细粒棘球蚴重组抗原B 8-kDa亚单位1对囊型包虫病的血清学诊断价值

目的通过基因工程技术获得细粒棘球蚴抗原B8-kDa亚单位1重组蛋白(rEgAgB8/1),探讨其对囊型包虫病(CE)的血清学诊断价值。方法将构建的rEgAgB8/1原核表达质粒(pET32b-rEgAgB8/1)转化至E.coli BL-21(DE3)中,用IPTG诱导表达,经亲和层析纯化获得高纯度rEgAgB8/1,以rEgAgB8/1为抗原,应用ELISA和Immuno blotting方法对31例手术确诊的囊型包虫病病人血清进行了回顾性检测与分析。结果ELISA和Immuno blotting方法检测CE病人血清阳性率均为90.3%(28/31),3例血清学检测阴性的CE病人均为初次诊断为CE及单纯性肝脏单发感染的病人;血清抗体水平随着病人棘球蚴囊数目增加而有所增加,棘球蚴囊的数目与血清抗体水平的比较用单因素方差分析有显著性差异(F=5.06,P=0.0142),1个囊与2个囊/3个囊组间血清抗体水平有显著差异,2个囊与3个囊组间差异无统计学意义。结论rEgAgB8/1重组蛋白抗原对囊型包虫病有较高的血清学诊断价值,多囊型包虫病人血清抗体水平高于单囊型包虫病人。

恒河猴STLV-1血清抗体流行病学研究

目的调查我国恒河猴ＳＴＬＶ－１流行病学特征。方法用免疫荧光法和蛋白印迹法对５３７只野捕恒河猴，３６５只繁殖猴和４４只Ｄ型逆转录病毒抗体阳性猴作了ＳＴＬＶ－１血清抗体检查。结果１０岁以上恒河猴的ＳＴＬＶ－１抗体阳性率（１５．５％）高于１０岁以下的恒河猴（６．２％）；雌猴的ＳＴＬＶ－１抗体阳性率（１７．５％）高于雄猴（５％）； Ｄ型逆转录病毒抗体阳性猴群的ＳＴＬＶ－１抗体阳性率（３４．１％）高于野捕猴群（８．８％）。结论在我国的野生和饲养恒河猴群中广泛存在ＳＴＶＬ－１血清抗体阳性动物，其抗体阳性率与动物的年龄和性别有关。

新疆部分地区马疱疹病毒1型感染的血清学调查

旨在了解新疆地区马疱疹病毒1型感染的流行现状和特点,本研究于2019—2020年从新疆乌鲁木齐、昌吉州、伊犁州、巴州16处规模化马场收集1657份马血清样品,采用酶联免疫吸附试验(ELISA)进行抗体检测,对不同地区、品种、性别及年龄马匹的马疱疹病毒1型抗体阳性率进行统计分析。结果显示,乌鲁木齐、伊犁州、昌吉州、巴州马疱疹病毒1型抗体阳性率分别为39.34%、22.56%、90.52%、5.00%;纯血马、混血马、哈萨克马、伊犁马、焉耆马、普氏野马的EHV-1抗体阳性率分别为20.34%、32.93%、44.92%、19.35%、5.00%、90.52%;普氏野马与家马的EHV-1抗体阳性率分别为90.52%和29.32%;家马中新疆本土品种马与引进品种马的EHV-1抗体阳性率分别为31.70%和25.50%;母马与公马的EHV-1抗体阳性率分别为38.84%和22.00%;处于幼年、青年、成年、老年阶段的马匹EHV-1抗体阳性率分别为35.37%、33.00%、34.31%、23.81%。结果提示,新疆乌鲁木齐、伊犁州、昌吉州、巴州规模化养殖场普遍存在EHV-1感染,且不同地区、品种、性别及年龄的马EHV-1感染率差异显著(P<0.05)。本研究为新疆地区EHV-1感染的探讨和防控工作提供调查数据。

交叉中和血清1型和血清3型鸭甲肝病毒单克隆抗体的制备与鉴定

鸭甲型肝炎(duck hepatitis A,DHA)是危害养鸭业的主要疾病之一,是一种雏鸭的急性、高度致死性传染病。本研究旨在研制一种对我国流行的鸭甲型肝炎血清1型(DHAV-1)和血清3型(DHAV-3)病毒具有交叉中和作用的单克隆抗体(monoclonal antibody,McAb)。人工合成12条DHAV-1和DHAV-3的VP1蛋白共有的抗原表位肽,分别与钥孔血蓝蛋白(keyhole limpet hemocyanin,KLH)载体偶联作为免疫抗原,免疫BALB/c小鼠制备McAb。通过检测McAb与DHAV-1和DHAV-3的交叉反应性,测定McAb对病毒增殖的抑制效率、中和效价以及攻毒保护率等来筛选McAb。本研究共获得了12株稳定分泌McAb的杂交瘤细胞株,其中6株(C1、C4、C7、C12、C13、C16)分泌的McAb同时与DHAV-1和DHAV-3发生特异性交叉反应;C1、C4、C7、C16可以抑制DHAV-1和DHAV-3在鸭胚中的增殖,抑制率在75.34%~100.00%不等;对DHAV-1和DHAV-3的中和效价:C1(1∶3&1∶5)、C4(1∶3&1∶3)、C7(1∶10&1∶11)和C16(1∶9&1∶9);C7和C16对DHAV-1和DHAV-3攻毒雏鸭的保护率较高,分别为“70%、80%”和“100%、60%”。本研究成功研制出对DHAV-1和DHAV-3具有交叉中和活性的McAb 4株,其中2株对病毒的感染具有良好的预防效果,为DHA的防控提供了新材料和新思路。

Petrogenesis of Late Cretaceous Jiangla＇angzong I-Type Granite in Central Lhasa Terrane, Tibet, China： Constraints from Whole-Rock Geochemistry, Zircon U-Pb Geochronology, and Sr-Nd-Pb-Hf Isotopes

The Jiangla＇angzong granite in the northern part of the Central Lhasa Terrane is composed of syenogranite and adamellite. LA-ICP-MS zircon U-Pb analyses suggest that syenogranite has a weighted mean 2±6pb/23SU age of 86±1 Ma （mean square weighted deviation=0.37）, which is in accordance with the muscovite Ar-Ar age （85±1 Ma） of Cu-Au ore-bearing skarns and the zircon U-Pb age （84±1 Ma） of adamellite. This suggests that the Jiangla＇angzong magmatism and Cu-Au mineralization events took place during the Late Cretaceous. The granite contains hornblende, biotite, and pyroxene, and does not contain Al-bearing minerals, such as muscovite, cordierite, and garnet. It has high contents of SiO2 （65.10 -70.91wt%）, K20 （3.44-5.17wt%）, and total K20＋Na20 （7.13-8.15wt%）, and moderate contents of A12Oa （14.14-16.45wt%） and CaO （2.33-4.11wt%）, with a Reitman index （δ43） of 2.18 to 2.33, and A/ CNK values of 0.88 to 1.02. The P205 contents show a negative correlation with SiO2, whereas Pb contents show a positive correlation with SiO2. Th and Y contents are relatively low and show a negative correlation with the Rb contents. These characteristics suggest that the Jiangla＇angzong granite is a high K calc-alkaline metaluminous I-type granite. It is enriched in light rare earth elements （LREE） and large ion lithofile elements （LILE）, and depleted in heavy rare earth elements （HREE） and high field strength elements （HFSE）, with LREE/HREE ratios of 11.7 to 18.1. The granite has negative Eu anomalies of 0.58 to 0.94 without obvious Ce anomalies （δCe=l.00-1.04）. The relatively low initial a7Sr/a6Sr ratios of 0.7106 to 0.7179, positive ε±nt（t） values of 1.0 to 4.1, and two-stage Hf model ages （TDM2） ranging from 889 Ma to 1082 Ma, These geochemical features indicate that the granite derived from a juvenile crust. The （143Nd/144Nd）t values from the Jiangla＇angzong granite range from 0.5121 to 0.5123, its eNd（t） values range from -10.17 to -6.10, its （^206pb /^204pb）t values range from 18.683 to 18.746, its （^207pb /^204pb）t values range from 15.695 to 15.700, and its （^208pb /^204pb）t values range from 39.012 to 39.071. These data indicate that the granite was formed by melting of the upper crust with the addition of some mantle materials. We propose that the Jiangla＇angzong granite was formed during the post- collision extension of the Qiangtang and Lhasa terranes.

Two Types of Granites in the Western Yangtze Block and Their Implications for Regional Tectonic Evolution： Constraints from Geochemistry and Isotopic Data

In the western Yangtze Block, widespread Mesoproterozoic to Neoproterozoic rocks are the key to understanding the Precambrian tectonic-magmatic evolution of the region. However, their petrogenesis and tectonic setting are still controversial. In this paper, zircon U-Pb ages, Sm-Nd isotopic and whole-rock geochemical data are reported from selected fresh samples in the southern Dechang county, southwestern China, in order to constrain their emplacement age and magma source, as well as their petrogenesis and tectonic setting. They are mainly composed of biotite monzogranite, monzonitic granite, biotite granodiorites, and quartz diorite. Two ages of 1055 ± 43 Ma and 837.6 ± 3.8 Ma were obtained through zircon U-Pb dating by LA-ICP-MS and LA-MC-ICP-MS, respectively. According to their major element compositions, the Grenville-age granites are peraluminous calc-alkaline series calcic S-type granite. In contrast, the mid-Neoproterozoic granites are metaluminous calc-aikaline series alkalic I-type granite. Furthermore, the S-type granites are enriched in LREEs relative to HREEs with （La/Yb）N ratios of 3.85-18.56 and underwent major fractionation with strongly negative Eu anomalies （Eu/Eu＊ = 0.38-0.66）. In the MORB-normalized trace element variation diagram, all the samples are enriched in Ce and large ion lithophile elements such as Rb, Th, and K, and depleted in high field strength elements such as Nb, and Ti, with negative Sr and Ti anomalies. The I-type granites are enriched in LREEs with slight negative Eu anomalies （Eu/Eu＊= 0.83-0.93）. They are characterized by the enrichment of highly incompatible elements （such as K, Rb, Ba, Th） and LREEs, relative to MORB. Neodymium isotopic data show that the S-type granites display 143Nd/144Nd values of 0.51241-0.51256, and have eNa （t = 1055 Ma） values of （-3.29） to （-3.81）. Calculated tDM ages yield values from 1.87 to 1.91 Ga with the tDM.2stg ages of 1.86 to 1.9 Ga. The I-type granites have 143Nd/144Nd ratios between 0.51192 and 0.51195, corresponding to initial eNd （t = 837 Ma） values of 1.22 to 5.63. Calculated tDM ages yield values from 1.0 to 1.38 Ga and the tDM.2stg ages yield values from 0.99 to 1.06 Ga. The S-type granites are distinguished as syn-collision granite, whereas the I-type granites were formed as arc magmas according to the Rb-（Yb＋Ta） and R1-R2 tectonic discrimination diagrams. To conclude, there are two types of spatially associated granite, the Mesoproterozoic S-type granite which were derived from re- melting of upper crustal mudstone and/or clastics and resulted from the convergence of two continental plates, and the mid-Neoproterozoic I-type granite which formed in continental arc and resulted from mantle-derived magma mixed crust material, in the western Yangtze Block. Furthermore, we suggest that collision between the Yangtze and Cathaysia blocks occurred at about 1055 Ma, and caused the S- type granite. The I-type granite related to the subduction of oceanic lithosphere eastward underneath the Yangtze Block in the mid-Neoproterozoic.

Effect of Chinese Herbal Treatment on Th1- and Th2-Type Cytokines,Progesterone andβ-Human Chorionic Gonadotropin in Early Pregnant Women of Threatened Abortion

Objective： To study the clinical effects of Prescription Zhuyun-Ⅲ （助孕3号方, ZYⅢ） on early pregnant women diagnosed as threatened abortion, and its mechanism in immunity and endocrine by determining serum Th1- and Th2-type cytokines, progesterone, and β-human chorionic gonadotropin （β-HCG）. Methods： The treatment group comprised 30 early pregnant women diagnosed as threatened abortion of deficiency syndrome of Pi （脾）, Shen （肾）, or both. The control group consisted of 20 normal early pregnant women of similar gestational age. Patients in the treatment group were administered with ZYⅢ for 4 weeks. Peripheral blood samples were collected pre- and post-treatment from both the treatment and the control groups. Serum Thl-type cytokine [interleukin-2 （IL-2）] and Th2-type cytokine [interleukin-10 （IL-10）] were determined by flow cytometry, and serum progesterone and 13-HCG were determined by ELISA. Results： （1） The treatment was effective in 26 and ineffective in 4 patients of the treatment group. Therefore, the cure percentage was 86.67%. （2） In the treatment group before the treatment, IL-2 was significantly higher, IL-10 tended to be less, and the Th1/Th2 balance shifted toward Thl compared with those in the control group. （3） After the treatment, IL-2 was decreased, IL-10 was increased, and IL-2/IL-10 was decreased. Both progesterone and β-HCG were increased. Changes of progesterone were positively correlated with changes of IL-10, whereas changes of β-HCG were negatively correlated with changes of IL-2. Conclusions： Our study suggests that ZYⅢ has an evident function of protecting the fetus, and one of its mechanisms is inhibiting the secretion of Thl cytokines, promoting the secretion of Th2 cytokines, and recovering the pathological shift of the Th1/Th2 balance. The other possible mechanism is increasing serum progesterone and β-HCG concentrations. Moreover, there are some correlations between the above two effects.

Petrogenesis of Kejie Granite in the Northern Changning-Menglian Zone, Western Yunnan: Constraints from Zircon U-Pb Geochronology, Geochemistry and Hf Isotope

The Kejie pluton is located in the north of the Changning-Menglian suture zone. The rock types are mainly biotite-granite. Zircon LA-ICP-MS U-Pb dating indicates that the Kejie pluton emplaced at about 80-77 Ma, Late Cretaceous. The Kejie pluton samples are characterized by high SiO2 （71.68%-72.47%）, K2O （4.73%-5.54%）, total alkali （K2O ＋ Na2O = 8.21%-8.53%）, K2O/Na2O ratios （1.36-1.94） and low P2O5 （0.13%-0.17%）, with A/CNK of 1.025-1.055; enriched in U, Th, and K, depleted in Ba, Nb, St, Ti, P and Eu. They are highly fractionated, slightly peraluminous 1-type granite. The two samples of the Kejie pluton give a large variation of εHf（t） values （-5.04 to 1.96） and Hf isotope crustal model ages of 1.16-1.5 Ga. Zircon Hf isotopes and zircon saturation temperatures of whole-rock （801℃-823℃） show that the mantle-derived materials maybe have played a vital role in the generation of the Kejie pluton. The Kejie pluton was most likely generated in a setting associated with the eastward subduction of the neo-Tethys ocean, where intrusion of mantle wedge basaltic magmas in the crust caused the anatexis of the latter, forming hybrid melts, which subsequently experienced high-degree fractional crystallization.

Geochronology and Sr-Nd-Hf isotopic composition of the granites,enclaves,and dikes in the Karamay area,NW China:Insights into late Carboniferous crustal growth of West Junggar

New whole-rock major and trace elements, and zircon U Pb and Hf-Nd isotope compositions are reported for the Karamay dikes, enclaves, and host granites in the West Junggar, NW China. Zircon U -Pb dating of the l（aramay pluton yields an age of 300.7 ~ 2.3 Ma for the enclave and 300.0 ~ 2.6 Ma for the host granite, which was intruded by dike with an age of 298 Ma. The host granites exhibit relatively low SiO2 contents and A/CNK and Ga/Al ratios, low initial 87Sr/86Sr ratios （0.703421 0.703526） and positive eHf（t） （5.5--14.1） and eNd（t） （7.3--8.1） values with a young model age, suggesting that they are I-type granites and were mainly derived from a juvenile lower crustal source. The enclaves and dikes belong to an andesitic calc-alkaline series and have high MgO concentrations at low silica content and positive eHf（t） （7.6--13.2, 14.2--14.9） and εNd（t） （6.8-8.3, ~6.9） values. They are enriched in LILEs （Rb, Ba and U） and LREE and depleted in HFSEs （Nb and Ta） with insignificant negative Eu anomalies, indicating that the melts were derived from an enriched lithospheric mantle modified by subducted oceanic crust-derived melts and minor fluids, followed by fractional crystallization. The Karamay host granites and enclaves are of mixed origin and are most probably formed by the interaction between the lower crust-and lithospheric mantle-derived magmas, and were intruded by the unmixed dikes subsequently. The upwelling mantle through a slab window in an island arc environment might have triggered partial melting of the lithospheric mantle and its subsequent interaction with the granitic magma, further suggesting that the ridge subduction played an important role in the crustal growth of West lun^gar.

Deviation matrix and asymptotic variance for GI/M/1-type Markov chains

We investigate deviation matrix for discrete-time GI/M/1-type Markov chains in terms of the matrix-analytic method, and revisit the link between deviation matrix and the asymptotic variance. Parallel results are obtained for continuous-time GI/M/1-type Markov chains based on the technique of uniformization. We conclude with A. B. Clarke＇s tandem queue as an illustrative example, and compute the asymptotic variance for the queue length for this model.

PROXIMINAL SUBSPACES OF 2-NORMED SPACES

In 1965 Gohler introduced 2-normed spaces and since then, this topic have been intensively studied and developed. We shall introduce the notion of 1-type proximinal subspaces of 2-normed spaces and give some results in this field.

Inactivated Pseudomonas PE(△Ⅲ)exotoxin fused to neutralizing epitopes of PEDV S proteins produces a specific immune response in mice

Porcine epidemic diarrhea(PED)caused by the porcine epidemic diarrhea virus(PEDV),is a severe infectious and devastating swine disease that leads to serious economic losses in the swine industry worldwide.An increased number of PED cases caused by variant PEDV have been reported in many countries since 2010.S protein is the main immunogenic protein containing some B-cell epitopes that can induce neutralizing antibodies of PEDV.In this study,the construction,expression and purification of Pseudomonas aeruginosa exotoxin A(PE)without domain Ⅲ(PE△Ⅲ)as a vector was performed for the delivery of PEDV S-A or S-B.PE(△Ⅲ)PEDV S-A and PE(△Ⅲ)PEDV S-B recombinant proteins were confirmed by sodium dodecyl sulfate-polyacrylamide gel electrophoresis and Western blot analysis.The immunogenicity of PEDV S-A and PEDV S-B subunit vaccines were evaluated in mice.The results showed that PEDV-S-B vaccine could not only induce specific humoral and Th1 type-dominant cellular immune responses,but also stimulate PEDV-specific mucosal immune responses in mice.PEDV-S-B subunit vaccine is a novel candidate mucosal vaccine against PEDV infection.

Environment-assisted excitation energy transfer in LH1-RC-type and LH2-type trimers

In this work,we study environment-assisted excitation energy transfer(EET) through calculating energy transfer efficiency(ETE) in LH1-RC-type and LH2-type trimers,which can be used to mimic energy transfer behaviors in the basic unit cells of LH1-RC and LH2 light-harvesting complexes.Quantum state evolution of the trimers is described by a non-Hermitian quantum master equation.ETE in these trimer systems is investigated by the use of numerical solutions at finite temperatures for the non-Hermitian master equation.We theoretically reveal the temperature-assisted ETE enhancement.It is found that highly efficient EET with nearly unit efficiency may occur in the nearby regime of the critical point of quantum phase transition.

Petrogenesis of the Mayo-Darley tin formations,anorogenic complex of the Cameroon Line:implication for tin deposit

The Mayo-Darley massif is an anorogenic complex of the Cameroon Line that has a mantle origin.Tin-bearing rocks were analyzed by ICP-AES and INAA analytical methods.The purpose of this work was to provide new geochemical data for the Mayo-Darley tin formation and to understand its petrogenesis and the origin of tin mineralization.The Mayo-Darley tin deposit is made up of tin-granite,and tin-greisen,greisenification was developed on the borders of quartz dykes.These rocks belong to the alkaline series and were classified into acid(SiO2-=61.6%–73.8%;65.4%–98%respectively)and basic(42.9%–47%SiO_(2))rocks.They showed enrichment in HSFE,LILE,Ga/Al and chondrite normalized REE patterns indicating LREE enrichment relative to HREE with a negative Eu anomaly,only sample SB8 of tin-granite showed Eu/Eu*=1.11.Rocks display metaluminous,peralkaline,peraluminous,ferroan,high-K calc-alkaline to shoshonitic,alkalic to calcic affinity,and crystallized at800°C.The chemistry of this deposit reflects the primary composition of granite,quartz monzonite,gabbro,and foid gabbro.This complex experienced multi-stage sub-solidus hydrothermal fluid reactions and shows variable alteration of feldspars alkali mobility.The rocks are classified as A1-type granite,overlap with the OIB field,and were derived from a within-plate setting,similar to mantle non plumederived magmas.The origin of tin mineralization in MayoDarley has a complex evolution,tin mineralization was derived from hydrothermal and hydrogenous metal-rich deposits and shows Sn–Hf–Zr and Sn–Tl–Nb association.These new data confirm the complexity of the Mayo-Darley tin complex and elucidate the origin of tin mineralization.

广西壮族自治区1～6岁儿童乙型病毒性肝炎血清流行病学调查

目的了解广西壮族自治区（广西）2012年1~6岁儿童乙型病毒性肝炎（乙肝）血清流行病学特征,为控制乙肝提供参考。方法调查广西122个县（区、市,下同）,每个县采用分层随机抽样方法按东、西、南、北、中方位各抽取1~6岁儿童25人,对儿童监护人进行问卷调查,利用化学发光法对调查儿童血清标本进行检测,并对调查结果进行流行病学分析。结果广西2012年1~6岁儿童乙肝病毒表面抗原[Hepatitis B Virus（HBV）Surface Antigen,HBs Ag]阳性率为0.60%,抗乙肝病毒表面抗原抗体（Antibody to HBs Ag,Anti-HBs）阳性率为59.76%,且随着年龄的增长HBs Ag阳性率逐渐上升,Anti-HBs阳性率逐渐下降（χ2=13.530,P=0.019;χ2=789.306,P=0.000）。不同地区、接种不同剂次和不同剂量乙肝疫苗（Hepatitis B Vaccine,Hep B）其Anti-HBs阳性率差异有统计学意义（χ2=10.469,P=0.655;χ2=429.417,P=0.000;χ2=818.100,P=0.000）。调查16 760儿童中,有Hep B接种史100.00%,首剂（First Dose）Hep B（Hep B1）及时接种率为89.68%,全程接种率为99.86%,全程合格接种率为84.87%。结论广西2012年1~6岁儿童HBs Ag阳性率为0.60%,开展儿童Anti-HBs监测,及时接种Hep B1,全程接种Hep B,可减少HBV感染机会。

2010年山东省1～6岁儿童麻疹血清流行病学调查

目的了解山东省2010年1～6岁儿童麻疹免疫现状,为免疫策略制定、麻疹预防控制提供借鉴与指导。方法按多级抽样原则,选取烟台、淄博、莱芜、滨州、菏泽5市1～6岁儿童360名开展血清IgG抗体水平检测。结果山东省2010年1～6岁儿童麻疹IgG抗体阳性率均在92.86%以上,东、中、西部地区及1、2,3、4,5、6岁年龄组间抗体阳性率差异均无统计学意义(P>0.05);血清抗体浓度在735.56～2 250.20 U/ml之间,1、2,3、4,5、6和1～6岁年龄组东、中、西部地区抗体浓度差异有统计学意义(F=4.31、6.89、8.97、12.69,均P<0.05)。结论山东省2010年1～6岁儿童麻疹抗体阳性率较高,东部地区抗体浓度明显低于中部及西部地区,需进一步关注。

流式细胞术分析HIV-1高暴露持续血清阴性人群淋巴细胞亚群

目的了解经性传播途径高暴露不易感人群淋巴细胞亚群的差异,分析其与艾滋病病毒Ⅰ型(HIV-1)不易感的关系,探讨经性途径高暴露HIV不易感的免疫基础。方法收集37例经性传播途径高暴露HIV-1持续血清阴性者(Highly exposed and persistently remain seronegative,简称HEPS人群)、65例HIV-1感染者(简称HIV阳性人群)及128例健康对照人群(简称HC人群)的抗凝全血,用流式细胞仪检测相关淋巴细胞亚群,并分析其相关性。结果HEPS人群与HC人群外周血淋巴细胞亚群差异没有统计学意义;HIV阳性人群外周血CD4+T淋巴细胞数量、CD4/CD8比值显著低于HEPS和HC两组人群(P<0.001),CD8+T淋巴细胞数量则显著高于该两组人群(P<0.001);HIV阳性人群外周血CD1+9B淋巴细胞、CD1+6CD5+6NK细胞数量显著低于HEPS人群和HC人群。HEPS人群的CD1+9B淋巴细胞数量与CD4+、CD8+T淋巴细胞数量呈显著正相关,而CD1+6CD5+6NK细胞数量与其CD4+、CD8+T淋巴细胞数量无相关性。结论经性途径高暴露HIV-1持续血清阴性人群的淋巴细胞亚群,和健康对照人群比较无显著性差异,HIV感染可明显降低CD4+T淋巴细胞、CD1+9B淋巴细胞和CD1+6CD5+6NK细胞数量。

F-doped O3-NaNi_(1/3)Fe_(1/3)Mn_(1/3)O_2 as high-performance cathode materials for sodium-ion batteries

The F-doped O3-type NaNi1/3Fe1/3Mn1/3O2-xFx （x = 0, 0.005, 0.01,002 and noted as NFM-F0, NFM-F0.005, NFM-F0.01, NFM-F0.02, respectively, united as NFM-Fs） cathode materials were investigated systematically. The rate performance and capacity retention of the O3-type cathode materials are significantly improved as a function of specific F-doping levels. Optimum performance is achieved in the NFM-F0.01 material having a capacity of -110mAhg-1 at a current density of 150mAg-1 after 70 cycles. The results indicate that the binding energy of oxygen changes as a result of F-doping, and in addition, F-doping results in changes to the stoichiometry of Mn3＋/Mn4＋, which stabilizes the O3-type layered structure, thus allowing cycling performance to be improved. However, NFM-F0.02, having a higher F-doping level, retains a high capacity retention, although a slight loss is observed. The results suggest there is an optimum F-doping level for the NFM-F system to deliver enhanced cycling performance.

Boundedness of Commutators of θ-Type Calderón-Zygmund Operators on Non-homogeneous Metric Measure Spaces

Let(X, d, μ) be a metric measure space satisfying both the upper doubling and the geometrically doubling conditions in the sense of Hyt?nen. In this paper, the authors obtain the boundedness of the commutators of θ-type Calderón-Zygmund operators with RBMO functions from L∞(μ) into RBMO(μ) and from Hat1,∞(μ) into L1(μ), respectively.As a consequence of these results, they establish the Lp(μ) boundedness of the commutators on the non-homogeneous metric spaces.

Micron-scale 1:5H-based precipitated phase with the lamellar structure of sintered Sm_(2)Co_(17)-based magnets and its potential application

The excellent thermal stability of magnetic properties of Sm_(2)Co_(17)-based magnets is their most impor-tant feature.However,this stability is reduced when the maximum energy product of Sm_(2)Co_(17)-based magnets is improved,which is mainly determined by the Fe/Cu distribution of the 2:17R cell and 1:5H cell boundary phases.During the demagnetization process,the Cu-rich 1:5H cell boundary phase with a width of 2-15 nm obstructs the motion of the domain walls,yielding coercivity.Herein,we report a micron-scale Cu/Zr-rich and Fe-lean 1:5H-based precipitated phase with a lamellar structure,probably induced by Sm_(2)O_(3) doping.This structure enables the separate regulation of Fe and Cu distribution for Sm_(2)Co_(17)-based magnets with Fe-rich 2:17R cell phases and Cu-rich 1:5H cell boundary phases,consid-erably optimizing the thermal stability of magnetic properties.This discovery can be further developed to produce Sm_(2)Co_(17)-based magnets with high performance and excellent thermal stability of magnetic properties.