不同耕作方式对黑土微生物特性的影响

东北黑土是我国有机质含量最高的土壤之一，但由于长期的掠夺式经营和不合理的耕作制度使得黑土有机质的收支严重失衡，土壤退化严重。保护性耕作是保持土壤质量和改善生态环境的有效措施。与传统耕作相比，保护性耕作能够在保证正常农业生产的前提下达到保护土壤的目的。 本文以吉林省德惠市中层黑土上进行了7年的田间定位试验小区土壤为研究对象，选取对耕作方式和作物覆盖较为敏感的微生物指标，包括微生物量碳和磷脂脂肪酸，探讨免耕措施和传统耕作对土壤微生物群落的影响，为保护性耕作在东北黑土的实践提供理论依据。 研究结果表明： 1耕作方式对土壤理化性质及微生物量碳有较大的影响。和传统耕作相比，免耕措施显著提高了土壤表层(0-5 cm)的全碳、全氮、碱解氮、热水溶性有机碳和微生物量碳，促进各种养分和有机质在土壤表层富集，为作物生长和微生物代谢提供了丰富的资源。土壤微生物量碳随时间的变化总体上呈现增加趋势。 2相对于传统耕作，免耕措施显著提高了土壤表层(0-5 cm)的总脂肪酸量、细菌和真菌生物量，尤其是免耕玉米连作的作用更明显。但真菌和细菌生物量的增加并不成比例，真菌生物量增加快于细菌，使得免耕措施下土壤的真菌/细菌值有所提高，有利于农田土壤生态系统的稳定性。不同耕作措施对G+/G-值影响的差异不显著。 3不同耕作措施在作物生长期内对微生物群落结构的影响较小，尤其在7月，由于温度和水分等环境条件的适宜，作物生长处于顶峰期，其根系活动对微生物群落结构的影响已经超过了不同耕作措施对微生物群落结构的影响，使得7月份不同耕作措施之间的生物量差异消除。 4耕作措施对不同土层的影响不同，不同耕作措施的PC1值对土层深度的响应明显(p<0.01)不同。2种免耕处理PC1值随土层深度的变化曲线是二次多项式，而传统耕作PC1值随土层深度呈现线性变化。7月的PC1值没有发现耕作措施对不同土层的影响。

岷江上游人工针叶、阔叶林土壤可溶性有机物质特征及其对凋落物分解的响应

土壤可溶性有机物质（Dissolved organic matter，DOM）作为土壤有机质的活性组分，在陆地生态系统物质循环中扮演非常重要的角色。土壤DOM的主要成分可溶性有机碳（Dissolved organic carbon，DOC）和氮（Dissolved organic nitrogen，DON）参与C、N循环过程。为深入揭示全球C、N循环过程机制，在未开展DOC和DON的地区进行相关研究是有必要的。森林土壤（包括枯枝落叶层）DOC、DON动态及调控机理的研究是目前国际上森林生态系统C、N循环研究热点之一。本研究立足于暖温带岷江上游茂县地区人工林植被，对土壤DOC和DON的库容量，季节动态及其与其它养分之间的关系进行了系统研究，旨在了解DOC和DON在该区生态系统中的重要作用，并探讨作为DOM主要来源的叶凋落物对DOC和DON的动态影响，研究有助于更加详细地了解该区生态系统C和N循环过程。本论文主要研究结论如下： 1研究了岷江上游地区两大主要土壤类型（棕壤和褐土）不同植物群落下土壤的DOC和DON含量及特征，结果表明：DOC和DON在两种土壤类型中均有库容量存在，DOC在0-10cm和10-20cm土层的含量幅度分别111.96~159.95 mg kg-1和69.02~100.84 mg kg-1。DON在0-10cm和10-20cm土层的含量幅度分别11.88~23.08 mg kg-1和4.70~10.77 mg kg-1。游离氨基酸在0-10cm和10-20cm土层的含量幅度分别0.84~1.66 mg kg-1和0.39~0.73 mg kg-1。DOC、DON与土壤中的一些养分因子表现出了显著的相关关系，共同反映了土壤的状况和质量，在该区开展DOC和DON的系统研究是有必要的。 2 对油松与连香树林地土壤DOC、DON以及其它化学指标的季节动态进行了研究，结果表明：油松与连香树林地土壤DOC和DON的季节动态变化表现了类似的规律，DOC和DON的含量均以秋季最高。DOC和DON的季节动态变化主要受凋落物生物因素的影响，但其微生物活力的生物因素以及降雨、温度等非生物因素也是控制土壤DOC和DON含量的重要因素。土壤DON在土壤中的行为不同于矿质氮，其季节动态不同于NO3--N和NH4+-N的季节动态，在研究N循环过程中，应考虑DON的变化情况。 3 对油松与连香树林地分解层和表层土壤（0-10cm）氨基酸周转动态进行了研究，结果表明：油松林地和连香树林地均以分解层的氨基酸含量高于矿质表层土壤的含量。每个取样时期，油松林地内各层次的氨基酸含量高于连香树林地内相应层次的含量。两林地各层次无机氮含量均超过了氨基酸的含量，并且室内培养30天后无机N的含量仍然高于氨基酸的含量，所以可以认为该区立地条件下无论是在有机分解层还是矿质土层植物吸收利用的氮素仍是以无机N为主。 4 松林下松针凋落物易于累积，这与松针凋落物分解缓慢有关，从而导致松林内养分周转缓慢。通过用不同性质凋落物和灌丛地土壤构建微生态系统，比较油松、辐射松、连香树、灌丛虎榛子凋落物分解对C、N循环过程的影响，结果显示油松和辐射松针叶凋落物比连香树、虎榛子凋落物分解更慢，减缓了养分循环过程。然而将针叶凋落物与阔叶凋落物混合后，油松和辐射松针叶凋落物的分解加快，C、N元素的循环过程也加速。此结果表明在松林内维持具有高质量凋落物的灌丛植被或在松林内栽植一些阔叶树种如连香树对维持和增进松树人工林的土壤肥力有重大的作用。室内培养的结果还显示添加凋落物后土壤DOC和DON的含量显著增加，表明凋落物是土壤DOM的直接来源。然而不同物种凋落物处理下土壤DOC和DON的含量有所不同，并随时间发生改变。混合凋落物处理下土壤DOC和DON的含量均高于松针凋落物单独处理下土壤DOC和DON的含量。DON是一个主要的水溶性N库，随时间的变化趋势与无机N的变化趋势不同，在土壤N循环过程中起到了中间N库的作用。 As a labile fraction of soil organic matter, dissolved organic matter (DOM) plays a very important role in material cycling of terrestrial ecosystem. The turnover of DOM is now being considered as main components in nutrient cycling. DOM mainly includes dissolved organic carbon (DOC), -nitrogen (DON), -phosphorous (DOP) and –sulfur (DOS). Among these constituents, DOC and DON directly participate in C and N cycling. It is essential to study DOC and DON dynamics and their controlling factors in the areas where no related study has ever been carried out. Study about them can provide data supports on understanding the mechanism of the global C and N cycling. DOC and DON dynamics and their controlling factors have been focused on in the research of C and N cycling of forest ecosystems. Based on forest plantations of Maoxian, Minjiang River in warm temperate zone, soil DOC and DON pool size, their seasonal dynamics, and the correlation between DOC, DON and other nutrients were studied in order to understand the importance of DOC and DON in the study area. Soil DOC and DON dynamics induced by leaf litter decomposition were also studied. The study contributed to comprehensively understanding C and N cycling processes and providing baseline data for including DOC and DON into the indices system of evaluating nutrient conditions. The results were as follows: 1 Several different plant communities under brown soil and Cinnamon soil were chosen as sampling plots. The contents and features of soil DOC and DON were evaluated. The results showed that DOC and DON were present under the two soil types. DOC contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 111.96 mg kg-1to 159.95 mg kg-1, and 69.02 mg kg-1 to 100.84 mg kg-1. DON contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 11.88 mg kg-1to 23.08 mg kg-1, and 4.70 mg kg-1 to 10.77 mg kg-1. Free amino acid contents in the top soil (0-10 cm) and the subsoil (10-20 cm) respectively varied from 0.84 mg kg-1to 1.66 mg kg-1, and 0.39 mg kg-1 to 0.73 mg kg-1. Significant correlations were found between DOC, DON and some nutrient indices, which together reflected soil condition and quality. It was hence essential to study DOC and DON in the study area. 2 Seasonal dynamics of DOC, DON, inorganic N, microbial biomass C and N were studied under Pinus tabulaeformis and Cercidiphyllum japonicum plantation. The results indicated that seasonal dynamics of soil DOC and DON under the two plantations performed similar change pattern, with the highest values in autumn. The seasonal dynamics of soil DOC and DON were mainly influenced by the litterfall. However, biotic factors such as soil microbial activities and abiotic factors such as precipitation and temperature also controlled the dynamics of soil DOC and DON. The seasonal dynamic of DON was different from that of NO3--N and NH4+-N, which showed that the behavioral differences between DON and inorganic nitrogen. And hence, it was proposed to include DON into soil N cycling in the study area. 3 Amino acid dynamics in Oa and topsoil (0-10 cm) under P. tabulaeformis and C. japonicum plantation were studied. The results showed that amino acid content in Oa was significantly higher than that in mineral soil. At each sampling time, significantly higher amino acid contents were found in P. tabulaeformis plantation than in C. japonicum plantation. The content of inorganic nitrogen was much higher than the content of amino acid in each sampling layer at each sampling time. After a 30-days laboratory incubation the content of amino acid was still lower than the content of inorganic nitrogen. The results implicated that the form of N absorbed by plants in these study sites were mainly inorganic nitrogen. 4 Usually needle litter is more resistant to decomposition, which leads to needle litter accumulation in pure coniferous stands and slows down the rate of nutrient circulation. By constructing microcosms with local shrubland soil and containing the four single-species (P. tabulaeformis, P. radiata, C. japonicum, Ostryopsis davidiana) litters, the decomposition rates and related C and N dynamics of needle litters and broadleaved litters during the early stage were compared. The results showed that the decomposition rates of pine needles were lower than those of broadleaved litters, which descended C and N cycling processes. However, the presence of C. japonicum or O. davidiana litter into pine needles increased the decomposition rates of pine needles and also dramatically promoted C and N cycling processes. It should be appropriate for plantation managers to consider C. japonicum as an ameliorative species or remain O. davidiana in pine plantations to improve soil conditions and help maintain soil fertility. The laboratory incubation still showed that DOC and DON contents in all litter-amended treatments were significantly higher than no litter-amended treatment, which proved that litter could be a direct source of DOM in soils. Different species litters induced different soil DOC and DON contents, which correspondingly changed over time. DOC and DON contents in mixed litter treatments were higher than those in pine needle litter treatments. As a major soluble N pool, DON developed a different changing pattern over time compared with inorganic N and played a role of interim N pool in soil N cycling.

模拟增温对川西亚高山人工云杉林土壤碳含量和土壤呼吸的影响

全球气候变化已经成为不争的事实，其中全球变暖是近年来国内外的研究热点之一。土壤碳库作为陆地生态系统最大的碳库，气温升高必然会导致一系列的土壤碳储量和碳通量的变化，这些微小的变化又可能导致大气CO2浓度的变化并强化这种变暖的趋势。目前，土壤碳循环对温度升高的响应仍然是陆地碳循环研究最缺乏的部分，对土壤有机碳动态变化的研究仍存在着很大的不确定性与争议。四川西部的亚高山人工针叶林是青藏高原东部高寒林区的重要组成部分，是研究全球变化对森林生态系统影响的关键地区和重要森林类型。本研究通过采用原位人工模拟增温装置（Open-top chambers，OTCs）对川西米亚罗60年人工云杉林土壤实施增温，研究高海拔地区森林，尤其是人工森林系统下的土壤有机碳 含量、土壤呼吸及土壤酶活性对温度升高的响应。结果表明： 1. 增温处理的660天（2005年11月至2007年9月）期间，增温条件下的平均气温和土壤平均温度分别比对照提高0.43 ℃和0.27 ℃；0~10 cm土壤含水量在增温的不同时期均有不同程度的降低。 2. 土壤蔗糖酶、蛋白酶和脲酶活性在温度升高的不同阶段均有不同程度的提高。在增温处理300天（2006.09）、540天（2007.05）、600天（2007.07）和660天（2007.05）后，0~10 cm层的蔗糖酶活性分别比对照提高了36.36%（P<0.05）、24.31%、14.54%（P<0.05）和7.22%，脲酶活性分别提高了12.90%、24.19%（P<0.01）、34.48%（P<0.05）和14.64%(P<0.05)，蛋白酶活性分别提高了31.37%、1.99%、3.70%和17.80%。10~20 cm层的土壤酶活性也均有不同程度的提高，但均没有显著差异。蔗糖酶、脲酶和蛋白酶活性均呈现出随土层加深而减弱的趋势。 3. 土壤过氧化氢酶和多酚氧化酶活性在增温的第1年内均有不同程度的提高，但在增温的第2年内比对照有所降低。增温300天后（2006.09），过氧化氢酶和多酚氧化酶在0~10 cm层分别比对照增加3.76%和49.25%（P<0.05），10~20 cm层分别增加了5.54%和29.67%。在增温的第2年内，增温540天（2007.05）、600天（2007.07）和660天（2007.09）后，0~10 cm层的过氧化氢酶活性分别比对照降低了27.70%（P<0.05）、4.34%和1.47%，多酚氧化酶活性分别降低了5.86%、11.76%（P<0.05）和7.47%。增温的第2年内，10~20 cm层的过氧化氢酶和多酚氧化酶活性也均有不同程度的降低，但差异均未达到显著水平。不同土层之间相比较，过氧化氢酶活性随土层加深而降低，多酚氧化酶活性随土层加深而增加。 4. 土壤有机碳和有机质在增温的不同阶段，含量比对照均有所降低；且随增温时间的延长，降低的幅度下降。0~10 cm层的土壤有机碳和土壤有机质在增温300天（2006.09）、540天（2007.05）、600天（2007.07）和660天（2007.09）后分别降低了8.69%、4.35%、3.80%和2.44%，差异均未达到显著水平。土壤全氮含量在增温后与对照相比无明显的增加或者降低趋势。增温条件下的土壤C/N比与对照相比有所降低，但在增温各阶段的差异均不显著。10~20 cm层的有机碳、有机质和C/N比也有不同程度的降低趋势，但差异均不显著。不同土层之间相比，0~10 cm层的有机碳、有机质、全氮含量和C/N比均高于10~20 cm层，呈现出随土层加深而降低的趋势。 5. 土壤呼吸速率在增温第1年内，与对照相比明显提高，但在增温处理2年后，与对照相比无显著变化。增温300天（2006.09）和360天（2006.11）后分别提高了13.32%和21.17%，差异显著。增温处理540天（2007.05）到660天（2007.09）期间，与对照相比，不仅没有明显的提升，反而有些月份比对照有所降低，对温度升高的敏感性降低，呈现出对温度升高的适应性。土壤呼吸的日呼吸速率呈现单峰曲线形式，在14:00~20:00期间达到最大值，在4:00~10:00期间具有最低值。土壤呼吸的季节变化，呈现出与外界环境温度相一致的趋势，在7月份（夏季） 最高，11月份（冬季）最低。土壤呼吸与2 cm土壤温度、5 cm土壤温度和空气温度均呈极显著指数相关，与0~10 cm土壤含水量呈线性相关，相关性达到显著水平，但低于土壤呼吸与温度的相关性。 The past century has seen a marked increase in atmospheric carbon dioxide concentrations and a concomitant warming that has drawn scientific attention to the link between global carbon stocks and climate change. In particular, the decomposition and turnover of soil organic matter is recognised as an important determinant of carbon driven climate change. The slightly variation in soil organic carbon will result in the increase of atmospheric carbon dioxide concentrations and reinforce the tendency of warming. The experiment was conducted in Subalpine coniferous forest in western Sichuan province. Subalpine coniferous forest in western Sichuan was a important part of eastern Qinghai-Tibetan Plateau, which play a important role in reseaching the sensitivity of forest ecosystem to climate change. To investigate the effects of elevated temperature on soil organic carbon content, soil respiration rates, and soil enzyme activities in subalpine Picea asperata plantations, a esimulated warming measure was applied with Open-top chambers. The results were as followed: 1) During the period from Nov. 2005 to Sep. 2007, mean air temperature and soil temperature were respectively 0.43℃ and 0.27℃ the ambient higher. Soil water content decreased to different exent in different months in warmed plots than in unwarned plots at depth of 0-10 cm. 2) In general, elevated temperature enhanced the soil enzyme activities of invertase, protease, and urease. In the first year of warming—after 300 days’ treatment (in Sep,2006), the activities of invertase, protease, and urease increased by 36.36%, 12.90% and 31.37% respectively at the depths of 0-10 cm，among which the activity of invertase reached statistic significance. In the second year of warming, invertase activity increased by 24.31% after 540 days’ treament (in May, 2007), 14.54% after 600 days’ treament (in Jul, 2007) and 7.22% after 660 days’ treatment (in Sep, 2007) at the depths of 0-10 cm, and the differences in July and Septemmber were statistically significant. Elveated temperature also increased the activity of urease in the second year of warming and had significant effects in May and July. The activity of protease in warmed plots was also higher than in unwarmed plots at depths of 0-10 cm, but there was no significant difference. Elevated temperature had no significant effects on all soil enzyme acitivities at the depths of 10-20 cm in the first and sencond year. The values of above-mentioned soil enzyme all decreased with soil layers. 3) Eleavted temperature enhanced the activities of catalase and polyphenol oxidase in the first year of warming while they turned out downtrend in the second year. The activity of catalase increased by 3.76% and 5.54% at depths of 0-10 cm and 10-20 cm respectively in the first year—after 300 days’ warming (in Sep, 2006), the differences of which had no statistical significance. The activity of polyphenol oxidase was significantly increased by 49.25% at depths of 0-10 cm and not significantly increased by 29.67% at depths of 10-20 cm after 300 days’ warming. In the second year of warming, the catalase activity was significantly decreased by 27.70% after 540 days’ treament (in May, 2007) and not significantly decreased by 4.34% and 1.47% after 600 days’ (in Jul, 2007) and 660 days’ treament (in Sep, 2007) respectively. The activities of catalase and polyphenol oxidase at depths of 10-20 cm were decreased to different extent, but there was no significant difference. Catalase activity stepped down with soil layers while polyphenol oxidase activity stepped up. 4) Increased temperature in both the first year and the second year resulted tendency of decrease in the contents of soil organic carbon and soil organic matter, and C/N ratios at soil depths of 0-10 cm and 10-20 cm. However, with the prolonged warming, the tendency of decrease gradually tapered off and the extent of decrease in the second year of experiment were lower than that in the first year. The contents of soil organic carbon and soil organic matter were all decreased 8.69% by warming in the first year and dcreased 4.35%, 3.80% and 2.44% in May, July and September of the second year, but no significant difference were found. The C/N ratios increased 8.52% in the first year of warming and had less increment in the second year, all of which were not statistical significant. Eleveated temperature had no obvious effect on the content of tatol N in two year consecutive warming experiment. The contents of soil organic carbon and soil organic matter, total N and C/N ratios all had the tendency of dcreasing with soil layers. 5) Soil respiration rates were significantly enhanced by 13.32% and 21.17% after 300 days’ (in Sep, 2006) and 360 days’ (in Nov, 2006) treament in the first year of warming, but the same showed no obvious difference in the second year of treatment, which was assumed the adaptability of soil respiration with a certain heightened temperature. Diurnal soil resspiration showed a daily variation with a minimum value between 4:00 and 10:00 h and a maximum value between 14:00 and 20:00 h, coinciding with the minimum and maximum values of soil temperature at 2 cm. Soil respiration rates exhibited a pronounced seasonal variation with minimum values in Novmber and a maximum value in July, approximately coinciding with the seasonal variation of air and soil temperature. An exponential function provided the best fit for soil respiration with temperature while a quadric equation was used to estimate the effect of soil moisture on soil respiration, which were all significantly correlated. Soil respiraion rate was more highly correlated with the soil temperature than soil moisture.

重离子诱导人舌鳞癌细胞凋亡和Bax/Bcl-2蛋白表达的变化

In order to investigate the effect of carbon ion irradiation on apoptosis and Bax/Bcl-2 expression inhuman tongue carcinoma cells, exponentially growing human tongue carcinoma cells (Tb) cultured in vitro were irradiated with 0, 0.5, 1.0, 2.0 or 4.0 Gy of 12C6+ ions respectively. Survival rate of irradiated cells at various doses were measured by MTT assay. The nucleus changes of apoptosis and necrosis of cells stained by Hochest/PI were observed through fluorescence microscope. The cell cycle changes were detected by flow cytometry (FCM). The expressions of Bax and Bcl-2 were detected by Western blot analysis. The results show that the viability of Tb cells decreases gradually with increment of irradiation doses of carbon ions. The proportions of apoptosis cells in the irradiated groups are significantly higher than those in the control group. There is a positive correlation between irradiation doses and retardation strength in G2 /M phase at 24 h after irradiation (P<0.05). And the expressions of Bax and bcl-2 are significantly up-regulated and down-regulated respectively by 12C6+ ion irradiation. It can be concluded from above that cell apoptosis induced by heavy ion with high-LET may be mediated through the Bax/Bcl-2 expression pathway. 探讨重离子辐照对人舌鳞癌Tb细胞的凋亡及Bax/Bcl-2蛋白表达的影响。采用0、0.5、1.0、2.0、4.0 Gy重离子束辐照人舌鳞癌 Tb 细胞，应用 MTT 法检测细胞存活，流式细胞技术检测细胞周期变化，Hoechst33258/PI 复染法观察 Tb 细胞凋亡形态，并采用 Western-blot 法检测 Bax/Bcl-2 蛋白表达情况。结果发现，Tb细胞经12C6+离子束辐照后存活率显著下降，呈剂量依赖性的生长抑制；Tb细胞呈现蓝色荧光浓集成团的凋亡形态，且凋亡比例随辐照剂量增加；G2/M 期细胞百分数随照射剂量增加而增加（P＜0.05） 。Western-blot结果显示 Bax 蛋白表达水平随辐照剂量逐渐上升，但在 4 Gy 组其表达不再增高，Bcl-2 蛋白在 1.0、2.0、4.0 Gy组随剂量增大呈下降趋势。以上结果提示重离子束辐照对 Tb 细胞有抑制作用，Bax/Bcl-2 蛋白表达是重离子治癌的机制之一。

重离子诱导人舌鳞癌细胞凋亡和Bax/Bcl-2蛋白表达的变化

探讨重离子辐照对人舌鳞癌Tb细胞的凋亡及Bax/Bcl-2蛋白表达的影响。采用0、0.5、1.0、2.0、4.0Gy重离子束辐照人舌鳞癌Tb细胞,应用MTT法检测细胞存活,流式细胞技术检测细胞周期变化,Hoechst 33258/PI复染法观察Tb细胞凋亡形态,并采用Western-blot法检测Bax/Bcl-2蛋白表达情况。结果发现,Tb细胞经12C6+离子束辐照后存活率显著下降,呈剂量依赖性的生长抑制;Tb细胞呈现蓝色荧光浓集成团的凋亡形态,且凋亡比例随辐照剂量增加;G2/M期细胞百分数随照射剂量增加而增加(P<0.05)。Western-blot结果显示Bax蛋白表达水平随辐照剂量逐渐上升,但在4Gy组其表达不再增高,Bcl-2蛋白在1.0、2.0、4.0Gy组随剂量增大呈下降趋势。以上结果提示重离子束辐照对Tb细胞有抑制作用,Bax/Bcl-2蛋白表达是重离子治癌的机制之一。

热峰模型在聚碳酸酯非晶化潜径迹中的应用

为了描述快重离子在聚合物中的潜径迹行为 ,用不同能量的快重离子 (1 15 8GeVFe56 ,1 75 5GeVXe1 36 及 2 6 36GeVU2 38)辐照叠层半结晶聚碳酸酯膜 (MakrofolKG型 ) ,结合x射线衍射测量技术 ,在较宽的电子能损 (1 9— 17 1keV nm)和离子注量 (5× 10 1 0 — 3× 10 1 2 cm- 2 )范围研究了离子在半结晶聚碳酸酯中引起的非晶化过程 .应用径迹饱和模型假设 (损伤过程只发生在面积为σ的柱形径迹内 ) ,分别给出了Fe,Xe和U离子在不同电子能损下辐照聚碳酸酯时的平均非晶化径迹半径 .用热峰模型对实验结果进行了检验 ,结果表明Szenes的热峰模型较好地描述了离子在聚合物中的潜径迹行为 .

关于强流ECR质子源氢等离子体发射光谱的诊断研究；OES diagnostics of H_2 plasma in an intense ECR proton source

本文通过发射光谱诊断方法,用H_2等离子体的辐射碰撞模型对连续溃入的微波功率和全永磁磁场约束下产生高密度的H_2等离子体进行光谱诊断,计算出一定放电条件下(微波功率200-700 W,压强0-2 Pa)H~+的密度为1010-1011 cm~(-3),另外讨论了实验中观察到的Balmer系氢原子发射光谱强度随放电条件的变化规律。

Dissociative recombination of the acetaldehyde cation, CH3CHO+

The dissociative recombination of the acetaldehyde cation, CH3CHO+, has been investigated at the heavy ion storage ring CRYRING at the Manne Siegbahn Laboratory in Stockholm, Sweden. The dependence of the absolute cross section of the reaction on the relative kinetic energy has been determined and a thermal rate coefficient of k(T) = (1.5 +/- 0.2) x 10(-6) (T/300)(-0.70 +/- 0.02) cm(3) s(-1) has been deduced, which is valid for electron temperatures between similar to 10 and 1000 K. The branching fractions of the reaction were studied at similar to 0 eV relative kinetic energy and we found that breaking one of the bonds between two of the heavy atoms occurs in 72 +/- 2% of the reactions. In the remaining events the three heavy atoms stay in the same product fragment. While the branching fractions are fairly similar to the results from an earlier investigation into the dissociative recombination of the fully deuterated acetaldehyde cation, CD3CDO+, the thermal rate coefficient is somewhat larger for CH3CHO+. Astrochemical implications of the results are discussed.

DISSOCIATIVE RECOMBINATION OF PROTONATED PROPIONITRILE, CH3CH2CNH+: IMPLICATIONS FOR TITAN'S UPPER ATMOSPHERE

The dissociative recombination of protonated propionitrile, CH3CH2CNH+, has been investigated at the heavy ion storage ring, CRYRING, at the Manne Siegbahn Laboratory, Stockholm University, Sweden. The thermal rate coefficient has been deduced to follow k(T) = (1.5 +/- 0.2) x 10(-6) (T/300)(-0.76) (+/-) (0.02) cm(3) s(-1) for electron temperatures ranging from similar to 10 to similar to 1000 K. Measurements of the branching fractions were performed at similar to 0 eV relative kinetic energy. It has been found that in 43% +/- 2% of the reactions the four heavy atoms remain in the same product fragment. An equal portion of the reactions leads to products where one of the heavy atoms is split off from the other three and 14% +/- 1% result in a breakup into two heavy fragments containing two heavy atoms each. We discuss the significance of the data to Titan's upper atmosphere.

Experimental studies of the dissociative recombination of CD3CDOD+ and CH3CH2OH2+

Aims. We determine branching fractions, cross sections and thermal rate constants for the dissociative recombination of CD3CDOD+ and CH3CH2OH2+ at the low relative kinetic energies encountered in the interstellar medium. Methods. The experiments were carried out by merging an ion and electron beam at the heavy ion storage ring CRYRING, Stockholm, Sweden. Results. Break-up of the CCO structure into three heavy fragments is not found for either of the ions. Instead the CCO structure is retained in 23 +/- 3% of the DR reactions of CD3CDOD+ and 7 +/- 3% in the DR of CH3CH2OH2+, whereas rupture into two heavy fragments occurs in 77 +/- 3% and 93 +/- 3% of the DR events of the respective ions. The measured cross sections were fitted between 1-200 meV yielding the following thermal rate constants and cross-section dependencies on the relative kinetic energy: sigma(E-cm[eV]) = 1.7 +/- 0.3 x 10(-15)(Ecm[eV])(-1.23 +/- 0.02) cm(2) and k(T) = 1.9 +/- 0.4 x 10(-6)(T/300)-0.73 +/- 0.02 cm(3) s(-1) for CH3CH2OH2+ as well as k(T) = 1.1 +/- 0.4 x 10(-6)(T/300)(-0.74 +/- 0.05) cm(3) s(-1) and s(Ecm[eV]) = 9.2 +/- 4 x 10(-16)(Ecm[eV])-1.24 +/- 0.05 cm(2) for CD3CDOD+

环境样品的低水平放射性测量

环境样品中的低水平放射性测量在环境放射性现状调查和探矿中有广泛的应用。本论文对CSR环境水样品的放射性利用γ能谱方法进行了测量；对铀矿坑水样铀电沉积层用红外谱图和扫描电镜进行了表征，并且对其进行了α能谱测量；对便携式钾40探测器样机在不同条件下进行了测试。 CSR环境水样品经过采集，静置，预处理和封装，用高纯锗探测器在低本底大铅室内对水样品进行了测量，每个样品测量86400秒。标准源由中国原子能科学研究院提供，用相对比较的方法，给出样品中天然铀、钍、镭和钾的放射性活度。测量结果表明，CSR环境水样品中的放射性处于兰州地区本底水平，在样品中没有发现人工放射性核素。 对铀矿坑水样中的铀进行离子交换化学分离，在0.8M的硫酸铵溶液中进行电沉积，电流密度为0.6A cm-2,pH值为2.5；和同样条件下电沉积的硝酸铀酰进行对比，并对二者分别作了红外光谱、扫描电镜、元素分析以及α能谱测量，红外谱上铀酰离子的反对称伸缩振动峰在887cm-1附近，电沉积在不锈钢片上的铀主要以铀酰离子水合物的形式存在，电沉积层中铀化合物形式为UO2(OH)2•xNH3•yH2O或者UO2(OH)2-x•(ONH4)x•yH2O。扫描电镜照片显示电沉积层均匀，没有成团现象出现。α谱表明电沉积层中铀的同位素主要是238U和234U，相应的α能量峰分别为4198keV和4773keV。 对研制的40K探测器样机在屏蔽和未加屏蔽的条件下进行了测试，测量配制的40K标准源，绘出标准曲线，在同样的条件下测量未知钾含量的样品，根据峰面积计算40K的含量。研制的40K探测器样机基本满足样品中钾含量测量的需要，在野外测量时，在一定程度上受本底的影响

薄膜硅材料的重离子辐照改性研究

选择具有重要应用价值的纳米晶硅及非晶硅薄膜材料，对比研究了快重离子辐照薄膜Si材料所引起的辐照效应，主要有如下工作： 1) 用等离子增强化学气相沉积法(PECVD)以及常压化学气相沉积法(APCVD)在玻璃衬底上制备纳米晶硅薄膜(nc-Si)与非晶硅(a-Si)薄膜。制备的nc-Si和a-Si薄膜的厚度分别为∼200 nm和∼400 nm。 2) 室温下，用94 MeV的Xe离子辐照nc-Si和a-Si薄膜以及单晶硅(c-Si，晶向(100)，电阻率0.001 Ω·cm，作为对比样品)，辐照量分别为1.0×1011、1.0×1012 和1.0×1013 ions/cm2。所有样品均在室温下用UV/VIS/NIR光谱仪、Raman谱仪进行检测分析，对比研究纳米晶、非晶、单晶硅样品的光学性能及结构的变化。 3) 通过UV/VIS/NIR谱，我们得到了不同结构硅材料的光学带隙值及折射率随辐照量的变化规律。通过分析硅材料辐照前后Raman谱的变化，讨论了不同晶体结构的影响。 4) 结合UV/VIS/NIR与Raman结果初步讨论了硅材料结构影响辐照效应的机理。对于a-Si薄膜样品，辐照可能引起了样品局域的再结晶。对于nc-Si薄膜样品，Xe离子辐照先引起nc-Si晶粒的破碎，使样品出现非晶化过程，然后再遵从a-Si薄膜样品中离子辐照效应变化规律

非晶态合金的表面辐照效应研究

本工作用120Kev的He~+离子对非晶态Ni_(60)Nb_(40)、Fe_(40)Ni_(38)Mo_4B_(18)、Fe-Ni-B合金样品进行了辐照，辐照剂量为1.6、2.0、2.5，3.0 * 10~(18)/cm~2四种。借助X射线衍射扫描电子显微镜（SEM），内转换电子穆斯堡文谱（CEMS）等方法对辐照前后的样品进行了分析。X射线衍射结果表明在冷却靶的辐照条件下，样品辐照前后的非晶状态来改变，但辐照产生了原子的重排。SEM研究发现：表面发论的形成须一定的临界剂量对于Ni_(60)N_(240)，所需临界剂量最高；随剂量的增加，在所研究的剂量范围内，发论大小增大且来观察到表面发论的破裂与剥学；对不同组织的非晶合金，其发论程度稍有不同；辗压减药不影响材料的发论性质；表面结构的粗糙有助于降低发论程度；晶化样品，发论程度的显加剂。CEMS分析指出；辐照使结构的天度增加，有效的平均原子间距减小；因辐照导致原子的重新溶合使CSRO降低；随辐照首先的缺陷周围自旋取向及急进的应力源的变化。磁各向异性发生了变化

IBM-2的有效玻色子数及数值计算

本文简单介绍了原子核集体运动的代数模型－IBM－2，评述了近年来的研究结果；提出了一种确定有效玻色子数的半经验方法，并且提出接近半满壳处偶偶核的有效玻色子数饱和的概念（50～82大壳饱和值为6，82～126大壳饱和值为7，126～184（？）大壳饱和值为8），把稀土区偶偶核的E2和M1之间的关联性及它们的饱和性解释为有效玻色子数的饱和，E_2~+的饱和解释为半满壳附近中子质子四极四极相互作用远大于对力的结果；并把本文关于有效玻色子数的结果用于Q_o和E_2~+系统学，F旋多重态和数值计算中，结果比过去有较大改进；本文还给出了哈密顿量参数的改变对能谱影响的经验规律，并用NPBOS程序计算了~(132-150)Nd偶偶核同位素，~(134)Ba等，对它们的状态特别是其中的混合对称态进行了细致的讨论，能谱和电磁跃迁计算结果与实验数据吻合较好，本文还计算了~(142)Ce的混合比并与实验进行了比较；此外，本文还通过具体的核对IBM－2数值计算参数g_(πv)~((1)) (1=0，2，4)进行了讨论，对M1跃迁算子的两体项作了初步的分析

氦离子辐照非晶态合金的表面损伤研究

本文研究了室温下氦离子辐照非晶态合金(Co94Fe4Cr2)78Si8B14、Fe37.5Ni37.5B25、Fe18.5Ni55.5B26、Fe77Ni5B18、Fe61.5Ni20.5B18、Ni78B14Si8、Fe77B16Si5Cr2、Ni60Nb40、Cu35Zr65、Cu43Ti57等的表面损伤。氦离子能量为40Kev和60Kev，平均通量密度分别为4.2μ A/cm~2和3.2μA/cm~2，总剂量为1.0*、1.5*、2.0*、2.5*、3.0*、4.0 * 10~(18)Ions/cm~2。用扫描电子显微镜观测了辐照后样品的表面形貌。实验结果表明：非晶态合金的辐照效应与材料的种类有关，金属／金属非晶合金的临界剂量（约1.0～1.5 * 10~(18)/cm~2）高于金属／类金属非晶合金的临界剂量（约0.5～1.0 * 10~(18)/cm~2）；不同组元的同类材料之间的损伤不同；不同组元比分的同类材料之间的损伤也有所差异。随总剂量的增加，损伤方式（发泡、层离、剥落）是重复出现的，从1.0*到4.0 * 10~(18)/cm~2共产生三代发泡，两代层离，并且损伤呈周期性变化的趋势。随能量的增加损伤程度减弱。剥落是周边型的，由发泡内气体压力驱动。根据发泡皮的厚度与入射离子的平均投影射程相近，层离层的厚度大于平均投影射程2～3倍这一新的实验现象，认为发泡由气泡间聚结机制形成，层离由气泡间破裂机制形成