土壤有机物料碳矿化进程及活性碳库变化规律

摘 要 在2005.8～2006.8期间，用埋袋法研究了1年中玉米秸、稻秸、苜蓿、鸡粪、猪粪、玉米秸-鸡粪-猪粪、苜蓿-鸡粪-猪粪中有机碳的矿化分解残留率动态变化、C/N比值动态变化、土壤中溶解性有机碳含量动态变化、土壤中微生物量有机碳含量动态变化、土壤易氧化有机碳含量动态变化、土壤轻组有机碳含量动态变化、土壤颗粒有机碳含量动态变化。 结果表明，物料中有机碳矿化进程可区分为快、慢两个阶段，大C/N比值有机物料(玉米秸、稻秸)在试验初期的分解比低C/N比值有机物料的分解迅速，至试验结速其残留率也较多。C/N比值的下降速率也可区分为快、慢两个阶段，试验结束时各种有机物料残留物的C/N比趋于稳定；低C/N有机物料(苜蓿、鸡粪、猪粪、玉米秸-鸡粪-猪粪、苜蓿-鸡粪-猪粪)残留物的C/N比值接近土壤腐殖质C/N比，完成其腐殖化过程；高C/N有机物料(玉米秸、稻秸)残留物的C/N比值处于适宜微生物活动的25左右，利于增加土壤有机质、培肥土壤。 添加有机物料能显著增加DOC、土壤微生物量碳、土壤易氧化有机碳、土壤轻组有机碳、土壤颗粒有机碳的含量；有机物料分解过程中不同处理DOC的变化、土壤微生物量碳的变化、土壤易氧化有机碳的变化、土壤轻组有机碳的含量变化、土壤颗粒有机碳的变化均与有机物料的组成及C/N比值以及由此引起的有机物质不同的分解残留率有关。 因此，土壤有机质需要不断的更新，这就是我们所提倡的持续不断的秸秆还田的意义所在。

HIRFL设备巡检报警与束流状态显示系统设计

在Visual C++环境下编制了一个用于HIRFL设备自动巡检和报警的应用。通过网络自动读取和显示当前所有受计算控制的设备（电源设备）状态，遇见设备故障时自动发出警报。具有响应用户的中断请求，选择或屏蔽设备，更改设备误差，自动存储故障记录等功能。在Visual C++环境下编制了另一个用于HIRFL束流状态显示的应用软件。通过网络自动读取和分析受计算机控制的束诊设备的参数，并实时显示相应的束流位置或状态。具有直观显示束流当前位置，动态描述束流走向等功能。这两个程序在功能上能够满足HIRFL设备自动巡检和报警以及束流状态显示系统研制的任务书要求。

Pressure drops of single and two-phase flows through T-type microchannel mixers

In this paper, preliminary experimental results are presented on pressure drop characteristics of single and two-phase flows through two T-type rectangular microchannel mixers with hydraulic diameters of 528 and 333 mum, respectively. It is shown that both N-2 and water single-phase laminar flows in microchannels, with consideration of experimental uncertainties, are consistent with classic theory, if additional effects, such as entrance effects that will interfere with the interpretation of experimental results, are eliminated by carefully designing the experiments. The obtained pressure drop data of N-2-water two-phase flow in micromixers are analyzed and compared with existing flow pattern-independent models. It is found that the Lockhart-Martinelli method generally underpredicts the frictional pressure drop. Thereafter, a modified correlation of C value in the Chisholm's equation based on linear regression of experimental data is proposed to provide a better prediction of the two-phase frictional pressure drop. Also among the homogeneous flow models investigated, the viscosity correlation of McAdams indicates the best performance in correlating the frictional pressure drop data (mean deviations within +/-20% for two micromixers both). Finally it is suggested that systematic studies are still required to accurately predict two-phase frictional performance in microchannels. (C) 2004 Elsevier B.V. All rights reserved.

Luminescent and Mesoporous Europium-Doped Bioactive Glasses (MBG) as a Drug Carrier

Luminescent and mesoporous europium-doped bioactive glasses (MBG:Eu) were successfully synthesized by a two-step acid-catalyzed self-assembly process combined with hydrothermal treatment in an inorganic-organic system. The obtained MBG was performed as a drug delivery carrier to investigate the drug storage/release properties using ibuprofen (IBU) as a model drug. The structural, morphological, textural and optical properties were well characterized by X-ray diffraction (XRD), transmission electron microscopy (TEM), N-2 adsorption/desorption, and photoluminescence (PL) spectra, respectively. The results reveal that the MBG exhibit the typical ordered characteristics of the hexagonal mesostructure. This composite shows sustained release profile with ibuprofen as the model drug. The IBU-loaded samples still show red luminescence of Eu3+ (D-5(0)-F-7(1, 2)) under UV irradiation, and the emission intensities of Eu3+ in the drug carrier system vary with the released amount of IBU, thus making the drug release be easily tracked and monitored by the change of the luminescence intensity.

Magnetic Mesoporous Silica Spheres for Drug Targeting and Controlled Release

Magnetically functionalized mesoporous silica spheres with different size (average diameter, A.D.) from 150 nm to 2 mu m and pore size distribution were synthesized by generating magnetic FexOy nanoparticles onto the mesoporous silica hosts using the sol-gel method. The X-ray diffraction (XRD), field emission scanning electron microscope (FESEM), N-2 adsorption/desorption results show that these composites conserved regular sphere morphology and ordered mesoporous structure after the formation of FexOy nanoparticles. XRD and X-ray photoelectron spectroscopy (XPS) analysis confirmed that the FexOy generated in these mesoporous silica hosts is mainly composed of gamma-Fe2O3. Magnetic measurements reveal that these composites with different gamma-Fe2O3 loading amounts possess super-paramagnetic properties at 300 K, and the saturation magnetization increases with increasing Fe ratio loaded.

Synthesis and characterization of magnetic FexOy@SBA-15 composites with different morphologies for controlled drug release and targeting

Magnetic functionalization of the ordered mesoporous SBA-15 (SiO2) aggregate blocks and rice grain-like particles were realized by using a sol-gel method, resulting in the formation of FexOy@SBA-15 composite materials. The X-ray diffraction (XRD), N-2 adsorption/desorption, and transmission electron microscopy (TEM) results show that these composites conserved ordered mesoporous structure after the formation of FexOy nanoparticles in the pores and on the outer surface of SBA-15. It was confirmed by the XRD and X-ray photoelectron spectroscopy (XPS) analysis that the FexOy generated in these mesoporous silica hosts is mainly composed of gamma-Fe2O3. Magnetic measurements reveal that these composites possess superparamagnetic properties at 300 K. The saturation magnetization of these composites increased with the increasing loading amount of gamma-Fe2O3. These composites, which possess high surface area and high pore volume, show magnetic response sufficient for drug targeting in the presence of an external magnetic field.

人参茎叶挥发油中倍半萜烯化合物的分离与鉴定

对人参茎叶挥发油的有效成分进行分离纯化 ,利用薄层层析 (TL C)、红外光谱 (IR)、气相色谱 (GC)、气相色谱 -质谱 (GC/MS)联机技术从该挥发油中分离鉴定 6个倍半萜烯类化合物 .

稀土与L-组氨酸L-谷氨酸三元配合物的pH电位法研究

报道了在模拟生理条件 ( 37℃ ,c =0 .15mol· L-1Na Cl)下用精密 p H电位法对 15种稀土元素与 L-组氨酸及 L-谷氨酸溶液体系三元配合物稳定常数的测定结果 ,实验数据处理用程序Miniquad- 82 A完成 ,玻璃电极的选择及校正用 Magec程序完成 .结果表明在该三元体系中普遍存在 3种类型的酸式配合物 ( 1111,1112及 1113型 ) ,且每一类型配合物的稳定常数相差较小.

High-pressure synthesis of gadolinium indium gallium garnet

High-pressure synthesis of garnet Gd3In2Ga3O12 is reported. It was found that the pressure-temperature region for the synthesis of Gd3In2Ga3O12 can be expressed as T(degrees C) < 2350-250P(GPa), and high pressure greatly reduced the reaction time. It was also found that the garnet Gd3In2Ga3O12 decomposed to GdGaO3 and In2O3 under 3.5 GPa and 1650 degrees C, and this process was accompanied by an increasing density of the products and an increasing coordination number for Ga3+ (4 to 6).

海洋微藻产生溶解有机物及东海溶解有机物三维荧光特征研究

本文通过胶州湾围隔实验、微藻培养实验研究了海洋微藻产生溶解有机物的三维荧光特性，并初步利用经验正交函数对三维荧光光谱图进行了主成分分析，通过东海取样研究了东海荧光溶解有机物的时空分布特征，并对荧光溶解有机物的来源进行了分析。得到了一些初步结论： 胶州湾围隔实验中不同营养盐培养结果表明浮游植物可产生类蛋白和类腐殖质荧光，类蛋白荧光峰由类酪氨酸(tyrosine-like)荧光峰和类色氨酸(tryptophan-like)荧光峰组成，主要位置为Exmax/Emmax=270nm/290~310nm，Exmax/Emmax= 270~290/320~350的荧光峰强度比较弱；在Exmax/Emmax=250~260/380~480nm(A峰)、Exmax/Emmax=310~320/380~420nm(C峰)和Exmax/Emmax=330~350/420~480nm(M峰)位置均出现零散的类腐殖质荧光峰，其中以A峰为主。类酪氨酸荧光强度明显高于类腐殖质荧光强度。浮游植物量降低时，类酪氨酸荧光强度与叶绿素a浓度呈明显的负相关。硅藻和甲藻产生的类酪氨酸和类色氨酸荧光强度之间具有较好的相关性，两者来源相似, 并且甲藻与硅藻相比能够产生更多的类蛋白荧光物质。不同环境下类腐殖质混合物的组分比例不同，甲藻生长环境下相对于硅藻具有较低的A:C比值。 在实验室培养中肋骨条藻（Skeletonema costatum）、塔玛亚历山大藻（Alexandrium tamarense）、微小亚历山大藻（Alexandrium mimutum）、锥状斯氏藻（Scrippsiella trochoidea）、东海原甲藻（Prorocentrum donghaiense）及海洋原甲藻（Prorocentrum micans）的实验结果表明，微藻在生长过程中产生出荧光溶解有机物，中肋骨条藻为代表的硅藻主要产生类腐殖质荧光物质，而甲藻在指数增长期主要产生类蛋白荧光物质。进入消亡期后类蛋白荧光和类腐殖质荧光强度迅速增大，原因可能是衰老、死亡藻细胞的破碎释放出大量的荧光有机物质所致，此外还有细菌对非荧光有机物进一步降解。塔玛亚历山大藻、微小亚历山大藻、东海原甲藻及海洋原甲藻的类蛋白荧光强度在消亡后期由于细菌降解或光降解等因素而降低。同属微藻产生的荧光物质相似，例如塔玛亚历山大藻与微小亚历山藻、东海原甲藻与海洋原甲藻，但具体荧光峰位置有所不同。利用经验正交函数能够对三维荧光光谱谱图进行主成份分析。 在利用三维荧光光谱法研究长江口海域台风前后不同站位荧光溶解有机物荧光特性及分布特征的结果表明，长江口海区主要的荧光溶解有机物荧光峰为T峰、S峰和A峰。风前和风后的类色氨酸分别来源于相似物质。风前，在表层浮游植物能够产生类蛋白荧光物质，而底层类蛋白荧光物质不受浮游植物的影响，长江冲淡水能够带来部分类蛋白荧光物质；表层的类腐殖质不受浮游植物的影响，而底层的浮游植物在降解过程中能够产生一部分类腐殖质，并且长江冲淡水对表层和底层的类腐殖质来源均有很大贡献。风后，表层的类色氨酸与叶绿素a浓度不呈相关性，而底层却呈正相关，另外表层和底层的类色氨酸均受到长江冲淡水的影响；表层和底层的类腐殖质与叶绿素a均没有相关性，但受陆源影响显著，长江冲淡水能带来类腐殖质。

Diet shift of upland buzzards (Buteo hemilasius): evidence from stable carbon isotope ratios

We measured the stable carbon isotope ratios for muscle of the upland buzzards (Buteo hemilasius), plateau pika (Ochotoma curzoniae), root vole (Microtus oeconomus), plateau zokor (Myospalax fontanierii) and passerine bird species at the Haibei Alpine Meadow Ecosystem Research Station (HAMERS), and provided diet information of upland buzzards with the measurement of stable carbon isotopes in tissues of these consumers. The results showed that δ~(13)C values of small mammals and passerine bird species ranged from -25.57‰ to -25.78‰ (n = 12), and from -24.81‰ to -22.51% (n = 43), respectively, δ~(13)C values of the upland buzzards ranged from -22.60‰ to -23.10‰ when food was not available. The difference in δ~(13)C values (2.88‰±0.31‰) between upland buzzards and small mammals was much larger than the differences reported previously, 1‰-2‰, and showed significant difference, while 1.31‰±0.34‰ between upland buzzard and passerine bird species did not differ from the previously reported trophic fractionation difference of 1‰-2‰. Estimation of trophic position indicated that upland buzzards stand at trophic position 4.23, far from that of small mammals, i.e., upland buzzards scarcely captured small mammals as food at the duration of food shortage. According to isotope mass balance model, small mammals contributed 7.89% to 35.04% of carbon to the food source of the upland buzzards, while passerine bird species contributed 64.96% to 92.11%. Upland buzzards turned to passerine bird species as food during times of shortage of small mammals. δ~(13)C value, a useful indicator of diet, indicates that the upland buzzards feed mainly on passerine bird species rather than small mammals due to "you are what you eat" when small mammal preys are becoming scarce.

Characterization of photosynthetic pathway of plant species growing in the eastern Tibetan plateau using stable carbon isotope composition

The photosynthetic pathway of plant species collected at Menyuan, Henan, and Maduo sites, east of Tibetan Plateau, China, during the growing season were studied using stable carbon isotopes in leaves. The 232 samples leaves analyzed belonged to 161 species, 30 families, and 94 genera. The delta(13)C values (from -24.6 to -29.2 %o) indicated that all the considered species had a photosynthetic C-3 pathway. The absence of plant species with C-4 photosynthetic pathway might be due to the extremely low air temperature characterizing the Tibetan Plateau. The average delta(13)C value was significantly (p < 0.05) different between annuals and perennials at the three considered study sites. Hence the longer-lived species had greater water-use efficiency (WUE) than shorter-lived species, that is, longer-lived species are better adapted to the extreme environmental conditions of the Tibetan Plateau.

流体地球化学：成因、流动和流体-岩石相互作用及塔里木盆地实例研究

Geofluid in sedimentary basins is related to petroleum generation, migration, accumulation and preservation, and is a topic of geological frontier. By integrating the multi-discipline methods of petroleum geochemistry, sedimentology, hydrogeology, petroleum geology and experimental geochemistry, the thesis has carried out experiments of microcline dissolution in solutions with organic acids, crude oil, brines with high total dissolved solids (TDS), and has dealt with Al distribution between the crude oil and the brines after the experiments. Cases for study includes Central Tarim, Hetianhe Gas Field and Kucha forland basin with data containing fluid chemistry and isotopic compositions, thin sections of sandstones and carbonates, homogenization temperatures and salinities of fluid inclusions, isotopic compositions of bulk rock and autigenic minerals. The aims are to elucidate fluid origin and flow in the three areas, effect of hydrocarbon emplacement on diagenesis, and to show occurrence of microbe-mediated, and thermochemical sulfate reduction in the Tarim Basin. Microcline dissolution experiments show that after 100 hour, part of the dissolved Al distributes in the crude oil, and the Al concentrations in the crude oil rise when organic acids are added. The result can be used to explain that most oilfield waters in the Tarim Basin are characterized by less than 3mg/L Al. Crude oil added to the solutions can enhance microcline dissolution, which is also observed in the case - Silurian sandstones with early crude oil emplacement in the Central Tarim. Al and Si have higher concentrations in the experiments of oxalic acid than of acetic acid under the same pH conditions, suggesting that there exist Al-oxalate and Si-oxalate complexes. Presence of acetate can enhance the activity of Ca and Al, but Al concentrations have not been increased significantly due to formation of small Al-acetate complex during the experiments. Relationships between δD and δ~(18)O in conjunction with chemistry of oilfield waters show that the waters are evaporated connate waters, which subsequently mixed with meteoric water, and were influenced by water-rock interactions such as salt dissolution, dolomitization of calcite, albitization of feldspar. In the Hetianhe Gas Field where salt dissolution took place, δD and δ~(18)O values can be used to trace nicely meteoric water recharge area and flow direction, but TDS can not. Part of the waters have high TDS but very light δD and δ~(18)O. When combined with paleo-topography, or fluid potentials, meteoric water is suggested to flow eastward in the Hetianhe Gas Field, which is the same with the Central Tarim. Whist in the Kuche forland basin, meteoric water may have permeated Cambrian-Ordovician strata. Relationship between ~(87)Sr/~(86)Sr and 1/Sr can be used to indicate migration and mixing of brines from carbonate strata (low ~(87)Sr/~(86)Sr ratio but high Sr content), clastic strata (high ~(87)Sr/~(86)Sr ratio but low Sr content) and crystalline basement (high ~(87)Sr/~(86)Sr ratio and heavy δ~(18)O value). Using this approach, it can be found that ~(87)Sr-depleted brine from Ordovician carbonates have migrated up to and mixed with ~(87)Sr-enriched waters from Silurian and Carboniferous sandstones, and that Silurian brines have mixed with meteoric water. In the Kuche forland basin, brines from the Cambrian and Ordovician carbonates have higher ~(87)Sr/~(86)Sr ratios than those from the overlying sandstones, when combined with chemistry, δ~(15)N and ~3He/~4He ratios of the coexisting natural gases, suggesting that the brines were derived from the basement. There exists some debate on the effect of hydrocarbon emplacement on mineral diagenesis. Case-study from Silurian sandstones in the Central Tarim show that quartz has kept overgrowing secondarily when oil saturation was decreased by meteoric water flushing subsequently to hydrocarbon emplacement. Silicon precipitates on the water-wet quartz surface, leading to decreased Si concentration close to the surface. A Si grads can result in Si diffusion, which supplies Si for quartz overgrowth. Hydrocarbon oxidation-sulfate reduction is an important type of organic-inorganic interaction. Not only can it make secondary alteration of hydrocarbons, but generate H_2S and CO_2 gases which can improve reservoir property. Thermochemical sulfate reduction took place at the temperatures more than 125 ℃ to 140 ℃ in the Cambrian-Ordovician carbonates, the products - H_2S and CO_2 gases migrated up to the Silurian, and precipitated as pyrite and calcite, respectively. The pyrite has an average δ~(34)S value close to those of Ordovician seawater and anhydrite, and calcite has δ~(13)C value as low as -21.5‰. In the Hetianhe Gas Field, sulfate reduction bacteria carried by meteoric water flowing eastward may have preferentially depleted ~(12)C of light hydrocarbon gases, and results in heavier δ~(13)C values of the residual hydrocarbon gases and higher molar CO_2 in the natural gases in the west than in the east. Coexisting pyrite has δ~(34)S values as low as -24.9‰.

降雨触发滑坡的非线性模型与斜坡演化的混沌效应

This paper analyzes landsliding process by nonlinear theories, especially the influence mechanism of external factors (such as rainfall and groundwater) on slope evolution. The author investigates landslide as a consequence of the catastrophic slide of initially stationary or creeping slope triggered by a small perturbation. A fully catastrophe analysis is done for all possible scenarios when a continuous change is imposed to the control parameters. As the slip surface continues and erosion due to rainfall occurs, control parameters of the slip surface may evolve such that a previously stable slope may become unstable (e.g. catastrophe occurs), when a small perturbation is imposed. Thus the present analysis offers a plausible explanation to why slope failure occurs at a particular rainfall, which is not the largest in the history of the slope. It is found, by analysis on the nonlinear dynamical model of the evolution process of slope built, that the relationship between the action of external environment factors and the response of the slope system is complicatedly nonlinear. When the nonlinear action of slope itself is equivalent to the acting ability of external environment, the chaotic phenomenon appears in the evolution process of slope, and its route leading to chaos is realized with bifurcation of period-doublings. On the basis of displacement time series of the slope, a nonlinear dynamic model is set up by improved Backus generalized linear inversion theory in this paper. Due to the equivalence between autonomous gradient system and catastrophe model, a standard cusp catastrophe model can be obtained through variable substitution. The method is applied to displacement data of Huangci landslide and Wolongsi landslide, to show how slopes evolve before landsliding. There is convincing statistical evidence to believe that the nonlinear dynamic model can make satisfied prediction results. Most important of all, we find that there is a sudden fall of D, which indicates the occurrence of catastrophe (when D=0).

富碱侵入岩与金成矿关系:云南省姚安金矿床成矿流体形成演化的微量元素和同位素证据

以产在姚安富碱侵入岩体内外接触带上的姚安金矿床为对象,对成矿流体形成演化过程中的微量元素和S、C同位素地球化学进行了综合研究。研究结果表明,富碱侵入岩成岩过程中分异出的岩浆流体提供了姚安金矿床早期成矿作用所必需的成矿流体;从早期成矿阶段至晚期成矿阶段,成矿流体经历了从以岩浆流体为主的流体体系至以大气降水为主的流体体系的转变。因此,钙碱性侵入岩成岩过程中可分异出成矿流体的过程,也存在于富碱侵入岩的成岩过程中。