因中，只有OsPRP1.2能够在水稻根中特异表达。根的原位杂交实验证明，OsPRP1在分化成熟程度低的细胞中大量表达，而在分化成熟程度高的细胞中几乎不表达。GUS染色的结果同样发现，基因在维管柱特别是中柱鞘附近的薄壁细胞的表达比别的细胞要强得多，而且在根的生长方向上表现出与发育相关的表达特征。说明OsPRP1基因可能参与了这些细胞的分化、发育过程。而基因表达的组织器官特异性的差异和对不同刺激因素的不同反应意味着它们可能参与了多种生理过程。为此构建了一个RNAi的表达载体，转化水稻，Southern杂交实验得到9个单位点插入的T2代独立株系，其中有6个株系与野生型对照相比，主根的早期伸长受到显著抑制，主根的一级侧根地数量减少，根尖分生区的细胞在轴向上的伸长受到了抑制。结合表达定位和原位杂交的结果，我们对它们在植物生长发育中的功能进行了深入探讨。

复苏植物牛耳草Boea hygrometrica耐旱复苏过程中LEA基因表达调控及功能研究

本实验室以复苏被子植物旋蒴苣苔（Boea hygrometrica (Bunge) R Br，牛耳草）为实验材料，利用cDNA微阵列技术，筛选到2个LEA蛋白的cDNA片段。它们在干旱条件下表达水平增加一倍以上。在上述基础上，通过5’-RACE的方法扩增得到这两个LEA基因的全长cDNA，BhLEA1和BhLEA2，发现二者编码蛋白均与玄参科复苏植物Craterostigma plantagineum中的第4组LEA蛋白pcCC2具有最高的同源性。PCR扩增得到的基因组序列中发现BhLEA1和BhLEA2在靠近5’端处各有一内含子，分别为97和171bp。利用tail-PCR和inverse-PCR扩增得到BhLEA2的1215bp的启动子序列，其中含ABRE、W-box、HDEs、MYB、MYC、和生长素响应元件等。两个基因在不同胁迫、激素等处理下都有诱导表达。构建过量表达载体, 转化烟草。筛选T2代的纯合体植株进行抗旱试验，测定了干旱过程中的土壤和叶片含水量，PSⅡ最大光化学效率Fv/Fm、SOD和POD酶的活性及蛋白质降解程度，发现BhLEA1和BhLEA2过量表达的烟草抗旱性有明显提高，与野生型相比，叶片含水量和光系统Ⅱ活性下降慢、SOD和POD活性增高、蛋白质降解减少。Western blot检测发现在干旱时，野生型烟草的RbcL、LHCⅡ和PsBO蛋白明显降解，而转基因植物的几乎没有降解，或者降解较少，说明BhLEA的过量表达可以在一定程度上抑制干旱诱导的蛋白质降解。这些结果表明，BhLEA基因可能直接或间接地在牛耳草干旱过程中参与了保护蛋白质的作用，为牛耳草叶片的复苏提供了基础。

嗜盐古菌启动子DNA片段的功能检测

将来源于嗜盐古菌染色体DNA的启动子片段RM07或RM13插入到启动子探针载体pYLZ_2的报告基因lacZ之前,通过β_半乳糖苷酶酶活性的检测,进一步确证RM07和RM13片段在大肠杆菌(Escherichia coli)中的启动功能。同时用微量热技术检测了大肠杆菌DH5α及其重组菌株在LB培养基中37℃生长过程的热输出功率。T2(pYLZ_2)、TE07(pYL726)、TE07_2(pYL702)、TE131(pYL131)和TE132(pYL132)菌株的生长速率分别比大肠杆菌DH5α降低了6.5

黄土高原沟壑区小麦品种演替过程中籽粒灌浆特性研究

为了解黄土高原沟壑区小麦品种演替过程中的籽粒灌浆特性,以此地区20世纪50年代至今的主栽小麦品种为供试材料,研究了不同小麦品种演替过程中籽粒干物质积累量及灌浆速率的变化。结果表明,黄土高原沟壑区小麦演替过程中,小麦籽粒千粒重呈现逐渐增加的趋势。平均灌浆速率逐渐增加,小麦籽粒的干物质积累随之增加,长旱58的W0最大,达50.53 g。灌浆三阶段中,各阶段的灌浆速率表现为,V2>V1>V3。从灌浆持续时间看,T1和T2持续的时间较长且变异系数较大,而T3和T相对稳定。从灌浆速率来看,V1、V2、V3、Vm、Va变异系数较大,灌浆速率易受环境因素影响而波动。

猴和人T淋巴细胞表面TRBC受体和E受体的比较研究

1985年贲昆龙等首次发现人和猴T淋巴细胞能与树鼩(Tupaia belangeri)的红细胞(TRBC)形成亲和力极强的玫瑰花结，它与绵羊红细胞(SRBC)玫瑰花结(E花结)明显不同。例如，TRBC经神经氨酸酶处理之后，结花率明显下降，TRBC与T淋巴细胞所形成的玫瑰花结，经45℃保温，仍不受影响，为了进一步探讨TRBC受体和SRBC受体(CD2)，以及与其它T细胞表面分化搞原(CD)的系。我用某些抗人T细胞CD的单克隆抗体(McAb)对人和猴淋巴细胞进行玫瑰花结抑制试验，抗原调变和共调变(Antigenic modulation or co-modulation)实验，并且研究了TRBC受体在其它免疫细胞和某些人类和长臂猿细胞系的分布。结果表明，TRBC与外周血E~+-PBL形成玫瑰花结的百分率为88.8%。而E~--PBL仅为4.16%。TRBC受体存在于所有被试T细胞系(CEM, H33JHJA1, Jurkat, MLA-144, Molt-3, Molt-4, Molt-4 clone-8 和PEER)，但不存在于外周血粒细胞，B细胞，以及B细胞系的绝大多数细胞表面(Daudi, Raji和Reh)。分布于全T细胞的CD3, TCR, CD5, CD6和CD7的相McAb OKT3, T108(F1), T136(F101-15), T149(M-T604)和T152(7G5)均不能调变和共调变TRBC受体。猴和人外周血淋巴细胞与TRBC玫瑰花结的形成，不被T11.1 McAb OKT11所阻断，相反，OKT11显著地阻断猴和人外周血淋巴细胞E玫瑰花结的形成，最大抑制率分别为49.3%和77.7%。在世界各地10个实验室送交第四次国际人白细胞化化抗原讨论会待鉴定的13个CD2 McAb中，除T089 (39C1.5)因抗体量不够未作实验外，对其他12种McAb都进行试验，T081 (x/3)，T082 (GLB-T11.2/1)，T083 (GLB-T11.1/1)，T085 (RPA-2.10)，T1088 (0-275)和T092 (M-T201)对TRBC玫瑰花结和E玫瑰花结都呈现明显的阻断作用，T084 (F110.08)，T091 (AICD2.1)以及已知参数CD2 McAb-T086 (D-66 clonel)和T087 (GT-2)都不阻TRBC玫瑰花结的形成，亦不调变TRBC受体，而对E玫瑰花结则有不同程度阻断效应，并且调变E变体，使E玫瑰花结形成细胞百分率下降。T090 (6F10.3)和T198 (JOR-T2)即不阻TRBC玫瑰花结的形成，也不抑制E玫瑰花结的形成。由此可见，TRBC受体分布于全T细胞，它不同于已知的全T细胞表面分化抗原CD2 (gp50), CD3/TCR复合物，CD5, CD6和CD7。CD2分子不与TRBC玫瑰花结的形成，也不是介导E玫瑰花结的唯一分子。至少有二个或三个以上的蛋白质与E玫瑰花结和TRBC玫瑰花结的形成有关，其中有的分子为E受体和TRBC受体所共有。TRBC受体很有可能包括新的T淋巴细胞分化抗原。

花椒水浸液及酚酸类化感物质对作物种子萌发和幼苗生长的影响效应

花椒（Zanthoxylum piperitum）是川西干旱河谷地区的重要经济作物，化感作用是花椒连作障碍的原因之一。系统研究花椒化感作用有助于深入理解并最终解决花椒连作障碍。本文通过研究花椒叶、林下土壤浸提液及单一纯化感物质对花椒幼苗生长、苜蓿种子萌发及幼苗生长的影响作用，从生理生化角度揭示浸提液及纯化感物质的作用方式。通过室外和室内模拟实验，对浸提液及纯化感物质的化感效应进行比较，为花椒连作障碍的解决和化感作用机制的深入理解提供依据。主要结果如下： 1.花椒叶及林下土壤浸提液对地下生物量影响作用强与对地上生物量的化感效应，两种浸提液的化感效应强度不同，叶浸提液作用表现更显著。其中在Y6、Y8 、T6和T8处理时，花椒幼苗地下生物量分别降低了31.2%、32.1%、31.6%和31.7%。 2.两种浸提液均能显著影响花椒幼苗体内的保护性酶活性，总体说来，在高浓度下抑制各种抗氧化物酶活性，幼苗体内丙二醛含量增加，幼苗受害严重；在较低浓度下，各种保护性酶活性有所增加，丙二醛含量减少，幼苗伤害减轻。同时，不同月份里，各种酶的活性高低显著不同，9月份的活性显著低于7月份的酶活性。对于养分含量的影响，Y8、T8的影响强度最大，分别使碳元素含量降低了27.8%和30.8%，使钾元素含量降低了34.7%和25.6%。 3.花椒叶及林下土壤浸提液对苜蓿种子萌发及幼苗生长有化感作用，表现在最终萌发率、不同物质代谢及保护性酶活性的差异上。两种浸提液对苜蓿种子萌发过程中蛋白质的含量均无显著性影响，对淀粉和可溶性糖的影响作用类似，高浓度处理无明显化感效应，较低浓度处理显著降低二者在萌发苜蓿种子中的含量。Y2、Y4与T4处理分别使可溶性糖含量减少了32.3%、29.1%和18.8%，Y2与T2处理分别使淀粉含量降低了29.3%和26.8%。 4.苜蓿种子在4种单一化感物质最高浓度即10-3 mol•L-1处理下，萌发率显著降低，半数萌发时间推迟，随着处理浓度降低，抑制作用逐渐减弱，当降低到10-6 mol•L-1时，又能够表现出对苜蓿种子萌发的促进作用。 5.纯化感物质在10-6 mol•L-1时使苜蓿幼苗叶片的保护性酶活性显著升高，丙二醛含量显著降低；在10-3 mol•L-1时使苜蓿叶片中保护性酶活性显著降低，丙二醛含量增加，膜脂过氧化程度加重。 Zanthoxylum piperitum is one of the most important cash crops and has been extensively cultivated in Eastern Tibetan Plateau, especially in the fragile dry valley areas. Allelopathic effects could be a reason for Z. piperitum’s continuous cropping impediment. Systemmatically research of the effect of Z. piperitum allelopathy could help to comprehend the continuous cropping impediment. The allelopathic effects on seedlings growth and seed germination of aqueous extracts of Zanthoxylum piperitum and phenolic allelochemicals were studied, and the action mechanism of the two substances was also discussed from physiology. Indoor and outdoor experiments were set to compare the difference between aqueous extracts and pure allelochemicals. The main results showed that: 1. The aqueous extracts of leaf and soil had significant allelopathic effects on aboveground and underground biomass, but the effect on underground biomass was stronger than the effect on underground evidently. Treated with Y6、Y8 、T6 and T8, the underground biomass was reduced 31.2%、32.1%、31.6% and 31.7% respectively. 2. The activity of activities of superoxide dismutase, catalase, peroxidase and ascorbate peroxidase were significantly reduced, while the content of MDA was increased and the seedlings were suffered stronger, when treated by the high concentration; but at the low concentration, these were reversed. And then, at the different month, the activities of antioxidant enzyme were significantly distinct. As for the contents of nutrient element, Y8、T8 had the more intensive effects than other treatments. 3. The results showed that the two types of aqueous extracts had significant allelopathic effects on seed germination, substances metabolize and the activity of antioxidant enzyme. But the aqueous extracts had no effects on the content of protein, while had the similar effects on the content of starch and soluble sugar. At Y2、Y4 and T4, the content of soluble sugar decreased 32.3%、29.1% and 18.8% respectively. 4. Treated with 10-3 mol•L-1 of the four allelochemicals, the seed germination of alfalfa was significantly inhibited. Ferulic acid, coumarin and vanillic acid at 10-3 mol•L-1 significantly reduced the activities of antioxidant enzyme, while the content of MDA in alfalfa seedling was significantly increased. The restrain effects became weakened with the treat concentration falled. However, ferulic acid, coumarin and vanillic acid could increase the activities of antioxidant enzyme at 10-6mol•L-1.

低能O~(3+)与H_2碰撞电子俘获过程中靶的同位素效应研究

利用全量子的分子轨道强耦合方法,我们研究了基态的O3+(2s22p2P)与氚分子和氢分子碰撞的电荷转移过程,计算了方位角为45°,能量分别为0.1eV/u,1.0eV/u,100eV/u,500eV/u的单电子俘获的振动分辨的态选择截面及总截面.分子轨道强耦合计算中采用了自旋耦合价带理论计算的三原子分子势能面和径向耦合矩阵元.对体系的电子运动同H2(T2)或H2+(T2+)的转动和振动之间的耦合,根据能量的不同,分别采用了无限阶的冲量近似或振动冲量近似.结果发现,低能O3+与H2碰撞电子俘获过程中靶的同位素效应显著:对不同的同位素靶,单电子俘获的总截面以及振动分辨态选择截面的分布明显不同;入射离子能量越低,同位素效应越显著.

17F和18Ne与质子弹性散射研究

论文讲述了采用逆运动学方法用放射性核束~(17)F和~(18)Ne与质子弹性散射的实验准备、设汁方法、实验情况、实验数据处理过程、理论分析处理和得到的结果。弹性散射测量核敞射的角分布，对位置探测器有很高的要求。在实验的准备阶段，为了对放射性核束的准确定位，研制了位置分辨为lITlm的高位团置分辨的PPAC。山于质予的穿透能力很强，在半导体硅探测器中的能损很小，实验前，刘。测量反冲质子的探测器PSSD在低能量沉积下的工作情况进行了测试，满足质f位置和I能量测量的要求。实验采用初级束流强度约为80nA能量为45Mev／A的~(20)Ne轰击lmm厚的~9Be，反应产物经过500μm厚的Wedge~(27)Al，通过次级束流线的筛选，得到~(17)F和~(18)Ne和少量的~(16)O束流，其能量分别为17.7Mev／A、16.1Mev／A和14.3Mev／A。然后轰击60μm厚的(CH_2)_n靶。用次级束流线装置的两个焦点处的塑料闪烁体测量放射性核束的时间Tl和T2，根据飞行时间差在相同的磁场条件下来鉴别粒子和得到放射性核束的能量。用靶前的两个PPAC和靶后的一个PPAC来确定放射性核束的入射方向、反应点和出射方向，反冲质子的位置由分布于各实验室系角区的五个PSSD来测定。实验数据处理时，根据放射性核束经过基本相同的飞行路径和磁场条件，用T1和T2测到的飞行时间差来确定放射性核束的能量。将入射到PPAC上的弹核粒子位置，经对宏观几何位置矫正后，来确定弹核粒子的入射方向、反应点位置和出射方向。将PSSD测量到的位置谱经与沉积能量相关的修正因子对位置修正后，确定反冲核在PSSD上的几何位置点，跟PPAC测量确定的靶上的反应点位置结合，确定反冲核的出射方向。测量得到的位置经过空间关系换算，由测量到的弹核入射方向、反应点位置和反冲核出射方向，得到弹性散射的实验室系散射角。累计所有测到的事件得到初始的反冲核实验测量角分布。采用逐个事件的方法，用一事先产生的一系列点组成的数据库模拟探测器边界，事件的几何探测效率进行归一化，得到实际的实验室系散射角分布。用弹核出射角度随反冲核的出射角度的运动学关系鉴别来自靶中的H和C的散射事件。将实验室系角分布转换到质心系下后，再根据弹核粒子数、单位面积靶核数和测量到的事件数，得到实验测量的质的弹性散射微分截面。实验得到的微分截面数据采用零程相互作用的扭曲波玻恩近似理论计算程序DWUCK4序进行光学势拟合计算，选用较准确描述奇异核性质的CH89参数化的光学势为初始的光学势参数，对光学势参数的组成成分进行敏感性分析后，确定参数搜索的顺序，用跟各参数相关联的自动参数搜索程序ABOD进行分析处理。进行光学模型的理论拟合计算时，将计算结果和实验值进行比较，拟合实验数据，求得光学势参数。参数拟合佳度用残差平方和检验(χ~2检验)。得到~(17)F和~(18)Ne与质子弹性散射的光学势参数。根据得到的光学势参数进行折叠模型分析。得到了，1)~(17)F和~(18)Ne实势相互作用均方根半径分别为，_(rF)~(1/2) = 3．239(fm)，_(r_Ne)~(1/2) = 3.317 (fm)。跟相对论平均场计算结果比较分析表明，~(17)F的核物质半径为2.95±0.03fm，~(18)Ne的核物质半径为3.07±0.03fm,~(17)F和~(18)Ne表面的密度要比相对论平均场理论预言的值要大。2)~(17)F和~(18)Ne的自旋轨道耦合相互作用主要作用于核表面区域，这是因为位于核外层的价质子的影响。

HIRFL剥离器后切束线物理设计

HIRFL is a tandem cyclotron complex for heavy ion. On the beam line between SFC and SSC, there is a stripper. Behind it, the distribution of charge states of beam is a Gauss distribution. The equilibrium charge state Q_0 is selected by 1BO2(a 50° dipole behind the stripper) and delivered to SSC. One of two new small beam line (named SLAS) after 1B02 will be builded in or der to split and deliver the unused ions of charge states (Q_0 ± n) to aspecific experimental area. Q_0 ± n ions are septumed and separated from initial(Q_0) ion beam by two septum magnets SM1, SM2. The charge state selected by SM1 will be Q_0 ± 1(6 ≤ Q_0 < 17), Q_0 ± 2(17 ≤ Q_0 < 33) and Q_0 ± 3 (Q_0 ≥ 33) forming a beam in one of the two possine new beam line with the stripping energy of (0.2 to 9.83 Mev/A), an emittance of 10π mm.mrad in the two transverse planes and an intensity ranging from 10~(11) pps for z ≤ 10 to some 10~5 pps for the heaviest element. Behind SM2, a few transport elements (three dipoles and seven qudrupoles) tra nsport Q_0 ± n beam to target positions T1, T2 (see fig. 1) and generate small beam spots (φ ≤ 4mm, φ ≤ 6mm). The optics design of the beam line has been done based on SLAC-75 (a first and second - order matrix theory). beam optics calculation has been worked out with the TRANSPORT program. The design is a very economical thinking, because without building a new accelerator we can obtain a lower energy heavy ion beam to provide for a lot of atomic and solid state physical experiments

黄土丘陵区典型植物群落根系垂直分布与环境因子的关系

深入研究植被恢复过程中根系与环境因子的响应规律,对于当前西部地区的生态环境建设中有关林草措施的配置问题具有重要理论意义和实践价值。采用对应分析(CA)和典范对应分析(CCA)方法研究黄土丘陵区4种典型植物群落的根系垂直分布特征及其与环境因子的关系。结果表明,所选群落的根系生物量随土层深度增加而明显减小,0~40 cm土层根系生物量超过总根量的85%。借助CA分析将根系的垂直分布特征分为T1、T2和T3,其中大多数群落属于T1型,即表层根量聚积型,0~20 cm土层根量远高于其他层次;T2和T3型为深根与浅根型根系的组合类型,层次变化相对缓和。群落根系的垂直分布及变化受环境因子的综合影响,T1型分布在硝态氮含量较高且有机质和全氮含量较低的地段;T2和T3型的有机质和全氮含量较高,硝态氮含量较低;土壤水分含量、密度、硝态氮是影响退耕地典型植物群落根系垂直分布特征的主要环境因子。

气候变暖对高寒草甸气候生产潜力的影响

利用多年定位测定的草地生产力资料及同步气象因素观测数据, 建立现实状况下光、温、水影响草地气候生产潜力模型: 　　Y= F1 (Q ) ·F2 (T ) ·F3 (P) 　　 = K ∑[(-b·exp (a+ b∑t/∑tmax) )/(1+ exp (a+ b∑t/∑tmax) )2 ] 0　　　　　　　　　　　T < 0℃ ·[W 0/∑tmax ]·△∑t· Tö2 0·016658　　　0℃≤T< 20℃ 1　　　　　　　　　　　T ≥20℃ 在分析现实高寒草旬气候生产力分布与环境条件关系的同时, 根据该模型模拟计算未来气温升高2℃和4℃, 降水增加10% 和20% 状况下的气候生产力情景。在上述两种气候情景下, 未来草地生产力分别出现降低(10% ) 和升高(1% ) 的两种可能。气候变暖在一定程度上减少和缓和低温对高寒草甸牧草生长的不利影响, 但地表及植被的蒸散量的加大远比降水增加的快, 水分则成为牧草生长的限制因素。

四川盆地构造控藏规律研究

Firstly, established sequence stratigraphy of Sinian System-Middle Triassic Series framework in Sichuan basin,be divided into 21 second-level sequence stratigraphy and 105 third-level sequence stratigraphy.From many aspects,discussed sequence stratigraphy characteristic. On the foundation of structure unconformity and fission track analysis, on the ground of An county-Shuinin county regional seismic section, using the positive evolution equilibrium principle technology, comprehensivly be mapped structure evolution of Sichuan basin. It can be divided into seven stages, that is :Pre-Sinian basement stage, cratonic depression basin(Z1-S)stage, cratonic rifted basin(D-T2)stage, passive continental margin(T3x1-3)stage, foreland basin(T3x4-6)stage, depression basin (Jurassic Period-Miocene Epoch) stage, formed basin (Holocene Epoch) stage. Analysis on structure evolution history,burial history,source rocks thermal evolution history, Maoba changxing formation gas pool forming process can be classified into four stages: ancient lithological oil pool stages in Indosinian-early Yanshanian period（T-J1-2）, ancient structure- lithological gas pool stages in middle Yanshanian period（J3-K1）, structure- lithological gas pool setting stages in last Yanshanian period（K2）, structure- lithological gas pool adjusting and transformation stages in Himalayan period（R-Q）. Maoba feixianguan formation gas pool forming process can be classified into two stages: second structure gas pool stages in last Yanshanian period（K2）,second structure gas pool physical adjusting and transformation stages in Himalayan period（R-Q）,and summarize reservoir formation model. On the base of newest exploration achievement and petroleum geologic comprehensive research , demonstrate how structure controls hydrocarbon accumulation. Structure controlling source rocks behaves structure controlling main source rocks’sedimentary facies, medium-large pools mainly located at center or margin of hydrocarbon generation. Structure controlling palaeo-karst reservoirs ,reef and beach facies reservoirs, fault and fracture reservoirs. Structure controlling palaeo-uplift, and palaeo-uplift controlling hydrocarbon migration, active reservoirs’forming, palaeo-structure traps forming. Structure controls distribution of mudstone and gypsolith, controls preservation. Structure controls hydrocarbon conducting, structure traps forming and hydrocarbon accumulation. Whether or no, Structure controls total process of basin forming-source rocks’generation- hydrocarbon accumulation. It is direct effect results of structure movements that large traps’ conditions, conducting migration conditions, high quality preservation. source rocks’condition and reservoirs’ condition are the indirect effect results. In the last analysis, “source rock controlling theory”, “high quality reservoir mainly controlling theory”, “palaeo-uplift controlling theory” and “current structure deciding theory” are structure controlling hydrocarbon accumulation. There are high variability and complex mechanisms in Sichuan basin , but the regional hydrocarbon accumulation conditions are very well, such as abundant source rocks, matching process of hydrocarbon accumulation and many exploration areas. By means of integrated analysis, put forward hydrocarbon exploration direction and large-middle targets of China Petroleum and Chemical Corporation .Thus, more and more hydrocarbon proved reserve and output in Sichuan basin will be contributed to China energy industry in a long future time.

下扬子北缘前陆盆地形成演化与油气赋存条件

The foreland basin on the northern margin of the lower reach of the Yangtze river (the lower Yangtze foreland basin) is tectonically situated in the basin-mountain transitional area along the southeastern flank of the Dabie mountains. The early formation and development of the basin is closely related to the open-up of the Mian-Lue paleo-oceanic basin on the southern margin of the Central Orogenic System represented by Qinling-Dabei orogenic belt, while the tectonic evolution of the middle-late stage of the basin is mainly related to development of the Mian-Lue tectonic zone that occurred on the basis of the previous Mian-Lue paleo-suture. The foreland basin of the northern rim of the lower reach of the Yangtze river was formed during the middle-Triassic collision between the Yangtze and North China plates and experienced an evolution of occuirence-development-extinction characterized by marine facies to continental facies and continental margin to intracontinent in terms of tectonic setting.The foreland basin (T2-J2) was developed on the basis of the passive continental marginal basin on the south side of the Mian-Lue paleo-ocean and superimposed by late Jurassic-Tertiary fault basin. The tectonic setting underwent a multiple transformation of rifting-collisional clososing-tensional faulting and depression, which resulted in changes of the property for the basin and the final formation of the superposed compose basin in a fashion of 3-story-building. According to the tectonic position and evolution stages of plate collision happening on the southeastern margin of the Dabie mountains, and tectono-tratigraphic features shown by the foreland basin in its main formational period, the evolution of the foreland basin can be divided into four stages: 1) pre-orogenic passive margin (P2-Ti). As the Mian-Lue ocean commenced subduction in the late-Permian, the approaching of the Yangtze and North China plates to each other led to long-periodical and large-scale marine regression in early Triassic which was 22 Ma earlier than the global one and generated I-type mixed strata of the clastic rocks and carbonate, and I-type carbonate platform. These represent the passive stratigraphy formed before formation of the foreland basin. 2) Foreland basin on continental margin during main orogenic episode (T2.3). The stage includes the sub-stage of marine foreland basin (T2X remain basin), which formed I-type stratigrphy of carbonate tidal flat-lagoon, the sub-stage of marine-continental transition-molasse showing II-type stratigraphy of marine-continental facies lake - continental facies lake. 3) Intracontinental foreland basin during intracontinental orogeny (Ji-2)- It is characterized by continental facies coal-bearing molasses. 4) Tensional fault and depression during post-orogeny (J3-E). It formed tectono-stratigraphy post formation of the foreland basin, marking the end of the foreland evolution. Fold-thrust deformation of the lower Yangtze foreland basin mainly happened in late middle-Jurassic, forming ramp structures along the Yangtze river that display thrusting, with deformation strength weakening toward the river from both the Dabie mountains and the Jiangnan rise. This exhibits as three zones in a pattern of thick-skinned structure involved the basement of the orogenic belt to decollement thin-skinned structure of fold-thrust from north to south: thrust zone of foreland basin on northern rim of the lower reach of the Yangtze river, foreland basin zone and Jiannan compose uplift zone. Due to the superposed tensional deformation on the earlier compressional deformation, the structural geometric stratification has occurred vertically: the upper part exhibits late tensional deformation, the middle portion is characterized by ramp fault -fold deformation on the base of the Silurian decollement and weak deformation in the lower portion consisting of Silurian and Neo-Proterozoic separated by the two decollements. These portions constitutes a three-layered structural assemblage in a 3-D geometric model.From the succession of the lower reach of the Yangtze river and combined with characteristics of hydrocarbon-bearing rocks and oil-gas system, it can be seen that the succession of the continental facies foreland basin overlies the marine facies stratigraphy on the passive continental margin, which formed upper continental facies and lower marine facies hydrocarbon-bearing rock system and oil-gas forming system possessing the basic conditions for oil-gas occurrence. Among the conditions, the key for oil-gas accumulation is development and preservation of the marine hydrocarbon-bearing rocks underlying the foreland basin. The synthetic study that in the lower Yangtze foreland basin (including the Wangjiang-Qianshan basin), the generation-reservoir-cover association with the Permian marine facies hydrocarbon-bearing rocks as the critical portion can be a prospective oil-gas accumulation.Therefore, it should aim at the upper Paleozoic marine hydrocarbon-bearing rock system and oil-gas forming system in oil-gas evaluation and exploration. Also, fining excellent reservoir phase and well-preserved oil-gas accumulation units is extremely important for a breakthrough in oil-gas exploration.