济阳-昌潍坳陷火成岩油气藏体系形成机理和分布规律研究

Jiyang & Changwei depressions are two neighboring depressions in Bahai Bay Basin, the famous oil rich basin in East China. The exploration activities in the past 40 years has proved that, within the basins, there exists not only plentiful sandstone hydrocarbon reservoirs (conventional), but also abundant special reservoirs as igneous rock, mudstone and conglomerate ones which have been knowing as the unconventional in the past, and with the prospecting activity is getting more and more detailed, the unconventional reservoirs are also getting more and more important for further resources, among which, the igneous lithological reservoir be of significance as a new research and exploration area. The purpose of this paper is, with the historical researches and data as base, the System Theory, Practice Theory and Modern Comprehensive Petroleum Geology Theory as guide, the theoretical and practice break through as the goal, and the existing problems in the past as the break through direction, to explore and establish a valid reservoir formation and distribution models for igneous strata in the profile of the eastern faulted basins. After investigating the distribution of the igneous rocks and review the history of the igneous rocks reservoirs in basins, the author focused on the following issues and correspondingly the following progresses have been made: 1.Come to a new basin evolution and structure model named "Combined-Basin-bodies Model" for Jiyang even Eastern faulted basins based on the study on the origin and evolution of Jiyang & Changwei basins, depending on this model, every faulted basin in the Bo-hai Bay Basin is consisted of three Basin-Bodies including the Lower (Mesozoic), Middle (Early Tertiary) and the Upper (Late Tertiary) Bodies, each evolved in different geo-stress setting and with different basin trend, shape and igneous-sedimentary buildings system, and from this one to next one, the basin experienced a kind of process named "shape changing" and "Style changing". 2. Supposed a serious of new realizations as follows (1) There were "multi-level magma sources" including Upper mantel and the Lower, Middle and even the Upper Shell magma Chambers in the historical Magma Processes in the basins; (2) There were "multi-magma accessing or pass" from the first level (Mantel faults) to the second, third and fourth levels (that is the different levels of fault in the basin sediment strata) worked in the geo-historical and magma processes; (3) Three tectonic magma cycles and more periods have been recognized those are matched with the "Basin -body-Model" and (4)The geo-historical magma processes were non-homogeneous in time and space scale and so the magma rocks distributed in "zones" or "belts". 3. The study of magma process's effect on basin petroleum conditions have been made and the following new conclusions were reached: (1) the eruptive rocks were tend to be matched with the "caped source rock", and the magma process were favorable to the maturing of the source rocks. (2) The magma process were fruitful to the accumulation of the non-hydrocarbon reservoirs however a over magma process may damage the grade of resource rock; (3) Eruptive activity provided a fruitful environment for the formation of such new reservoir rocks as "co-eruptive turbidity sandstones" and "thermal water carbonate rocks" and the intrusive process can lead to the origin of "metamorphism rock reservoir"; (4) even if the intrusive process may cause the cap rock broken, the late Tertiary intrusive rocks may indeed provide the lateral seal and act as the cap rock locally even regionally. All above progresses are valuable for reconstructing the magma-sedimentary process history and enriching the theory system of modem petroleum geology. 4. A systematic classification system has been provided and the dominating factors for the origin and distribution of igneous rock reservoirs have been worked out based on the systematic case studies, which are as follows: (1) The classification is given based on multi-factors as the origin type, litho-phase, type of reservoir pore, reservoir ability etc., (2) Each type of reservoir was characterized in a detailed way; (3) There are 7 factors dominated the intrusive reservoir's characteristics including depth of intrusion, litho-facies of surrounding rocks, thickness of intrusive rock, intrusive facies, frequency and size of the working faults, shape and tectonic deformation of rock, erosion strength of the rock and the time of the intrusion ect., in the contrast, 4 factors are for eruptive rocks as volcanic facies, frequency and size of the working faults, strength of erosion and the thermal water processing. 5. Several new concept including "reservoir litho-facies", "composite-volcanic facies" and "reservoir system" ect. Were suggested, based on which the following models were established: (1) A seven reservoir belts model for a intrusive unit profile and further more, (2) a three layers cubic model consisted of three layer as "metamorphic roe layer", "marginal layer" and "the core"; (3) A five zones vertical reservoir sequence model consisted of five litho-facies named A, B, C, D and E for a original lava unit and furthermore three models respectively for a erosion, subsidence and faulted lava unit; (4) A composite volcanic face model for a lava cone or a composite cone that is consisted of three facies as "crater and nearby face", "middle slope" and "far slope", among which, the middle slope face is the most potential reservoir area and producible for oil & gas. 6. The concept of "igneous reservoir" was redefined as the igneous, and then a new concept of "igneous reservoir system" was supposed which means the reservoir system consisted of igneous and associated non-igneous reservoirs, with non-hydrocarbon reservoir included. 7. The origin and distribution of igneous reservoir system were probed and generalized for the exploration applications, and origin models of the main reservoir sub-systems have been established including those of igneous, related non-igneous and non-hydrocarbon. For intrusive rocks, two reservoir formation models have been suggested, one is called "Original or Primary Model", and the another one is "Secondary Model"; Similarly, the eruptive rock reservoirs were divided in three types including "Highly Produced", "Moderately Produced" and "Lowly Produced" and accordingly their formation models were given off; the related non-igneous reservoir system was considered combination of eight reservoirs, among which some ones like the Above Anticline Trap are highly produced; Also, the non-hydrocarbon. Trap system including five kinds of traps was discussed. 8. The concept models for four reservoir systems were suggested, which include the intrusive system consisted of 7 kinds of traps, the land eruptive system with 6 traps, the under water eruptive system including 6 kinds of traps and the non-hydrocarbon system combined by 5 kinds of traps. In this part, the techniques for exploration of igneous reservoir system were also generalized and probed, and based on which and the geological progresses of this paper, the potential resources and distributions of every reservoir system was evaluated and about 186 millions of reserves and eight most potential non-hydrocarbon areas were predicted and outlined. The author believe that the igneous reservoir system is a very important exploration area and its study is only in its early stage, the framework of this paper should be filled with more detailed studies, and only along way, the exploration of igneous reservoir system can go into it's really effective stage.

太阳辐射对溶解有机质荧光光谱特征的影响

利用三维荧光光谱研究了太阳辐射对溶解有机质(DOM)荧光光谱特征的影响。实验结果表明,太阳辐射使DOM的荧光发射光谱强度减弱。在三维荧光光谱图中,红枫湖样品的荧光峰A,C,南明河样品的荧光峰A,B,C,尤其是荧光峰C的λExmax/λEmmax位置随着太阳辐射时间的延长而逐渐向短波长移动。从腐殖酸样品的三维荧光光谱图中则发现,原始样品荧光峰位置出现在λEx/λEm=275/500nm处,光照作用后出现两个荧光峰λEx/λEm=245/450nm和310/450nm。太阳辐射对DOM中不同荧光组分的光降解速率存在差异,从荧光峰A和C的比值r(A,C)随太阳辐射时间的变化趋势得知,荧光峰C比荧光

过去5000年西太平洋副热带高压活动的泥炭纤维素碳同位素记录

文章以金川和红原两组泥炭纤维素Δδ13C 时间序列值的反向变化来指示西太平洋副热带高压活动变化。结果表明,在过去5 000 年中,西太平洋副热带高压的活动可分为4 个阶段,即西太平洋副热带高压位置在2800～2200 B. C. 期间持续偏北,2200～600 B. C. 期间持续偏南,600 B. C. ～ 1200 A.D. 期间在北进与南移之间频繁波动,以及1200 ～1900A. D. 期间再次持续偏北,它们导致降雨量在中国大陆上不同的分布。从约1900A. D. 起西太平洋副热带高压的活动似乎又开始一个新的偏南阶段,值得进一步加强研究。

临沧锗矿床的微量元素地球化学

采用ICP—MS测定了临沧锗矿中51个含矿煤、5个无矿煤、9个硅质岩样品的微量元素含量，并与基底二云母花岗岩进行对比，探讨了含矿煤与无矿煤的微量元素地球化学及其与锗超常富集的关系，得出几点认识：a.含矿煤、无矿煤和硅质岩中的大多数微量元素来自基底的二云母花岗岩；b．热水携带了成矿所必需的锗；c．Nb可作为锗矿化的指示元素。

中国炼锌向大气排汞及其环境影响的初步研究

汞是一种毒性极强的环境污染物。由于汞能在大气中存在并能长距离迁移，因此汞已经被定义为全球性污染物。研究表明有色金属锌的冶炼是大气汞的一个重要的人为汞污染源。西方发达国家在炼锌过程中由于有严格的污染物控制措施，使得这个问题得到有效的控制。由于经济和技术的原因我国大多数锌冶炼企业在冶炼过程中没有进行烟气汞的回收，从而使得我们不能借鉴国外的相关研究成果。我国2005年精锌总产量占到了世界的1/4，是全世界最大的锌锭生产国家，但相关的研究却非常滞后。近年来我国锌冶炼向大气排汞的问题已经引起了国际争议，而且冶炼过程中排放的汞对局部生态系统会产生重要影响，因此锌冶炼过程中释放汞所造成的环境问题已经越来越受到人们的关注和重视。 本研究的目的是通过对不同锌矿山的锌矿石和浮选锌精矿以及冶炼厂不同源锌精矿的研究从而了解我国的矿石汞含量，及矿石浮选过程中汞的分配；通过对冶炼过程向大气排汞的研究，认识锌精矿中汞在锌冶炼过程中的分配，估算不同冶炼方式汞的释放因子。如A、B和C冶炼厂是用不同的工艺来炼锌的，其汞的释放因子也不同。通过对土法炼锌区和工业炼锌区水体、土壤、大气和植物中汞的分布、迁移转化规律的研究，认识锌冶炼对局部生态系统产生的影响。 1.矿石和锌精矿中汞的研究 成因和分类不同的铅锌矿床锌矿石和浮选锌精矿中汞的测定结果表明：凡口矿的矿石和浮选的锌精矿中汞含量比兰坪矿矿石和浮选锌精矿高了2个数量级。凡口矿锌矿石和锌精矿中汞的含量分别是64.5-107 mg∙kg-1，588-602 mg∙kg-1；对应兰坪矿锌矿石和锌精矿中汞的含量分别是0.23~0.40 mg∙kg-1，1.91-3.33 mg∙kg-1。不同冶炼厂不同矿源的锌精矿中汞含量测定结果表明：不同源锌精矿中汞含量在0.10-1100 mg∙kg-1之间，变动范围非常大。而冶炼厂冶炼所用的混合锌精矿中汞含量差别不大，冶炼所用的混和锌精矿汞含量在37-105 mg∙kg-1之间变动。 2.锌精矿中汞在冶炼过程中的分配和汞释放因子的研究 对采用不同炼锌工艺的冶炼厂和有除汞工艺的A、B冶炼厂所用的锌精矿中的汞在冶炼过程分配的质量平衡对比表明，A冶炼厂和B冶炼厂锌精矿中的汞在冶炼过程中的分配显著不同，主要制约因素是是否对烟气中汞进行回收。在烟气到达除汞设备前，A和B冶炼厂在焙砂和尘、酸洗、电除雾等流程对烟气中汞的去除效果相近。不同的是，A厂要进行烟气汞回收，烟气经过汞回收后，50%以上烟气中的汞在这一流程被去除。这使得A、B冶炼厂后续的流程制酸吸收汞和排向大气汞所占的比例有较大的差异。 不同冶炼方式的汞释放因子表明，无任何环保措施的土法炼锌活动的释汞因子为113 g·t-1，不对烟气汞进行回收的B厂和C冶炼厂汞的释放因子分别为49 g·t-1和243 g·t-1，对烟气汞回收的A冶炼厂汞的释放因子为5.7 g·t-1。综合各种不同炼锌方式的汞释放因子及其精锌产量，得出了锌冶炼过程中汞的综合释放因子，从而估算出我国锌冶炼向大气排汞量约61.3-178 t·y-1。 3.锌冶炼对局部生态系统的影响 炼锌区的冶炼废渣是冶炼过程中的主要废弃物，随意堆放的废渣是当地农田土壤的重要汞污染源，大气汞中活性汞和颗粒态汞的沉降也是当地农田土壤另一个汞污染源。土法炼锌区和工业炼锌区土壤分析结果表明，工业炼锌对局部环境的影响更为严重。土壤汞含量对比如下：A冶炼厂周边环境污染土壤汞含量259-2990 μg·kg-1，远高于威宁土法炼锌点污染土壤汞含量72-355 μg·kg-1。威宁土法炼锌点土壤中甲基汞含量的分析表明，在冶炼点附近的土壤中甲基汞绝对含量和甲基汞/总汞的比例都高于其它样点，说明冶炼点附近土壤中汞的甲基化水平提高。A冶炼厂污水处理渣亦没有得到妥善的处理，成为当地潜在的汞污染源。 土法炼锌区水体汞的含量明显受到冶炼渣的影响。工业炼锌过程产生的废水经处理后的水汞含量100%超过国家工业废水排放标准，这些处理后的水的排放是当地重要的汞污染源。A冶炼厂周边稻田水分析表明，溶解态甲基汞占溶解态总汞的的平均比率（5%）远高于一般自然水体（<1%），可能与稻田特殊环境有关。 土法炼锌区大气汞含量测定表明，冶炼点附近大气汞浓度剧增，高达5220 ng·m-3，锌冶炼是当地主要的大气汞污染源。大气汞浓度的提升，是导致农作物玉米叶部位汞含量增高的原因。植物体的地上绿色部分通过叶片吸收大气汞是植物体内汞富集的重要途径之一。 土法炼锌区和工业炼锌区农作物果实中汞含量的测定结果对比如下：A冶炼厂附近稻田产出的部分大米样品中总汞含量已经超过了国家食品限量卫生标准（20 µg·kg-1），所有辣椒中总汞含量全部超出了国家蔬菜卫生限量标准（10 µg·kg-1）。土法炼锌区所取农作物样品未出现果实汞含量超标现象。食用这些汞含量超标的食物将对当地居民带来潜在的危害。

贵州碳酸盐岩风化壳次生石英表面结构、裂变径迹测年及其指示意义

我国西南地区分布有广阔的亚热带潮湿区岩溶，以贵州为中心，总面积达50万km2，是世界上连片分布面积最大的岩溶区。贵州高原地处青藏高原东南缘,云贵高原的东翼，是中国大陆“西高东低”地貌格局中重要的过渡区段，对其新生代地质、地貌演化进行研究无疑具有重要的意义，不仅是对贵州薄弱的新生代地质、地貌研究的补充，而且可以直接通过夷平面展开与青藏高原的对比，探讨青藏高原隆升对贵州高原的直接影响。风化壳作为夷平面的组成部分，在过去没有引起足够的重视，但随着成功实例的不断出现，人们逐渐开始认识到风化壳是夷平面识别和重建的重要依据，也是夷平面环境信息的重要载体。贵州作为碳酸盐岩集中分布区，碳酸盐岩风化壳剖面广泛存在，尤其在黔中、黔北等地区各级夷平面上均发育有红色风化壳，利用碳酸盐岩红色风化壳能为夷平面的识别和形成时代的确立提供可靠的证据，特别是风化壳形成年龄的确定对夷平面时标的建立更具有积极意义。有关贵州地区红色风化壳形成时代的确定，多年来已有一些学者对此展开了研究，但贵州红色风化壳形成时代的确定存在着很大争论。虽然存在其它原因的可能性，但造成这种争论的根本原因在于贵州红色风化壳形成时代是依据其它资料(如夷平面、气候事件等)推断出来的，而不是根据直接测年数据界定的。因此，风化壳直接测年才是解决问题的关键。 本文在前人工作研究的基础之上，利用扫描电镜手段对贵州碳酸盐岩地区上覆风化壳土层中的石英颗粒进行观察、统计、分析，为风化壳成土的物质来源寻找新的证据；同时，经地球化学分析、测试等手段，判断风化壳土层中的晶体石英颗粒为风化壳形成初期的新生矿物——次生石英颗粒，并利用裂变径迹测年法对这种次生石英颗粒进行测年，最终探讨贵州碳酸盐岩地区上覆风化壳土层的形成年代。主要取得了以下几点认识： 一、石英颗粒蚀刻条件的优选 由于石英颗粒裂变径迹的长度和数量与晶格、铀含量、年龄等因素有关，所以不同地区的石英颗粒样品的裂变径迹蚀刻条件也存在差别；目前国际上有关石英颗粒的裂变径迹测年应用的实例较少，还没有统一的有关石英颗粒蚀刻条件的国际标准；现有的石英颗粒蚀刻条件有多种，但是缺乏对这些方法的优缺点进行对比评价。因此，我们要进行反复的条件实验，对比不同石英蚀刻剂的蚀刻效率，找寻适合石英颗粒的最佳蚀刻剂。实验结果表明，40%的HF溶液为最佳蚀刻剂，最佳蚀刻时间：温度在4℃左右（冬季）时为40min；温度在29℃左右（夏季）时为30min。 二、石英的外形、表面机械作用特征及其指示意义 我们利用扫描电镜对石英颗粒外形特征进行观察、统计、分析，结果表明本次研究的石英颗粒形态类型主要有两种：棱状-次棱状石英颗粒以及圆状、次圆状石英颗粒，其中棱状-次棱状石英颗粒包含了一部分晶体形态较为完整的石英颗粒。 根据石英颗粒表面机械作用特征分析结果，结合剖面区域地质特征，可初步判断剖面中的石英颗粒有三种物质来源：碳酸盐岩中的原生碎屑石英，有长时间长距离搬运特征；燧石团块石英，有短距离搬运或原位沉积特征；晶形较完整的次生石英，无搬运特征。三种石英均具有原位特征，前两种类型的石英是直接对基岩的继承，第三种类型的石英是风化壳剖面的次生矿物。 三、石英颗粒表面的化学作用特征及其风化强度指示意义 我们通过对石英颗粒表面化学作用形态的观察，发现大兴剖面、新蒲剖面和官坝剖面的石英颗粒表面化学溶解作用和化学沉淀作用都非常强烈，这表明三个剖面均处于湿、热环境中，均处于强烈的化学风化阶段。而且大兴剖面中石英颗粒表面的化学作用最强烈，气候较其他两个剖面更湿热，剖面的风化强度也最大，即各剖面的风化强度由强到弱排序为：大兴、新蒲、官坝。这一结果与矿物组成分析、化学风化强度、硅铝、铝铁硅风化系数比以及相对风化强度等的地球化学分析指标相一致，这也再次证明了我们采用石英颗粒表面形态特征分析手段的可行性和可靠性。 四、石英颗粒的裂变径迹年龄 三种类型石英颗粒的裂变径迹测年数据表明：a、同一样点石英颗粒裂变径年龄呈现一定的规律：F.T.AGE圆状、次圆状＞F.T.AGE不规则状（棱状、次棱状）＞F.T.AGE标准晶形（次生石英）。b、不同剖面的不规则状石英颗粒形成于同一个时期；不同剖面的圆状、次圆状石英颗粒形成于同一个时期。这两种石英颗粒不适于贵州碳酸盐岩风化壳的测年研究。c、不同剖面的标准晶形石英颗粒形成于不同时期，形成于碳酸盐岩酸不溶物原地堆积过程中，即与风化壳剖面同期形成，可用于贵州碳酸盐岩风化壳的测年研究。这一测量结果与我们对石英颗粒表面形态特征的观察、统计、分析结果相一致。 五、风化壳物源的新证据 贵州碳酸盐岩风化壳中的石英颗粒表面形态的分析结果表明，贵州碳酸盐岩风化壳的物质来源于碳酸盐岩中酸不溶物原地风化残积的产物，与其下伏基岩有着明显的继承性。这一分析结果与王世杰等人的碳酸盐岩酸不溶物的提取实验、地球化学、矿物学、粒度特征及区域地质背景等多方面的分析结果相一致，为贵州碳酸盐岩风化壳的物质来源及成因提供新的、更细致的证据。 六、贵州晚新生代地质-环境研究历史轮廓初建 由于目前对贵州及周边地区的风化-气候研究相对缺乏，数据资料较稀少，还没有形成完整的系统，我们本次研究也是建立在对风化壳中次生英颗粒年代学研究的基础上，研究还不是很透彻，因此只能对地质-环境研究历史轮廓进行初建。本文根据本次研究剖面土层中晶体次生石英颗粒的裂变径迹年龄分布情况，结合前人已有资料，对贵州25Ma以来的地质-环境演化历史的轮廓进行初建。从次生石英裂变径迹年龄值来看，中新世以来贵州主要经历了如下构造-风化期：25-19Ma、16-13Ma、10-6.5Ma、5-2Ma、1.7-1Ma。

贵州红枫湖汇水区黄壤化学风化动力学及其生态环境效应

在地球的环境界面上，发生着重要的物理、化学和生物学反应，进行着频繁的物质交换和输送，研究和认识环境界面的地球化学过程对揭示环境演化，评价环境质量，认识成矿机理具有重要意义[万国江，1988]化学风化是元素表生地球化学循环的重要环节，是地表碉石（浮土）-水界面间的物质交换过程，其中大气成份和植物微生物代谢产物作为活化剂。化学风化的研究历史大致分为三个阶段：定性描述阶段、化学风化速度定量测定阶段、化学风化的环境生态效应研究阶段。化学风化的动力学理论经过了扩散作用理论、表面反应理论、表面络合反应理论三个发展阶段。化学同化动力学理论及其生态效应方面的研究存在的主工问题是：矿物溶解速度是由表面反应控制的，土壤具有特殊的表面性质，但目前还没有土壤化学同化动力学的实验数据。溶解铝主要来自土壤活性铝，但土壤铝的溶解机理还不清楚；仅根据化学平衡计算就认为Al~(3+)浓度是由矿物溶解平衡控制的，这很不可靠；因为土壤孔隙水的酸度控制矿物的溶解平衡，而土壤中Al~(3+)的水解制约着土壤孔隙水的酸度。孤立地研究养分的释放和流失是不完深善的，需要建立养分循环的动力学模型。黄壤是贵州分布最广的一种土壤。贵州存在着环境酸化、土壤缺钾和“石山”化等一系列生态环境问题。黔中是一个较强的酸雨区，区内降水pH值位于3.5-4.2之间；黄壤酸度高，缓冲能力弱。黄壤中活性铝浓度高，但国内没有进行黄壤中铝的淋溶和毒性的研究。黄壤是中国最贫钾的土壤之一，但缺钾的原因和发展趋势还不清楚。本文的目的是完善土壤化学风化动力学理论、阐明环境中铝的转化机理、建立钾素循环的动力学模型。同时，预测环境酸化趋势、评价土壤钾素供给状况和铝的毒性，讨论关于贵州环境酸化、土壤缺钾和“石山”化等环境生态问题的对策。作者在红枫湖汇水区采集土壤、土壤孔隙水和河水样品。土壤孔隙水用经改进的离心法提取；用化学浸提法测定土壤中铝的形态；完成了河水、土壤孔隙水的水化学全分析、土壤化学性质的测定、土壤的化学全分析和X射线衍射分析，湖水水化学全分析数据由导师提供。作者完成了土壤淋溶实验的研究，测定了淋溶前土壤样品的化学质和化学组成，测定了淋溶液的pH、Ca~(2+)、Mg~(2+)、K~+、Na~+溶解硅和单体铝。通过土壤、土壤孔隙水、湖水的化学年组成，研究土壤的化学风化动力学；通过土壤、土壤孔隙水中铝的形态分布，研究环境中铝的迁移转化机理；根据河水中钾的含量，研究土壤钾素的地球化学循环；通过土壤淋溶实验研究土壤化学风化、土壤铝淋溶、钾素循环的动力学过程。综合现场取样和淋溶实验两方面的研究成果，获得以下几点认识：1、红枫湖汇水区黄壤的化学风化处于高岭石化阶段，酸沉降增大化学风化速度，土壤化学风化符合硅酸盐矿物溶解的表面反应理论。2、实验证实了Johnson (1981)提出的土壤缓冲机制，同时发现弱酸性和中性土壤在淋溶过程中吸附H~+。3、黄壤中铝的移动性与土壤酸度和有机质含量有关，溶解铝在土壤A-B、B-C���面发生沉淀。4、实验证实铝的溶解由三水铝石溶解反应控制，同时发现溶解铝浓度由H~+供给量和盐基离子释放量控制。5、建立钾素循环的动力学模型：EXCH. K=Fw-Fd-Fa利用河水中K~+浓度计算土壤钾素的化学侵蚀速率，可以预测土壤缺钾的趋势。6、实验发现土壤钾素的化学侵蚀过程由离子交换反应控制，钾素侵蚀速率与径流强度、土壤酸度和酸沉降有关。7、酸沉降加剧黄壤酸化和缺钾的趋势，加重黄壤中铝的毒性，需要控制酸沉降通量，使雨水pH值大于4.5。

Novas técnicas de multiplicação de ramas de batata-doce.

2005

Esplanada: cultivar de cenoura de verão para processamento.

2005

Qualidade visual de cenourete e catetinho em função das operações de acabamento e centrifugação.

2007

Tamanho da matéria prima e tempo de processamento para produção de minicenouras cenourete e catetinho.

2007

Procedimento da Embrapa Milho e Sorgo para extração de DNA de tecido vegetal em larga escala.

2010

Utilização de marcadores moleculares na seleção assistida para tolerância ao alumínio em sorgo.

2010

Instability of anthocyanin accumulation in Vitis vinifera L. var. Gamay Freaux suspension cultures

The inherent instability of metabolite production in plant cell culture-based bioprocessing is a major problem hindering its commercialization. To understand the extent and causes of this instability, this study was aimed at understanding the variability of anthocyanin accumulation during long-term subcultures, as well as within subculture batches, in Vitis vinifera cell cultures. Therefore, four cell line suspensions of Vitis vinitera L. var. Gamay Freaux, A, B, C and D, originated from the same callus by cell-aggregate cloning, were established with starting anthocyanin contents of 2.73 +/- 0.15, 1.45 +/- 0.04, 0.77 +/- 0.024 and 0.27 +/- 0.04 CV (Color Value)/g-FCW (fresh cell weight), respectively. During weekly subculturing of 33 batches over 8 months, the anthocyanin biosynthetic capacity was gradually lost at various rates, for all four cell lines, regardless of the significant difference in the starting anthocyanin content. Contrary to this general trend, a significant fluctuation in the anthocyanin content was observed, but with an irregular cyclic pattern. The variabilities in the anthocyanin content between the subcultures for the 33 batches, as represented by the variation coefficient (VC), were 58, 57, 54, and 84% for V vinifera cell lines A, B, C and D, respectively. Within one subculture, the VCs from 12 replicate flasks for each of 12 independent subcultures were averaged, and found to be 9.7%, ranging from 4 to 17%. High- and low-producing cell lines, VV05 and VV06, with 1.8-fold differences in their basal anthocyanin contents, exhibited different inducibilities to L-phenylalanine feeding, methyl jasmonate and light irradiation. The low-producing cell line, showed greater potential in enhanced the anthocyanin production.

Avaliação do fosfito de potássio no controle do míldio da videira.

2003