不同年份早酥梨叶片浸提液对几种套作蔬菜的影响

采用室内培养皿滤纸法进行种子发芽的方法,通过测定早酥梨叶片浸提液对几种蔬菜种子胚根生长的影响,研究了不同浓度浸提液对几种蔬菜的化感作用。为制定合理的间套作耕作制度,更好的安排果树生产布局提供科学依据。结果表明:早酥梨叶片浸提液对蔬菜胚根生长的影响总体上表现为低促、高抑,即低浓度的浸提液对蔬菜胚根的生长有促进作用,较高浓度的浸提液对蔬菜胚根的生长产生抑制作用,浓度越高,抑制作用越强。不同生长年限的早酥梨叶提取液对其间作套种蔬菜抑制作用的强弱顺序为生长第6年>第7年>12年>生长第22年>第4年。

乙酰丙酸钾对黄土高原山地红枣生长发育及产量品质的影响

选用9 a生盛果期矮化密植梨枣树为试验材料,研究乙酰丙酸钾叶面喷施对黄土高原山地红枣生长发育及产量品质的影响。结果表明:叶面喷施稀释800倍的乙酰丙酸钾,对枣树的生长发育、产量和品质都有明显的促进作用,建议在黄土高原区红枣实际生产中采用稀释800倍的乙酰丙酸钾喷施。

宁南山区防雹网内梨园生境状态研究

2007年实地观测固原上黄村1 500 m2设防雹网梨园土壤水分、空气、湿度等微生境条件变化程度,研究分析了防雹网对宁南山区梨园生境状况的影响。结果表明:梨园使用防雹网能改善果园小气候,提高梨园1 m高度空气相对湿度,其日变化符合y=ax2-bx+c二次抛物线,晴天的曲线曲率高于阴天,梨园1 m高度温度有防雹网低于无防雹网;0~200 cm土壤剖面的水分含量有防雹网高于没有防雹网;同时,使用防雹网能够在白天降低土壤温度,夜间维持较高的土壤温度,缓解土壤温度的变化幅度,特别是表层温度变化更明显。

南海北部大陆边缘盆地热演化史及其与油气关系

This thesis focuses on the present-day thermal field features, evolution and their connections to hydrocarbon generation of the three continental margin basins-the Yinggehai (Yingge Sea), Qiongdongnan(southeast Qiong), and Pear River Mouth basins-in northern South China Sea, based on available data from drillings, loggings, seismic cross-sections, BHTs, thermal indicators (Ro%, inclusion, etc) and geopressure measurements. After studying of present-day distribution of geothermal field and thermal disturbance of fluid in the sedimentary strata, the author discovered that the distribution of gas fields in Yinggehai Basin are closely related to the distribution of anomalously high thermal gradient area, whereas it is not the case for the Pear River Mouse Basin. And detailed processing of the fluid inclusion data indicates that geothermal fluids activated frequently in this area, and they may mainly be derived upward from the overpressure and hydrocarbon-generating beds, 3000-4500 m in depth. Therefore, the abnormal gradients in sedimentary beds were mainly caused by the active geothermal fluids related to hydrocarbon migrating and accumulating in this area. Because of the effect of overpressure retarding on vitrinite reflectance, the thermal indicators for thermal history reconstruction should be assessed before put into use. Although some factors, such as different types of kerogen, heating ratio, activities of thermal fluids and overpressure, may have effects on the vitrinite reflectance, under the circumstance that thermal fluids and overpressure co-exist, overpressure retarding is dominant. And the depth and correction method of overpressure retarding were also determined in this paper. On the basis of reviewing the methods of thermal history studies as well as existing problems, the author believes that the combination of thermal-indicator-inversion and tectono-thermal modeling is an effective method of the thermal history reconstruction for sedimentary basins. Also, a software BaTherMod for modeling thermal history of basins was successfully developed in this work. The Yinggehai Basin has been active since Tertiary, and this was obviously due to its tectonic position-the plate transition zone. Under the background of high thermal flow, long-term quick subsidence and fluid activities were the main reasons that lead to high temperature and overpressure in this basin. The Zhujiangkou Basin, a Tertiary fault-basin within the circum-Pacific tectonic realm, was tectonically controlled by the motion of the Pacific Plate and resembles the other petroliferous basins in eastern China. This basin developed early, and characterized intensive extension in the early stage and weak activity in the later stage of its development. Whereas the Qiongdongnan Basin was in a weak extension early and intensity of extension increased gradually. The relative geographical locations and the extensional histories of three basins ilustrate that the northern continental margin of South China Sea spread from south to north. On the other hand, the Qiongdongnan and Yinggehai Basins may have been controlled by the same tectonic regime since later Tertiary, whereas the Zhujiangkou Basin was not meaningfully influenced. So, the tectono-thermal evolution character of the Qiongdonnan basin should be closely to the other two. It may be concluded that the three basins have been developed within the active continental margin since Tertiary, and the local lithosphere might undergo intensive extension-perhaps two or three times of episodic extension occurred. Extension lead to large tectonoc subsidence and extreme thick Tertiary sediments for hydrocarbon generation in the basins. In response to the periodic extension of the basins, the palaeothermal flow were also periodical. The three basins all have the characteristics of multi-phase thermal evolutions that is good for oil-gas generation. And the overpressure expands the depth range of oil-gas habitat, which is meaningful to petroleum exploration in this region.