抗 LDH－C4 IgA 和IgG 抗体在粘膜免疫系统的分布及其抗生育作用的研究

已有的研究表明，小鼠背部携带能分泌抗原特异的IgA 单克隆抗体的杂交细 胞瘤，可以保护小鼠抵抗微生物和病毒等多种病原体经粘膜途径感染机体。我们 利用背部携带能分泌抗精子特异抗原（LDH-C4）的IgA 和IgG 杂交细胞瘤、以 及抗DNP 的IgA 骨髓细胞瘤的小鼠为动物模型，采用定量ELISA 法研究了抗 LDH－C4 IgA 与抗DNP IgA 单克隆抗体在呼吸道、肠道及生殖道内转运和分布， 抗LDH-C4 IgG2b 在肠道内转运与分布，以及抗LDH-C4 IgA 和IgG 单克隆抗体 在体内抗生育作用。 研究结果表明，带瘤小鼠血液中含有较高水平抗原特异的 IgA 和IgG 单克 隆抗体。PA4 和MOPC IgA 单克隆抗体在呼吸道、肠道以及雌性生殖道分泌物 内有较高的分布水平。在肠道，PA4 和MOPC IgA 单克隆抗体的分布水平显著 高于IgG（p<0.01 和p<0.05）。在肠道和生殖道的不同部位，IgA 抗体的分布水 平不同。在肠道，结肠分泌物中的IgA 单克隆抗体显著高于其它肠道部位 （p<0.01）。在生殖道，IgA 单克隆抗体分布水平以子宫角分泌物中最高。雄性 的前列腺也有较高的IgA 抗体水平。在呼吸道、肠道以及雌性生殖道相应部位的 分泌物内，PA4 IgA 单克隆抗体的水平显著高于MOPC IgA 单克隆抗体的分布水 平（p<0.05）。PA4 和MOPC IgA 单克隆抗体在粘膜分泌物内的分布水平差异可 能与其IgA 聚合形式的不同有关。另外，除气管外，在两时间点间分泌物中的 IgA 抗体水平没有显著差异。 检测背部带瘤小鼠交配后的两细胞胚胎期，发现携带PA4 和G2b 杂交细瘤 的雌性小鼠的受精率与对照组并没有显著的差异，这表明抗LDH-C4 IgA 和IgG 单克隆抗体在体内不能明显抑制小鼠的精子和卵子的结合或受精过程。注射细 胞后的27 天，检测鼠着床胚胎时，发现带瘤两性小鼠均携带PA4 时或者只有 雌性携带PA4 杂交瘤时，以及雌雄两性小鼠均携带G2b 杂交瘤细胞时，交配后的怀孕率与能分泌抗DNP 抗体的MOPC 的骨髓瘤细胞瘤的相应组别相比，显 著降低（p<0.01）。但PA4 各组与G2b 各组之间无显著差异(p>0.05）。然而，雌 雄的小鼠均带瘤时，最高怀孕减少率未能达100%。这些结果提示，抗LDHC4 IgA 和IgG 单克隆抗体在小鼠体内不能有效地抑制小鼠的精子与卵子的结 合，但能显著地抑制小鼠受精后胚胎的发育。抗LDH-C4 的IgA 和IgG 单克隆 抗体单独存在时，在体内均具有抗生育作用，但不能完全抑制生育。

抗LDH-C4 IgA和IgG抗体在带瘤小鼠生殖道和其它粘膜分泌物内分布特性的研究

中文摘要 　 已有的研究表明，小鼠背部携带能分泌抗原特异的IgA单克隆抗体的杂交细胞瘤，可以保护小鼠抵抗微生物和病毒等多种病原体经粘膜途径感染机体。我们利用背部携带能分泌抗精子特异抗原（LDH-C4）的IgA和IgG杂交细胞瘤、以及抗DNP的IgA骨髓细胞瘤的小鼠为动物模型，采用定量ELISA法研究了抗LDH-C4 IgA与抗DNP IgA单克隆抗体在呼吸道、肠道及生殖道内转运和分布，抗LDH-C4 IgG2b在肠道内转运和分布，以及抗LDH-C4 IgA和IgG单克隆抗体与体内抗生育作用的关系。研究结果表明，带瘤小鼠血液中含有较高水平抗原特异的IgA和IgG单克隆抗体。PA4和MOPC IgA单克隆抗体在呼吸道、肠道以及雌性生殖道分泌物内有较高的分布水平。在肠道，PA4和MOPC IgA 单克隆抗体的分布水平显著高于IgG（p < 0.01和p < 0.05）。在肠道和生殖道的不同部位，IgA抗体的分布水平不同。在肠道，结肠分泌物中的IgA单克隆抗体显著高于其它肠道部位（p < 0.01）。在生殖道，IgA单克隆抗体分布水平以子宫角分泌物中最高。雄性的前列腺也有较高的IgA抗体水平。在呼吸道、肠道以及雌性生殖道相应部位的分泌物内，PA4 IgA单克隆抗体的水平显著高于MOPC IgA单克隆抗体的分布水平（<0.05）。PA4和MOPC IgA单克隆抗体在粘膜分泌物内的分布水平差异可能与其IgA聚合形式的不同有关。另外，除气管外，在两时间点间分泌物中的IgA抗体水平没有显著差异。检测背部带瘤小鼠交配后的两细胞胚胎期，发现携带PA4或G2b杂交细胞瘤的雌雄小鼠的受精率与对照组并没有显著性差异，这表明抗LDH-C4 IgA和IgG单克隆抗体在体内不能显著抑制小鼠的精子和卵子的结合或受精过程。注射细胞后的27天，检测着床胚胎时，发现带瘤两性小鼠均携带PA4时或者只有雌性携带PA4杂交瘤时，以及雌雄性小鼠均携带G2b杂交瘤时，交配后的怀孕率与带能分泌抗DNP抗体的MOPC骨髓瘤细胞瘤的相应组别相比，显著降低（p < 0.01）。但PA4各组与G2b各组之间无显著差异（p < 0.05）。然而，雌雄小鼠均带瘤时，最高怀孕减少率也未达到100%。这些结果提示，抗LDH-C4 IgA和IgG单克隆抗体在小鼠体内不能有效地抑制小鼠的精子和卵子的结合，但能显著地抑制小鼠受精后胚胎的发育。抗LDH-C4 的IgA或者IgG单克隆抗体单独存在时，在小鼠体内均具有抗生育作用，但不能完全抑制生育。

抗LDH-C4的IgA单克隆抗体在生殖道局部的分布

为了弄清生殖道内抗体，特别是IgA抗体的准确来源和它的调控因子，同时也为了弄清生殖的局部免疫与典型的粘腊免疫之间的关系，以同位素标记的针对精子特有抗原乳酸脱氢酶C4(LDH-C4)的多聚IgA单抗及其单体，与小鼠精子发生反应的IgA单抗，以及LDH-C4特异的IgG抗体，尾静脉注射给雌雄Balb/c小鼠，4小时后测定小鼠的生殖道及其分汾物，肠道、呼吸道及其分泌物，各相关淋巴组织以及其它器官内这些抗体的分布。还研究了特异抗原刺激、性激素等对这些抗体分布状况的影响。

抗小鼠乳酸脱氢酶C4（LDH-C4）IgA单克隆抗体的制备及其对精子功能的影响

乳酸脱氢酶C4 （LDH-C4）是一种人和哺乳动物精子特有的乳酸脱氢酶同功酶。用纯化的小鼠LDH-C4 免疫动物，有一定的避孕效果。这种避孕效果与血清特异性抗体水平并不完全一致。这可能是由于受精过程是在生殖道内进行的，而生殖道内又有粘膜免疫因素存在。IgA抗体是生殖道内的主要抗体成分，研究抗LDH-C4 IgA抗体的抗精子作用有助于了解局部分泌性免疫系统在抗精子免疫避孕中的作用。由于足够量的特异性IgA抗体难于从动物或人粘膜分泌液中分离到，为了获得供体内外试验用的该种抗体，直接证明它在抗生育方面的作用，我们采用一种特殊的免疫方法制备了一系列的抗LDH-C4的单克隆抗体，包括6株IgA和9株IgM。这种免疫方法的主要特点是将抗原直接注射到派伊尔氏淋巴小结（PP）或小肠腔内。ELISA检测表明，按这种方法免疫后，分泌IgA的克隆出现的比例明显高于常规免疫的结果。这是因为PP是粘膜免疫的中枢，其中含有大量的IgA前体细胞，直接将抗原注射到PP内有助于刺激IgA前体细胞的分化和增殖，诱导局部分泌性免疫反应。我们用所得到的单克隆抗体研究了LDH-C4在人，小鼠和树鼩精子表面的定位。结果表明，大多数单克隆抗体可以结合到这些精子的表面；不同的单抗在同一物种的精子表面呈现不同的结合区域。这一方面说明来源于人，小鼠和树鼩的LDH-C4的抗原决定簇有很高的同源性；另一方面提示LDH-C4在精子表面不同的区域所暴露的抗原决定簇不同。初步的功能试验表明，某些抗LDH-C4的IgA单克隆抗体可以凝集或制动精子，说明生殖道内的IgA抗体可以通过凝集和制动作用来影响精子的功能，从而影响精子的受精力。

定量ELISA检测小鼠血清中抗LDH-C4IgG2b抗体的水平

用定量EL ISA 的方法检测背部携带分泌抗LDH - C4 IgG2b 抗体杂交瘤小鼠的血清中IgG2b 抗体浓 度, 结果表明: 本法稳定, 批间变异系数为7104 %～13130 % , 批内变异系数为3161 %～10120 %; 标准曲线 相关性良好, 相关系数从01962 884～01996 795 ; 灵敏度较高, 最低检出浓度为0101 mg/ L ; 特异性亦较好.

乳酸脱氢酶C_(4)的精子免疫荧光定位特性

研究表明精子表面的乳酸脱氢酶C_(4)(LDH-C_(4))呈现多位点分区分布, 精子的 不同部位暴露的LDH-C_(4)的抗原决定簇不同。在被检动物中, LDH-C_(4)显示明显的同源性。图版1表4参12

Mechanism of interaction of hydrocalumites (Ca/Al-LDH) with methyl orange and acidic scarlet GR

The development of new materials for water purification is of universal importance. Among these types of materials are layered double hydroxides (LDHs). Non-ionic materials pose a significant problem as pollutants. The interaction of methyl orange (MO) and acidic scarlet GR (GR) adsorption on hydrocalumite (Ca/Al-LDH-Cl) were studied by X-ray diffraction (XRD), infrared spectroscopy (MIR), scanning electron microscope (SEM) and near-infrared spectroscopy (NIR). The XRD results revealed that the basal spacing of Ca/Al-LDH-MO was expanded to 2.45 nm, and the MO molecules were intercalated with a inter-penetrating bilayer model in the gallery of LDH, with 49o tilting angle. Yet Ca/Al-LDH-GR was kept the same d-value as Ca/Al-LDH-Cl. The NIR spectrum for Ca/Al-LDH-MO showed a prominent band around 5994 cm-1, assigned to the combination result of the N-H stretching vibrations, which was considered as a mark to assess MO- ion intercalation into Ca/Al-LDH-Cl interlayers. From SEM images, the particle morphology of Ca/Al-LDH-MO mainly changed to irregular platelets, with a “honey-comb” like structure. Yet the Ca/Al-LDH-GR maintained regular hexagons platelets, which was similar to that of Ca/Al-LDH-Cl. All results indicated that MO- ion was intercalated into Ca/Al-LDH-Cl interlayers, and acidic scarlet GR was only adsorped upon Ca/Al-LDH-Cl surfaces.

Effective adsorption of sodium dodecylsulfate (SDS) by hydrocalumite (CaAl-LDH-Cl) induced by self-dissolution and re-precipitation mechanism

Hydrocalumite (CaAl-LDH-Cl) were synthesized through a rehydration method involving a freshly prepared tricalcium aluminate (C3A) with CaCl2 solution. To understand the intercalation behaviour of sodium dodecylsulfate (SDS) with CaAl-LDH-Cl, X-ray diffraction (XRD), Fourier transform infrared (FTIR), scanning electron microscopy (SEM), transmission electron microscope (TEM), X-ray photoelectron spectroscopy (XPS), inductively coupled plasma-atomic emission spectrometer (ICP) and elemental analysis have been undertaken. The sorption isotherms with SDS reveal that the maximum sorption amount of SDS by CaAl-LDH-Cl could reach 3.67 mmol•g-1. The results revealed that CaAl-LDH-Cl holds a self-dissolution property, about 20-30% of which is dissolved. And the dissolved Ca2+, Al3+ ions are combined with SDS to form CaAl-SDS or Ca-SDS precipitation. It has been highlighted that the composition of resulting products is strongly dependent upon the SDS concentration. With increasing SDS concentrations, the main resulting product changes from CaAl-SDS to Ca-SDS, and the value of interlayer spacing increased to 3.27 nm.

Electron petrography of fine-grained matrix in the Karoonda C4 carbonaceous chondrite

The study of matrices of rare Type 4 carbonaceous chondrites can reveal important information on parent body rnetamorp~ic processes and provide a comparison with processes on parent bodies of ordinary chc-idrites. Reflectance spectra (Tholen, 1984) from the two largest asteroids in the asteroid belt, Ceres and Pallas, suggest that they may be metamorphosed carbonaceous chondrites. These two asteroids constitute - onethird of the mass in the asteroid belt implying that type 4-6 carbonaceous chondrites are poorly represented in the meteorite collection and may be of considerable importance. The matrix of the C4 chondrite Karoonda has been investigated using a JEOL 2000FX analytical electron microscope (AEM) with an attached Tracor-Northem TN5500 energy dispersive spectrometer (EDS). In previous studies (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969), the petrography of the Karoonda matrix has been described as consisting largely of coarse-grained (50-200 urn in size) olivine and plagioclase (20-100 um in size), associated with micrometer sized magnetite and rare sulphides. AEM observations on matrix show that in addition to these large grains, there is a significant fraction (10 vol%) of interstitial fine grained phases « 5 urn). The mineralogy of these fine-grained phases differs in some respects from that of the coarser-grained matrix identified by optical and SEM techniques (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969). I~ particular crystals of two compositionally distinct pyroxenes « 2 urn in size) have been identified which have not been previously observed in Karoonda by other analytical techniques. Thin film microanalyses (Mackinnon et al., 1986) of these two pyroxenes indicate compositions consistent with augite and low-Ca pyroxene (- Fs27). Fine-grained anhedral olivine « 2 urn size) is the most abundant phase with composition -Fa29' This composition is essentially indistinguishable from that determined for coarser-grained matrix olivines using an electron microprobe (Scott and Taylor, 1985; Fitzgerald, 1979; Van Schmus, 1969). All olivines are associated with subhedral magnetites « 1 urn size) which contain significant Cr (- 2%) and Al (- 1%) as was also noted for larger sized Karoonda magnetites by Delaney et al. (1985). It has recently been suggested (Burgess et al., 1987) on the basis of sulphur release profiles for S-isotope analyses of Karoonda that CaS04 (anhydrite) may be present. However, no sulphate phase has, as yet, been identified in the matrix of Karoonda. Low magnification contrast images suggest that Karoonda may have a significant porosity within the fine-grained matrix fraction. Most crystals are anhedral and do not show evidence for significant compaction. Individual grains often show single point contact with other grains which result in abundant intergranular voids. These voids frequently contain epoxy which was used as part of the specimen preparation procedure due to the friable nature of the bulk sample.

Mid- and near-infrared spectroscopic investigation of homogeneous cation distribution in MgxZnyAl(x+y)/2-layered double hydroxide (LDH)

In this report, a detailed FTIR fitting analysis was used to recognize Mg, Zn and Al homogeneous distribution in MgxZnyAl(x+y)/2-Layered double hydroxide (LDH) hydroxyl layer. In detail, OH-Mg2Al:OH-Mg3 ratios decreased from 95.2:4.8 (MIR) and 94.2:5.8 (NIR) to 58.9:41.1 (MIR) and 61.8:38.2 (NIR), when Mg:Al increased from 2.2:1.0 to 4.1:1.0 in MgAl-LDHs. These fitting results were similar with theoretical calculations of 94.3:5.7 and 59.0:41.0. In a further analysis of MgxZnyAl(x+y)/2-LDHs, OH bonded Zn2Mg, Zn2Al, MgZnAl, Mg2Al and Mg2Zn peaks were identified at 3420, 3430, 3445–3450, 3454 and 3545 cm-1, respectively. With the decrease of Mg:Zn from 3:1 to 1:3, metal-hydroxyl bands changed from OH-Mg2Al and MgZnAl (with a ratio of 49.4:50.6) to OH-MgZnAl and Zn2Al (with a ratio of 55.0:45.0). They were also similar with theoretical calculations of 47.6:52.4 and 54.6:45.4. As a result, these results show that there is an ordered cation distribution in MgxZnyAl(x+y)/2-LDH, and FTIR is feasible in recognizing this structure.

Organo-LDH synthesized via tricalcium aluminate hydration in the present of Na-dodecylbenzenesulfate aqueous solution and subsequent investigated by near-infrared and mid-infrared

Na-dodecylbenzenesulfate (SDBS), a natural anionic surfactant, has been successfully intercalated into a Ca based LDH host structure during tricalcium aluminate hydration in the presence of SDBS aqueous solution (CaAl-SDBS-LDH). The resulting product was characterized by powder X-ray diffraction (XRD), mid-infrared (MIR) spectroscopy combined with near-infrared (NIR) spectroscopy technique, thermal analysis (TG–DTA) and scan electron microscopy (SEM). The XRD results revealed that the interlayer distance of resultant product was expanded to 30.46 Å. MIR combined with NIR spectra offered an effective method to illustrate this intercalation. The NIR spectra (6000–5500 cm−1) displayed prominent bands to expound SDBS intercalated into hydration product of C3A. And the bands around 8300 cm−1 were assigned to the second overtone of the first fundamental of CH stretching vibrations of SDBS. In addition, thermal analysis showed that the dehydration and dehydroxylation took place at ca. 220 °C and 348 °C, respectively. The SEM results appeared approximately hexagonal platy crystallites morphology for CaAl-SDBS-LDH, with particle size smaller and thinner.