BaLiF_3∶Ce~(3+)纳米粒子的制备及其光谱特性

BaLiF3属立方钙钛矿型复合氟化物,作为高效闪烁晶体可用于热中子检测[1].由于其能带隙宽,易于实现各种不同价态稀土离子掺杂,可以获得许多可调谐性质,因此它也是比较理想的光学功能材料的基质[2].Ce3+激活的BaLiF3晶体作为紫外发射的短波固体激光材料和光放大材料的研究多有报道[3~5].Ce3+的发射特性强烈依赖于基质晶体结构[6,7].氟化物基质中氧杂质的含量是影响光谱性质的重要因素[8].为了寻找氧含量低、发射波长更短、可调谐范围更宽的激光材料,本工作制备了BaLiF3∶Ce3+纳米晶,获得了一些新的有意义的实验结果.如果将其引入合适的聚合物基体制备出纳米复合体系,有可能为新一代杂化激光材料提供更理想的光学活性组分[9].1实验部分1.1仪器用日本R igaκu D/maxⅡB型X射线衍射仪(XRD)测量样品的晶体结构,辐射源CuKα1(λ=0·154 1 nm);用日本H itachi S-570环境扫描电子显微镜(ESEM)观察样品的形貌和粒径大小;用日立F-4500荧光光谱仪测试样品的激发和发射光谱;用英国VG公司ESCALAB MKⅡX射线电子能谱仪(XPS)检测样品的含氧量.1.2实验过...

Determination of ultra-trace concentrations of elements in high purity tellurium by inductively coupled plasma mass spectrometry after Fe(OH)(3) coprecipitation

In this work, a method was established for the determination of impurities in high purity tellurium by inductively coupled plasma mass spectrometry (ICP-MS) after Fe(OH)(3) coprecipitation. After comparison of coprecipitation ability and separation efficiency between Fe(OH), and Al(OH)(3), Fe(OH)(3) was chosen as the precipitate. A separation factor of 160 for 200 mg tellurium was obtained under conditions of pH 9 and 2 mg of Fe3(+). The 13 elements, such as Bi, Sn, Pb, In, Tl, Cd, Cu, Co, Ni, Zn, Ti, Be and Zr, could be almost completely coprecipitated under these conditions. In addition, Te memory effect imposed on the ICP-MS instrument was assessed, as well as Te matrix effect that caused the low recovery of Ga, As, Sb and V in real sample was discussed. Finally, the method was evaluated through recovery test and was applied to practical sample analysis, with detection limits of most of the elements being below 0.15 mug g(-1) and R.S.D. below or at approximately 10%, which indicated that this method could fully satisfy the requirements for analysis of 99.999% similar to 99.9999% high purity Te.

H/D exchange reaction of cyclopropane derivatives in the ion system of CD3OD

The fragmentation properties of the product ions [M + 1](+), [M + 2](+) and [M + 3](+) formed by ion-molecule reaction of four cyclopropane derivatives with the ion system of CD3OD were investigated by using collision-induced dissocation technique. The experiment results indicated that the product ions were produced via the H/D exchange reaction between reactants and reactive reagent ions of CD3OD. There are two exchangable hydrogen atoms on the ring of compounds 1 and 2, and only one for compound 3 and 4.

环丙烷衍生物在CD_3OD离子体系中的H/D交换反应

研究了环丙烷衍生物在CD3 OD离子体系中的H/D交换反应产物离子 [M +1]+ 、[M +2 ]+ 和[M +3]+ 的碰撞诱导碎裂 (CID)反应特征。实验结果表明这些产物离子是由反应物与试剂离子之间发生H/D交换反应生成的。获得了环丙烷衍生物结构中活泼氢位置及其数量的信息

La_(1-x)Li_xMnO_3体系的输运特性及EPR研究

利用固相反应法合成了掺杂锂的La1-xLixMnO3(x=0,0.10,0.15,0.20,0.25,0.30)钙钛矿氧化物．XRD测试表明，所有样品均为菱方结构．除x=0,0.3外，其它样品均随温度的降低在液氮温区可观察到从绝缘态到金属态的转变，其中x=0.15样品的转变温度最高为167K．在H=1T的磁场下，出现了负磁阻现象．EPR谱上的ｇ＝2.00信号与Mn3+和Mn4+组成的复合团簇有关

SYNTHESIS AND CHARACTERIZATION OF TRISUBSTITUTED HETEROPOLYTUNGSTOGERMANATES CONTAINING GROUP 3A ELEMENTS

Six new compounds, alpha,beta-KaHb[GeW(9)M(3)(H2O)(3)O-37]. xH(2)O(M = Al, Ga, In; a + b = 7) and alpha-K9H5[Ge2W18Ga6(H2O)(3)O-74]. 20H(2)O, were synthesized from the lacunary precursors a and beta-GeW9O3410- and characterized by elemental analysis, spectroscopy and electrochemistry. Tungsten-183 NMR spectra of the title complexes consist of two lines with intensity ratio 2:1 as expected for trisubstituted heteropoly anions. The intensity ratio of alpha-Ga compound is 1:2, which is different from others(a:1). With the help of FAB mass spectrum, we concluded that it is a dimer with D-3h structure in aqueous, and the others exist by monomers with C-3v structures.

A DYNAMIC LASER LIGHT-SCATTERING STUDY OF CHITOSAN IN AQUEOUS-SOLUTION

The solution behavior of four chitosans (91% deacetylated chitin) with different molecular weights in 0.2M CH3COOH/0.1M CH3COONa aqueous solution was investigated at 25 degrees C by dynamic laser light scattering (LLS). The Laplace inversion of the precisely measured intensity-intensity time correlation function leads us to an estimate of the line-width distribution G(Gamma), which could be further reduced to a translational diffusion coefficient distribution G(D). By using a combination of static and dynamic LLS results, i.e. Mw and G(D), we were able to establish a calibration of D = k(D)M(-alpha D) with k(D) = (3.14 +/- 0.20) X 10(-4) and alpha(D) = 0.655 +/- 0.015. By using this calibration, we successfully converted G(D) into a molecular weight distribution f(w)(M). The larger alpha(D) value confirms that the chitosan chain is slightly extended in aqueous solution even in the presence of salts. This is mainly due to its backbone and polyelectrolytes nature. As a very sensitive technique, our dynamic LLS results also revealed that even in dilute solution chitosan still forms a small amount of larger sized aggregates that have ben overlooked in previous studies. The calibration obtained in this study will provide another way to characterize the molecular weight distribution of chitosan in aqueous solution at room temperature. (C) 1995 John Wiley & Sons, Inc.

HOST-GUEST INTERACTIONS OF THIAMINE WITH ANIONS - CRYSTAL-STRUCTURE OF THIAMINE IODIDE SESQUIHYDRATE

The crystal structure of thiamine iodide sesquihydrate has been determined by X-ray diffraction methods as a host-guest model for coenzyme-substrate interactions. The asymmetric unit contains two chemical units. Both the thiamine molecules A and B, which are crystallographically independent, assume the usual F conformation and have a disordered hydroxyethyl side chain. An iodide anion (or a water molecule) bridges the pyrimidine and thiazolium rings of molecule A (or B) by forming a hydrogen bond with the amino group and an electrostatic contact with the thiazolium ring to stabilize the molecular conformation. In the crystal the thiamine molecules self-associate to form a pipe-like polymeric structure, in which four thiamine hosts surround an iodide guest and hold it through C(2)-H...I hydrogen bonds and thiazolium...I electrostatic interactions. Crystal data: C12H17N4OS+.I- . 1.5 H2O, monoclinic, P2(1)/c, a = 12.585(2), b = 25.303(5), c = 12.030(2) angstrom, beta = 115.15(1)degrees, V = 3468(1) angtrom3, Z = 8, D(c) = 1.606 g cm-3, R = 0.045 for 3328 observed reflections.

THE YELLOW-TO-BLUE INTENSITY RATION (Y/B) OF DY-3+ EMISSION

Various borates, vanadates, niobates, antimonates, titanates, zirconates and CaS doped with Dy3+ were prepared. Factors which have an effect on the yellow-to-blue intensity ratio (Y/B) of Dy3+ emission are reported. Y/B increases with decreasing Z/r or electronegativity of the next-neighbour element M in the complex oxides Dy-O-M. The greater the degree of covalency between Dy3+ and O2-, the greater Y/B is. When Dy3+ is located at a site with an inverse centre and high symmetry, Dy3+ displays no luminescence. It seems that Y/B of Dy3+ located at a site deviated from an inverse centre is greater than that of Dy3+ located at a site without an inverse centre. Y/B does not vary much with the variation in concentration of Dy3+ when Dy3+ is substituted for an element with the same valency, but it does depend on the concentration of Dy3+ when Dy3+ is substituted for an element with a different valency in the matrix, because defects are formed in this case.

YP_xV_(1-x)O_4(0≤x≤1):Dy~(3+)的合成及其光谱性质的研究

本文报道了不同组成的YP_xV_(1-x)O_4(0≤x≤1):Dy~(3+)的合成和结构。YP_xV_(1-x)O_4(0≤x≤1)为四方晶系,晶胞参数随x的增大呈线性减小。基质的Stokes位移随x的增大逐渐变大,而激发光谱峰值则向短波方向移动。在YP_xV_(1-x)O_4:0.006Dy~(3+)体系中,x>0.4时出现的基质发射是由P0_4~(3-)引起的。基质及Dy~(3+)的发光效率和Dy~(3+)的发光强度的黄蓝比均与x有关。同时探讨了Bi~(3+)和温度对Dy~(3+)的发光强度的影响。

Er_(3x)~(3+):Y_(3-3x)Al_5O_(12)和Er_x~(3+)Yb_(1-x)P_5O_(14)晶体的光谱强度参数

本文报道了用J-O理论计算的Er_(3x)~(3+):Y_(3-3x)A_5O_(12)和Er_x~(3+)Yb_(1-x)P_5O_(14)两种晶体中Er~(3+)五种浓度的振子强度、Ω_λ参数、辐射跃迁几率与荧光分支比。并观察了这些参数的变化规律。

He, Ne and Ar isotopic composition of Fe-Mn crusts from the western and central Pacific Ocean and implications for their genesis

The noble gas nuclide abundances and isotopic ratios of the upmost layer of Fe-Mn crusts from the western and central Pacific Ocean have been determined. The results indicate that the He and Ar nuclide abundances and isotopic ratios can be classified into two types: low He-3/He-4 type and high He-3/He-4 type. The low He-3/He-4 type is characterized by high He-4 abundances of 191x10(-9) cm(3.)STP(.)g(-1) on average, with variable He-4, Ne-20 and Ar-40 abundances in the range (42.8-421)x10(-9) cm(3.)STP(.)g(-1), (5.40-141)x10(-9)cm(3.)STP(.)g(-1), and (773-10976)x10(-9) cm(3.)STP(.)g(-1), respectively. The high He-3/He-4 samples are characterized by low He-4 abundances of 11.7x10(-9) cm(3.)STP(.)g(-1) on average, with He-4, Ne-20 and Ar-40 abundances in the range of (7.57-17.4)x10(-9) cm(3.)STP(.)g(-1), (110.4-25.5)x10(-9) cm(3.)STP(.)g(-1) and (5354-9050)x10(-9) cm(3.)STP(.)g(-1), respectively. The low He-3/He-4 samples have He-3/He-4 ratios (with RIRA ratios of 2.04-2.92) which are lower than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (447-543) which are higher than those of air (295.5). The high He-3/He-4 samples have He-3/He-4 ratios (with R/R-A ratios of 10.4-12.0) slightly higher than those of MORB (R/R-A=8 +/- 1) and Ar-40/Ar-36 ratios (293-299) very similar to those of air (295.5). The Ne isotopic ratios (Ne-20/Ne-22 and Ne-21/Ne-22 ratios of 10.3-10.9 and 0.02774-0.03039, respectively) and the Ar-38/Ar-36 ratios (0.1886-0.1963) have narrow ranges which are very similar to those of air (the Ne-20/Ne-22, Ne-21/Ne-22, Ar-38/Ar-36 ratios of 9.80, 0.029 and 0.187, respectively), and cannot be differentiated into different groups. The noble gas nuclide abundances and isotopic ratios, together with their regional variability, suggest that the noble gases in the Fe-Mn crusts originate primarily from the lower mantle. The low He-3/He-4 type and high He-3/He-4 type samples have noble gas characteristics similar to those of HIMU (High U/Pb Mantle)- and EM (Enriched Mantle)-type mantle material, respectively. The low He-3/He-4 type samples with HIMU-type noble gas isotopic ratios occur in the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain and the Mid-Pacific Seamounts whereas the high He-3/He-4 type samples with EM-type noble gas isotopic ratios occur in the Line Island Chain. This difference in noble gas characteristics of these crust types implies that the Magellan Seamounts, Marcus-Wake Seamounts, Marshall Island Chain, and the Mid-Pacific Seamounts originated from HIMU-type lower mantle material whereas the Line Island Chain originated from EM-type lower mantle material. This finding is consistent with variations in the Pb-isotope and trace element signatures in the seamount lavas. Differences in the mantle surce may therefore be responsible for variations in the noble gas abundances and isotopic ratios in the Fe-Mn crusts. Mantle degassing appears to be the principal factor controlling noble gas isotopic abundances in Fe-Mn crusts. Decay of radioactive isotopes has a negligible influence on the nuclide abundances and isotopic ratios of noble gases in these crusts on the timescale of their formation.

中国海异毛虫科和海稚虫科分类学和地理分布研究

异毛虫科（Paraonidae）和海稚虫科（Spionidae）是环节动物门（Annelida），多毛纲（Polychaeta）中两个常见的科，其成体在海洋生态系统尤其是海洋底栖动物群落中占有重要地位。中国近海异毛虫科和海稚虫科种类极为常见，在潮间带和潮下带均有分布。但由于此两科种类个体小，采集和鉴定困难，在中国一直没有系统的分类学研究。 本论文选择异毛虫科和海稚虫科为研究对象，以中国科学院海洋研究所海洋生物标本馆馆藏的3000余号成体标本为主要研究材料，结合攻读博士学位期间对全国各海域的补充采集标本和从其它单位借用的标本，在认真阅读相关文献和比对某些种类模式标本的基础上，首次对此两科的中国种类进行了全面系统的分类学和地理分布研究。结果如下： 1. 本文记述了中国海域异毛虫科4属18种，其中包括3新纪录种；海稚虫科16属39种，包括7新种，10新纪录种。各鉴定种类均进行了详细的分类学特征描述，并附有形态学结构图。对罕见种类的标本和保存状况较差、光学显微镜无法获得可靠分类学信息的标本进行了扫描电镜观察，并拍摄有电镜照片。 2. 对中国海域有关异毛虫科和海稚虫科种类记录进行了系统的分类学修订，澄清了部分种类特别是一些常见种类分类学研究中存在的错误和混淆。（1）通过大量阅读文献和反复比较检查标本，认为以前我国文献记录的海稚虫科奇异稚齿虫属的奇异稚齿虫Paraprionospio pinnata (Ehlers, 1901)实际包括3种，即扭鳃奇异稚齿虫Paraprionospio inaequibranchia (Caullery, 1914)、枫香树奇异稚齿虫Paraprionospio coora Wilson, 1990和冠奇异稚齿虫Paraprionospio cristata sp. nov.，其中扭鳃奇异稚齿虫和枫香树奇异稚齿虫在中国海属首次记录，冠奇异稚齿虫为一新种。枫香树奇异稚齿虫主要分布于黄海，其分布南界为121°30′ E, 34°30′ N, 扭鳃奇异稚齿虫分布于南海，其分布北界为114°00′ E, 21°45′ N，冠奇异稚齿虫分布区域较广，从长江口到南海的沿岸水域均有分布。奇异稚齿虫是分布在智利、南加利福尼亚、西墨西哥（可能还有安哥拉）的种，在我国海域未见分布。（2）将在我国北方沿海非常常见但长期被记录为鳞腹钩虫Scolelepis (Scolelepis) squamata (Müller, 1806)(海稚虫科)的标本重新鉴定为一个新种，即红纹腹钩虫Scolelepis (Scolelepis) daphoinos sp. nov.；鳞腹钩虫分布于北大西洋和地中海沿岸水域，在我国海域未见分布。（3）明确了中国海Prionospio steenstrupi复合体种类。此复合体所包含的种类在形态上十分相似，分类学研究时极易混淆。在已有的文献记录中，该复合体中国种类包括两种，玛氏稚齿虫Prionospio (Prionospio) malmgreni Claparède, 1870和西沙稚齿虫Prionospio (Prionospio) sishaensis Wu & Chen, 1964。本文将该复合体中国种类修正为5种，分别是包氏稚齿虫Prionospio (Prionospio) bocki Söderström, 1920、开普敦稚齿虫Prionospio (Prionospio) dubia Maciolek, 1985、太平洋稚齿虫Prionospio (Prionospio) pacifica sp. nov.、欢乐稚齿虫Prionospio (Prionospio) paradisea Imajima, 1990和西沙稚齿虫Prionospio (Prionospio) sishaensis Wu & Chen, 1964。现在大多数分类学者认为玛氏稚齿虫是一个不可鉴定种，该种的原始描述可能包括数种，且模式标本已丢失。（4）将中国海记录的矮小离稚齿虫Apoprionospio pygmaea (Hartman, 1961)更正为卡米拉离稚齿虫Apoprionospio kirrae Wilson, 1990；将中国海记录的科氏光稚虫Spiophane kroyeri Grube, 1860更正为深蓝光稚虫Spiophanes fuscatus sp. nov.。 3. 比较研究了中国海域异毛虫科和海稚虫科的区系特点，详细分析了两科中国海种类的组成。认为中国种类在区系组成上属于印度-马来区系，异毛虫科中国海特有种较少，仅2种，占该科中国种数的11%；而海稚虫科中国海特有种较多，共9种，占该科中国种数的23%。中国海异毛虫科种类组成和日本、俄罗斯附近水域的组成较为相似，中国海海稚虫科种类组成和日本、澳大利亚附近水域的组成较为相似。

刺参Apostichopus japonicus生态免疫与夏眠的基础研究

针对目前刺参养殖过程中亟需解决的种质、环境和产品品质之间日益突出的矛盾，本论文从刺参的自身防御和内分泌机制入手，比较系统地研究了环境胁迫与细胞免疫和应激激素之间的作用机理；并从生理和分子的角度对刺参的夏眠机理进行了初步研究，主要研究成果如下： 1. 查阅国内外大量文献资料，较为系统地综述了海参的免疫体系、生态免疫学研究进展、当前夏眠机理的研究状况和刺参夏眠的基础研究。对刺参生态免疫及其夏眠机理研究提出了新的见解和思路。 2. 研究了温度(0、8、16、24、32℃)和盐度(20、25、35)的急性胁迫(72h)作用对刺参免疫指标的影响。刺参体腔液内几种免疫酶类活性受升温胁迫影响显著；而降温胁迫的影响并不显著。高盐胁迫可使刺参体腔液细胞吞噬活性、超氧化物歧化酶和过氧化氢酶活性显著变化，而对髓过氧化物酶和溶菌酶活性都没有显著影响。从这几种免疫指标变化情况来看，温度胁迫对刺参的影响要强于盐度胁迫，且高温胁迫的影响要强于低温胁迫。 3. 研究了温度(8、16、24℃)、盐度(20、25、35)和露空等急性胁迫(24h)作用对刺参体腔液儿茶酚胺类激素含量的影响。急性温度胁迫能够显著影响刺参体腔液内肾上腺素、去甲肾上腺素和多巴胺的含量；而盐度和露空胁迫对刺参体腔液肾上腺素含量、去甲肾上腺素含量以及多巴胺含量都没有产生显著影响。 4. 完成了刺参体腔液几种酶类变化的周年测定(2006年7月到2007年6月)。一年内刺参体腔液内几种酶类变化的转折点为9月份，10月份，1月份，2月份，4月份和5月份。刺参体腔液内几种酶类活性变化与温度和盐度等环境因素并不存在简单的相关关系，因此推测这些显著变化并不是单一温度、盐度等因素作用的结果，还可能与刺参生长、繁殖及其它环境因素的作用有关。 5. 开展了夏眠期间刺参免疫指标的现场研究(2006年7月到11月)。在此期间刺参体腔液细胞总数显著下降；刺参体腔液内免疫相关酶类均在8月份、9月份达到最高值；肾上腺素和去甲肾上腺素的含量均在8月下旬和11月下旬显著升高，而多巴胺含量则没有显著变化。刺参完全进入夏眠的8、9月份，体腔液内各项免疫指标也都具有显著变化，说明夏眠对刺参机体的免疫状态产生影响。 6. 探讨了刺参夏眠前后肠道基因表达的差异(2007年7月至12月)。抑制消减杂交实验结果表明接头连接效率大于50%，说明连接效率较高。消减效率分析结果表明，消减后进行cDNA保守序列扩增比未消减落后约10个循环才能明显看到扩增产物，说明对共同序列的消减效率比较高。利用抑制消减杂交技术成功构建了符合技术要求的夏眠刺参与未夏眠刺参肠道抑制消减杂交基因文库。

大型藻类在工程治理海水富营养化和抑制病原微生物中的作用

沿海工农业生产的快速发展和人类活动对近海生态系统产生了很大影响，大量化肥的使用和工业污水、生活污水的排放导致近海环境污染，海水富营养化，赤潮频发。另外，由于近海养殖活动的迅猛发展以及养殖的不规范和不科学性导致近海生态系统结构和功能改变，一方面加重了海水富营养化，另一方面养殖动植物病害经常发生，严重影响了海产品的质量和效益。 大型海藻是海区重要的初级生产者，生命周期长、生长快，能通过光合作用吸收固定水体的C、N、P等营养物质来合成自身，同时增加水体溶解氧。因此，大型海藻被称为海洋环境中的生物过滤器。另外，由于大型藻类自身营养成分的复杂性和与藻共生的微生物多样性，大型海藻还可对生态系统中的浮游生物和微生物产生直接和间接影响。 在海洋环境，尤其是海水养殖水体环境存在着两个主要问题：海水富营养化和病源微生物控制，本文针对海洋环境中存在的这两个问题进行了探索研究。 以大型经济藻种长心卡帕藻（Kappaphycus alvarezzi）作为实验材料，分别在实验室内、室外藻类处理系统和海湾养殖现场三种条件下，进行藻类去除海水氮磷的一次性实验、半连续实验和连续实验，研究了其对海水中无机氮、无机磷的吸收速率和去除能力，初步评估了其生态价值。 构建了一种半封闭海域富营养化治理模式，以长心卡帕藻为实验材料，研究了其去除海水富营养化的能力，主要结果如下： （1）室内实验研究发现，长心卡帕藻对氮、磷的吸收速率随底物浓度升高而升高。在氮磷比为10:1，温度28℃条件下，氮浓度为50μmol • L-1时，藻对氮、磷的吸收速率达到最大，分别为0.93µmol • g-1（FW）• h-1和0.072µmol • g-1（FW）• h-1。 （2）人工修建的藻类养殖系统中进行的长心卡帕藻去除氮、磷的半连续实验，结果表明该藻具有连续去除海水DIN、DIP的能力。只要保持足够的底物浓度，长心卡帕藻对无机氮、无机磷的吸收速率达到最大，分别为0.3µmol • g-1（FW） • h-1和0.03µmol • g-1（FW）• h-1。但是对氮磷的吸收速率较室内实验有所降低。 （3）自然条件下，通过调查黎安海湾水质情况发现，长心卡帕藻具有较大的生态效益。在整个海湾大面积养殖卡帕藻，通过收获藻体，每年大约可以从海水中带走33吨氮素，7.5吨磷素。由于在海湾长心卡帕藻的作用，全年海湾水质保持在1-2级国家海水质量标准，产生了明显的生态效益。 另外，我们对大型藻类浒苔（Ulva clathrata）吸收氮磷和抑制鳗弧菌（Vibrio anguillarum）的效果进行了初步探索，结果表明：浒苔不仅对培养系统内无机氮和磷具有明显的去除作用，而且在异养细菌总量没有降低的情况下，对鳗弧菌有显著抑制作用，该抑制作用还受到水体中氮磷营养盐浓度的影响。在10g • L-1海藻的条件下，鳗弧菌以105－107 cfu • mL-1接入2天后，无论是否添加外源氮磷，鳗弧菌密度降到10 cfu • mL-1以下，鳗弧菌去除率几乎达到100%。实验数据还显示，添加氮磷营养盐可以增强浒苔对鳗弧菌的抑制作用，但没有降低其中的异养菌群数量，系统内异养细菌总量均维持在较高水平。进一步研究表明，培养浒苔24h后的海水，也对鳗弧菌65#产生抑制作用，这说明浒苔代谢释放到水体中某种化学成分或与藻共栖的微生物对鳗弧菌生长产生了抑制。