线性交换子的加权估计

 多线性交换子T_b(f)(x)=∫_Rⁿ∏_i=1^m(b_i(x)-b_i(y))k(x,y)f(y)dy在L^p(Rⁿ)(1K是一个标准的Calderón-Zygmund核.主要研究交换子Mf(x)=sup_x∈Q∫_Q|f(y)|dy,其中f∈L_loc(Rⁿ),x∈Rⁿ,Q是任何包含x的方体,并用Sharp极大估计得到了该多线性交换子在Herz空间的一个加权有界性.     

一个单核三价铬配合物的晶体结构、发光性质及热稳定性

我们重新合成了曾经报道过的反式K[Cr(C₂O₄)_2·(H₂O)₂]_2·3H₂O三价铬配合物, 并借助先进的单晶衍射仪和更先进的解析手段得到了该配合物更加精确的结构模型,该配合物属于单斜晶系,P2/n（No. 13）空间群,晶胞相关参数为：a = 7.8827 (4) Å,b = 5.7296(3) Å,c = 13.6447(7) Å,β= 103.506(5)°,Z = 2,Dc =1.980 Mg/m³,V = 599.22(5) ų。热重测试结果显示该配合物在357 K以前是稳定的,在410 nm最有效的紫外光光源的激发下,配合物在610 nm处有一个尖锐的发射峰。     

N,N′-双水杨醛缩二氨基乙醚的合成和晶体结构

合成了一种新的西佛碱配体N,N''双水杨醛缩二氨基乙醚,并采用x射线单晶衍射法测定了它的晶体结构。该晶体属正交晶系空间群P_bcn,a=5.667(2)Å,b=9.192(3)Å,c=31.829(11)Å,v=1658.2(7)ų,分子式为C₁₈H₂₀N₂O₃,Mr=312.36,Z=4,D_C=1.251g·cm^-3,晶体结构测定和UV,IR谱均表明分子内形成氢键。在甲醇溶液中有一个荧光发射带,λ_max=443nm。     

一种用于次氯酸根检测的螺二芴类双光子荧光探针的合成及性能研究

设计并合成了一种用于次氯酸根（ClO^-）检测的螺二芴类双光子荧光探针.加入50 μmol·L^-1ClO^-后,可以裸眼观察到探针溶液颜色从黄色变为无色,在波长365 nm的紫外光照射下荧光明显增强（10倍）.在物质的量浓度为0~20 μmol·L^-1范围内,荧光强度（Y）与ClO^-物质的量浓度（X）存在较好的线性相关性,其拟合方程为：Y=7.142 41X+65.675 57.根据3σ/k准则,计算出检测限为2 μmol·L^-1,表明探针对ClO^-有很好的灵敏性.该探针对ClO^-的荧光响应不受其他干扰物存在的影响,对ClO^-有很好的选择性.探针的荧光响应在广泛的pH范围内表现稳定,适宜在pH值为6~9对ClO^-的检测.用Z-扫描技术,测得探针的双光子吸收截面为300 GM.实验结果表明：该探针对环境和生物中ClO^-的检测具有很好的应用前景.     

3种兜兰属植物光合特性的比较研究

通过研究硬叶兜兰(Paphiopedilum micranthum)、带叶兜兰(P.hirsutissimum)和长瓣兜兰(P.dianthum)3种兜兰属植物的光合特性,为其种质资源保育及引种栽培提供理论依据。以广西雅长兰科植物国家级自然保护区内3种兜兰属植物为试验材料,测定其叶片的光响应曲线、CO₂响应曲线以及叶绿素含量,比较3种兜兰光合特性的差异。结果表明：硬叶兜兰、带叶兜兰和长瓣兜兰的最大净光合速率(P_max)分别为2.719 μmol·m^-2·s^-1、1.836 μmol·m^-2·s^-1、2.015 μmol·m^-2·s^-1,光饱和点(LSP)分别为578.74 μmol·m^-2·s^-1 、467.72 μmol·m^-2·s^-1、481.25 μmol·m^-2·s^-1,光补偿点(LCP)均较低,分别为15.65 μmol·m^-2·s^-1、12.79 μmol·m^-2·s^-1、10.34 μmol·m^-2·s^-1,是典型的阴生植物。硬叶兜兰的最大净光合速率(P_max)、CO₂饱和点(CSP)、羧化效率(CE)均显著高于长瓣兜兰和带叶兜兰(P<0.05),硬叶兜兰对CO₂的利用能力更强。叶片叶绿素相对含量(SPAD值)表现为硬叶兜兰(58.13)>长瓣兜兰(55.12)>带叶兜兰(51.88)。3种兜兰属植物的光合能力较弱,对光的利用范围狭窄,在引种栽培时应注意增加荫蔽度。     

NaBH4还原改性TiO2(B)及光催化性能研究

以TiCl₄为原料,在（CH₂OH）₂溶液中通过一步水热法制备单斜相二氧化钛[TiO₂(B)]。使用不同质量含量NaBH₄对TiO₂(B)进行还原改性,调控其内含Ti³⁺的浓度,合成了含Ti³⁺的TiO₂(B)-NaBH₄X样品。采用X射线衍射仪（X-ray diffraction,XRD）、拉曼光谱仪（Raman spectroscopy）、紫外-可见漫反射光谱仪（UV-visible diffuse reflectance spectroscopy,UV-DRS）、X射线光电子能谱仪(X-ray photoelectron spectroscopy,XPS）对材料进行表征。改性后TiO₂(B)-NaBH₄X样品保持其原有晶体结构,并未发生相变,仅有结晶度的改变。原始TiO₂(B)禁带宽度为3.15 eV,通过改性,Ti³⁺的存在改变了禁带宽度,成功地将禁带宽度降低到2.82 eV,将吸光区域扩展到可见光区域。通过可见光光催化分解水制氢与可见光降解甲基橙试验,确立了TiO₂(B)-NaBH₄3样品有最好的可见光光催化活性,产氢速率达到0.58 μmol·h^-1·g^-1,6 h降解率达到40%。     

3种观赏性石斛的光合特性比较研究

为探明3种观赏性石斛属Dendrobium Sw.植物在光合生理方面的差异,为其栽培及规模化种植提供理论依据。本研究以3种观赏性石斛(叠鞘石斛D.denneanum Kerr.、流苏石斛D.fimbriatum Hook.和束花石斛D.chrysanthum Wall.ex Lindl.)为材料,测定其叶片的光响应曲线、CO₂响应曲线及叶绿素相对含量(SPAD值),探究其光合特性。结果表明,叠鞘石斛、流苏石斛和束花石斛3种石斛属植物的光补偿点(LCP)分别为2.15 μmol·m^-2·s^-1、3.74 μmol·m^-2·s^-1、1.79 μmol·m^-2·s^-1,光饱和点(LSP)分别为995.09 μmol·m^-2·s^-1、679.44 μmol·m^-2·s^-1、712.28 μmol·m^-2·s^-1,LCP均低于5 μmol·m^-2·s^-1,LSP均低于1 000 μmol·m^-2·s^-1,属于典型的阴生植物,具有较强的耐阴性;3种石斛的最大净光合速率(P_max)分别为3.54 μmol·m^-2·s^-1、3.86 μmol·m^-2·s^-1、4.03 μmol·m^-2·s^-1,表观量子效率(AQY)分别为0.042,0.044和0.051,束花石斛的P_max和AQY最大,光合作用能力较强。3种石斛的CO₂响应曲线中,最大净光合速率(A_max)大小依次为叠鞘石斛(11.99 μmol·m^-2·s^-1)、流苏石斛(10.87 μmol·m^-2·s^-1)、束花石斛(4.75 μmol·m^-2·s^-1),叠鞘石斛利用CO₂进行光合作用的能力最强;3种石斛的CO₂饱和点(CSP)无显著性差异,在CO₂浓度不大于2 000 μmol·mol^-1时均未到达饱和点;CO₂补偿点(CCP)具有显著性差异,CCP分别为100.12 μmol·m^-2·s^-1、158.02 μmol·m^-2·s^-1、134.44 μmol·m^-2·s^-1,其中叠鞘石斛的CCP最低,对低浓度CO₂的利用能力最强。3种石斛叶片的SPAD值分别为51.09,56.93和58.06,其高低与其净光合速率的大小有一定程度的相关性。在3种石斛中,束花石斛的光合作用能力最强,对弱光的利用能力较强;流苏石斛对弱光的利用能力较弱,光照适应范围狭窄;叠鞘石斛对强光的利用能力较强,光合作用适应范围较广。此外,3种石斛均具有较强的耐阴性,对CO₂的耐受性也较强,在种植时应提供适当的遮阴和增加CO₂浓度来提高石斛的光合作用能力。     

保E*关系且方向保序严格部分一一变换半群的秩

设X为有限集合,E为X上的等价关系,令SOPI_E^*(X)为X 上的所有保E^*关系且方向保序严格部分一一变换构成的半群. 为了讨论此变换半群的秩,引入了新的等价关系从而得到新的等价类. 通过对等价类的分析得到了半群SOPI_E^*(X)的秩.     

三核铜配合物[Cu3(TBSSB)2(BSA)2(bipy)2]·H2O的合成、晶体结构及性质研究

以牛磺酸缩5-溴水杨醛席夫碱（TBSSB）、5-溴水杨醛（BSA）、2,2''-联吡啶（bipy）为混合配体,合成了三核铜配合物[Cu₃（TBSSB）₂（BSA）₂（bipy）₂]·H₂O （1）,并对该化合物进行了元素分析、红外光谱、X-射线单晶衍射、光致发光光谱、固体漫反射光谱及分子轨道分析等表征。晶体结构分析表明,该化合物结晶属三斜晶系,Pī空间群,晶胞参数为a=10.031（2）Å,b=11.480（2）Å,c=12.913（3）Å,α=73.13（3）°,β=78.58（3）°,γ=75.24（3）°,V=1363.6（5）ų,Z=1,M_r=1533.30,Dc=1.867 g/cm³,F（000）=759,μ=4.236 mm^-1,S=0.921,R₁=0.0488,wR₂=0.0471（I > 2σ（I））,R₁=0.1812,wR₂=0.0546。Cu （2）离子与来自于两个TBSSB配体的两个氮原子和两个氧原子配位,形成正方形配位构型。Cu （1）离子与来自于一个2,2''-bipy的两个氮原子,TBSSB配体的一个氧原子,以及BSA的两个氧原子配位,形成四方锥形配位构型。该化合物分子通过O-H…Br分子内氢键和C-H…O分子间氢键相互连接形成三维超分子结构。研究发现该化合物能够发出蓝色荧光,它的带隙为2.19 eV。     

B10白铜晶界特征分布对耐腐蚀性能的影响

B10白铜（Cu-Ni合金）管材作为一种船舶常用的管道用材料,耐腐蚀性一直是困扰其被广泛应用的一大原因。以4种不同的B10白铜管材为试验样品,采用电子背散射衍射及电化学腐蚀试验研究了B10白铜晶界特征分布及其对腐蚀性能的影响。结果表明：低重位点阵(coincidence site lattice,CSL) 晶界比例越高,其耐腐蚀性能越强,特别是低CSL ?3ⁿ(n=1, 2, 3)晶界的大量存在,降低了普通晶界的网络连通性,阻碍了腐蚀沿晶界的扩展,提高了B10白铜对海水的耐腐蚀性。当样品B中?3ⁿ晶界的长度为47.07%时,其腐蚀电势为 -0.289 V、腐蚀电流密度为3.341×10^-6 A/cm²、腐蚀膜阻抗为33.102 Ω/cm²、腐蚀膜厚度为17.5 μm。     

In situ simultaneous determination of trace elements, U-Pb and Lu-Hf isotopes in zircon and baddeleyite

This paper describes a combined method of simultaneously measuring U-Pb and Lu-Hf isotopes as well as trace elements in Phalaborwa baddeleyite and 91500, GJ-1, TEMORA-1 and SK10-2 zircons by means of Neptune MC-ICPMS and Agilent Q-ICPMS connected to a 193 nm excimer laser ablation system. Material ablated by laser was carried in different proportions into Q-ICPMS for U-Pb isotopic and trace elemental and MC-ICPMS for Lu-Hf isotopic compositions. Experiments indicate that different proportions of ablated material for the Q-ICPMS and MC-ICPMS （6：4, 5：5 and 4：6 respectively） do not show any bias for the zircon/baddeleyite U-Pb age, Lu-Hf isotope and trace elemental compositions within analytical errors. Using 40-60 μm spot size, the obtained U-Pb ages of Phalaborwa baddeleyite, 91500, GJ-1, TEMORA and SK10-2 zircons are 2065±15 （2σ, n=20）, 1063±6 （2σ, n=-19）, 613±6 （2σ, n=20）, 416±5 （2σ, n=20） and 32.6±0.5 （2σ, n=20） Ma, respectively. The ^176Hf/^177Hf ratios are 0.281231±24 （2SD, n=20）, 0.282310±35 （2SD, n=19）, 0.282028±34 （2SD, n=20）, 0.282687±34 （2SD, n=20） and 0.282752±53 （2SD, n=20）, respectively. The obtained trace elemental compositions are identical to the reference values. Therefore, this kind of technique makes it possible to simultaneously obtain the U-Pb age, Lu-Hf isotopes and trace elemental compositions of zircon and baddeleyite, which could be an important tool in solving problems in earth sciences.     

Export and remineralization of POM in the Southern Ocean and the South China Sea estimated from 210Po/210Pb disequilibria

Disequilibria between ^210Po and ^210Pb in the upper water and their potential applications as a proxy of particle export and remineralization were examined in the Southern Ocean （station IV3） and the South China Sea （NS44）. ^210po was deficit in surface waters but excessive relative to ^210Pb in subsurface waters. Good positive correlation between ^210Po and particulate organic carbon （POC） indicated deficits and excess of ^210Po resulted from particulate organic matter （POM） export and remJneralization respectively, which was also supported by the decreased δ^13C and increased δ^15N downwards as a result of particle remineralization. On the basis of ^210Po/^210Pb box-model, POC export flux out of the surface waters were 1.2 mmol C. m^-2. d^-1 and 2.3 mmol C. m^-2. d^-1 for station NS44 and IV3, respectively. In the subsurface waters, remineralization fluxes of ^210Po were 0.062 Bq. m^-2.d^-1 and 0.566 Bq.m^-2.d^-1 for station NS44 and IV3 along with the recycle efficiency of 52±26% and 119±52%, respectively. Remineralized fluxes of POM derived from ^210Po and exported POC were 0.6 mmol C.m^-2.d^-1 and 2.7 mmol C. m^-2. d^-1 for NS44 and IV3. This study suggested that ^210Po was a powerful tracer of particle export and remineralization.     

Characterization of type<Emphasis Type="Italic">p</Emphasis> Banach spaces by the weak law of large numbers

For weighted sums of the form where {a _nj , 1 ⩽j⩽k _n ↑∞,n⩾1} is a real constant array and {X _aj , 1≤j≤k _{n, n}≥1} is a rowwise independent, zero mean, random element array in a real separable Banach space of typep, we establishL ^r convergence theorem and a general weak law of large numbers respectively, conversely, we characterize Banach spaces of typep in terms of convergence inr-th mean and probability for such weighted sums. Foundation item: Supported by the National Natural Science Foundation of China (No. 10071058) Biography: Gan Shi-xin (1939-), male, Professor, research direction: martingale theory, probability limiting theory and Banach space geometry theory.     

The concentration quenching characteristics of 5D3-7FJ and 5D4-7FJ (J=0―6) transitions of Tb3+ in YBO3:Tb3+ phosphor

The photoluminescence quenching behaviors of ^5D3-^7Fj and ^5D4-^7Fj （J = 0—6） transitions of Tb^3＋ in YBO3：Tb under 130—290 nm excitation were systematically investigated. The results revealed that the quenching concentrations of both ^5D3-^7Fj and ^5D4-^7Fj transitions of Tb^3＋ in YBO3：Tb were mainly dependent on excitation wavelength. Particularly, the quenching concentrations of ^5D4-^7Fj transitions of Tb^3＋ under 130—290 nm excitation were correlated with excitation bands of YBO3：Tb. The quenching concentrations of ^5D3-^7Fj transitions remained at low concentration （2%） under 186—290 nm excitation and then increased gradually with energy of incoming excitation photon when excited at 130—186 nm. This dependence should be involved in their excitation mechanisms and quenching pathway in particular excitation region.[第一段]     

A sufficient condition fork′(z)(k(z)∈H q,q≥1) to be ofH 1

We proved ifk(z)∈H ^q (q≥1),g(z) is analytic on |z|=1, , thenk′(z)∈H ¹, especially, ifq=1, thenk(z) is an analytic function on the closed unit disk |z|≤1. Peng Zhigang: born in June 1970, Ph. D     

Synoptic-scale variation of δ18O in summer monsoon rainfall at Lijiang, China

Based on the daily δ~(18)O data in June―September 2003 at Lijiang and the daily mean NCEP/ NCAR reanalysis data, synoptic-scale variation of δ~(18)O in summer monsoon rainfall was investigated. The 'precipitation amount effect' is obvious for the daily δ~(18)O variation, whereas the 'temperature effect' is insignificant. Alternate occurrences of active phase and break phase of the southwest monsoon probably influence the synoptic-scale δ~(18)O variation prominently. Moreover, the isotopic composition in precipitation during the late monsoon months is presumably influenced significantly by recycling of monsoon precipitation. Both the above factors disturb the 'amount effect' of isotopic variation in the monsoon region. This study also indicates that the synoptic-scale rainfall δ~(18)O variation at Lijiang in summer is domi-nated by the Indian monsoon depression (low pressure) system at large scale. These results are important for further studying the 'amount effect' and reconstructing paleoclimate in the monsoon region.     

Multi-parameter infinite-dimensional (r,δ)-OU process

The definition of n-parameter infinite-dimensional (r,δ) -Ornstein-Uhlenbeck process {xt (·) } ((r, δ)-OUPn∞ for short) is given. The absolute continuity of distribution μt of Xt(·) and the limit of Xt(·) when |t| →∞ is discussed.     

不同轮伐期对巨尾桉人工林碳固存的影响

【目的】深入探讨不同轮伐期对巨尾桉人工林碳固存的影响,为从应对全球气候变化的视角确定合理轮伐期提供理论依据。【方法】以轮伐期为短(7a)、中(13a)和长周期(21a)的巨尾桉人工林为研究对象,通过对不同轮伐期桉树林分生物量、碳固存、年平均固碳量的分析,揭示不同轮伐期对桉树林分碳固存的影响。【结果】巨尾桉人工林的生物量碳随着轮伐期的延长而逐渐增加,由7a轮伐期的(75.81±5.12)t·C/hm~2增至13a轮伐期的(180.11±19.97)t·C/hm~2以及21a轮伐期的(192.08±16.50)t·C/hm~2,方差分析表明,13a和21a轮伐期的总生物量碳显著高于7a轮伐期,而13a和21a轮伐期之间的差异不显著。巨尾桉人工林土壤有机碳随轮伐期延长而显著降低,由7a轮伐期的(89.99±0.35)t·C/hm~2、13a轮伐期的(85.42±0.76)t·C/hm~2下降到21a轮伐期的(74.64±0.24)t·C/hm~2。7~13a仍是巨尾桉人工林固碳能力迅速增长期,年平均总生物量碳由7a时的10.78t·C/(hm~2·a)迅速提高到13a的19.54t·C/(hm~2·a),增长81%;21a时巨尾桉人工林进入固碳能力下降期,年平均总生物量碳降至3.78t·C/(hm~2·a),固碳能力只是13a的19.34%。【结论】在南亚热带,巨尾桉人工林的最佳轮伐期确定在13a左右较为适宜,这与经济效益的最大化一致。     

Comparison of the carbon isotope composition of total organic carbon and long-chain <Emphasis Type="Italic">n</Emphasis>-alkanes from surface soils in eastern China and their significance

Surface soil samples collected over a high spatial resolution in eastern China were analyzed for carbon isotope composition （δ^13C） of total organic carbon （TOC） and higher plant-derived long-chain n-alkanes, with the latter reported as weighted mean values. The two sets of δ^13C values are significantly correlated and show similar trends in spatial variation. The spatial distribution of δ^13C shows less negative values in the mid-latitudes between 31°N and 40°N and more negative ones at higher and lower latitudes. This is consistent with previously reported carbon isotope data from surface soil phytoliths in the same region and suggests that the mid-latitude area provides relatively favorable growing condi- tions for C4 plants. Furthermore, δ^13C values of both TOC and long-chain n-alkanes from 12 surface soil samples collected from a small grassland in north China displayed similar carbon isotope values and the difference between paired δ^13C of a soil samples remains relatively constant. Our data demonstrate that in eastern China, soil δ^13C composition of both TOC and long-chain n-alkanes is effective indicators of C3/C4 ratios of the prevailing vegetation. This work suggests that -22‰ and -32‰ are good es- timated end members for the weighted mean δ^13C values of long-chain n-alkanes （C27, C29 and C31 n-alkanes） from soils under dominant C4 or C3 vegetation, allowing us to reconstruct paleovegetation trends.     

Preliminary results of the study on wind erosion in the Qinghai-Tibetan Plateau using137Cs technique

The worldwide fallout of caesium-137 (¹³⁷Cs) associated with the nuclear weapon tests during the 1950s and 1960s has provided a valuable man-made tracer for studies of soil erosion and sediment delivery. But relatively few researchers have used it to estimate wind erosion. In this note, the¹³⁷Cs technique is introduced into the studies of wind erosion and its modern processes in the Qinghai-Tibetan Plateau. Two¹³⁷Cs reference inventories of 982.11 and 2 376.04 Bq · m⁻² were established preminarily, distributed in the south and middle-north parts of the studied area respectively. By analyzing the patterns of¹³⁷Cs depth profiles from sampling sites, the aeolian processes of erosion and deposition in nearly 40 years have been revealed, i.e. the shrub coppice dunes (S1) and semi-fixed dunefields (S3) experienced the alternation of erosion and deposition, while the grasslands (S4, S6 and S7) and dry farmlands (S5) suffered erosion only. By using¹³⁷Cs model, the average wind erosion rates for shrub coppice dune (S1), semi-fixed dune fields (S3), dry farmlands (S5) and grasslands (S4, S6 and S7) were estimated to be 84.14, 69.43, 30.68 and 21.84 t · ha¹ · a⁻¹ respectively, averaging 47.59 t · ha⁻¹ · a⁻¹ for the whole plateau, which can be regarded as of the medium erosion standard. These results derived from Cs for the first time have significant implications for the further research of wind erosion and desertification control in the Qinghai-Tibetan Plateau.