472 resultados para CAST MG-ZN


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检测10种外眼病141例、178眼泪液中的Ca、Mg、Zn、Fe含量。结果显示,翼状胬肉和泡性角结膜炎泪液中的Ca,复发单疱病毒性角膜炎(HSK)泪液中的Ca、Mg、Zn、Fe,慢性结膜炎泪液中的Ca、Fe含量均明显低于对照组(P<0.001~0.05)。提示这4种外眼病的病因可能与泪液Ca、Mg、Zn、Fe含量不足有关。

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The BaMA(10)O(17) (M = Be, Mg, Ca, Zn, Cd, Mn, Co, Li) system has been synthesized by solid state method and characterized by XRD. The results show that when M is Mg, Zn, Mn, Co, Li, there exists the structure of beta-Al2O3 for BaMAl10O17 system, and when M indicates Cd, beta-Al2O3 structure is formed accompanying alpha-Al2O3 phase, and when M represents Be and Ca, beta-Al2O3 structure cannot be formed. This demonstrates that the condition forming beta-Al2O3 structure compounds for the system BaMAl10O17 is 0.05nm < R-M < 0.09nm (R-M represents the radius of M). The thought that if a M ion can form a stable spinel structure there exsits a corresponding magnetoplumbite and beta-alumina structure is proposed for BaMAl10O17 system according to the experimental results. When M is Li, Be, Zn, Eu2+ activator produces an emission of nearly 450 nm with half height width about 50 nm, when M is Mn, there are simultaneously the emissions of Eu2+ and Mn2+ and the excitation energy of Eu2+ can transfer to Mn2+ in the host, when M is Cd, Eu2+ displays a double-emission band, which can be explained by the Jahn-Teller's effect. It is possible for the system BaMAl10O17 with M being Li, Be, Zn to become blue-emitting component in three colour lamp through further study.

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Mg-5Al-0.3Mn-xCe (x = 0-3, wt.%) alloys were prepared by metal mould casting method. The microstructures and mechanical properties were investigated. The results revealed that the main phases of as-cast Mg-5Al-0.3Mn alloy consist of alpha-Mg matrix and beta-Mg17Al12 phase. With the addition of Ce element, Al11Ce3 precipitates were formed and mainly aggregated along the grain boundaries. The amount of the Al11Ce3 precipitates increased with increasing addition of Ce, but the amount of beta-Mg17Al12 phase decreased. The highest tensile strength was obtained in Mg-5Al-0.3Mn-1.5Ce alloy. The ultimate tensile strength (UTS), yield strength (YS) and elongation at room temperature are 203 MPa, 88 MPa and 20%, separately.

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In the present work, the edge-to-edge matching model has been introduced to predict the orientation relationships (OR) between the MgZn2 phase which has hexagonal close packed (HCP) structure and the HCP a-Mg matrix. Based on the crystal structures and lattice parameters only, the model has predicted the two most preferred ORs and they are: (1) [1 1 2 3](alpha-Mg) vertical bar vertical bar]1 1 2 3](alpha-Mg), (0 0 0 1)(alpha-Mg) 0.27 degrees from (0 0 0 1)(MgZn2), (1 0 1 1)(alpha-Mg) 26.18 degrees from (1 1 2 2)(MgZn2), (2) [1 0 1 0](alpha-Mg),vertical bar vertical bar[1 1 2 0](MgZn2), (0 0 0 1)(alpha-Mg) vertical bar vertical bar(0 0 0 1)(MgZn2), (1 0 1 1)(alpha-Mg) 3.28 degrees from ( 1 1 2 2)(MgZn2). Four experimental ORs have been reported in the alpha-Mg/MgZn2 system, and the most frequently reported one is ideally the OR (2). The other three experimental ORs are near versions of the OR (2). The habit plane of the OR (2) has been predicted and it agrees well with the experimental results.

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Microstructure and mechanical properties of as-cast and heat-treated Mg–12.3Zn–5.8Y–1.4Al (ZYA1261) alloy were investigated. The phase compositions of the as-cast alloy are -Mg, Mg3YZn6 (I-phase), Mg3Y2Zn3 (W-phase), Mg12YZn (Z-phase), Mg24Y5, MgZn and a small quantity of Al-containing phase. The phase compositions change with various heat treatment conditions. The highest Vickers hardness is obtained in the alloy aged at 200 ◦C for 5 h, the transmission electron microscopy indicated that fine scale Z-phase precipitates in the matrix. The tensile properties of the as-cast and heat-treated alloys were reported.

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l、有机质和全N在草甸土壤的不同层次之间呈现明显的差异,表现力随着土壤深度的增加,含量逐渐降低。无机N包括NH4+-N和No3--N在土层之闻的差异并没有象全N和有机质那么显著。NH4+-在表面30Cm的土壤中明显高于NO3--N的。全P在各层土壤中的含量差异并不显著,但有效p在三层土壤中表现出明显的差异,表现为随土壤深度的增加而降低。 K、Na、Ca、Mg、Fe和AI等6种金属元素的可交换成分在革甸土壤中的含量除K表现出明显的土层间的差异外,在表层30cm的土壤中并没有明显的随土壤深度变化的趋势。 有机质和全N在东灵山地区主要森林土壤中的含量以0~lOcm土层中的显著高于10~20cm的土层中的。20cm的土层中无机N中也以NH4+-为主,这与草甸土壤中的一致。全p和有效P在两个土层之间的差异并不十分显著,而以0^lOcm土层略高于10~20Cm土层的。 K、Na、Ca、Mg、Fe和AI等6种金属元素的可交换成分在不同土层间的差异以K和Ca较为明显,K和Ca在O—1Ocm的土层中要高于lO-20cm的。 森林土壤中的有机质、全N(包括NH4+-N)、全p(包括有效P)都表现为低于亚高山草甸土壤中的,主要原因是亚高山革甸分布于海拔1800cm至2300m,而主要森林类型则基本分布在海拔120m至1500m,亚高山草甸较为恶劣的气候条件明显不利于有机质的矿化,因而分解速率较低,积聚了较多的有机质.而森林土壤中较低的NH4+-N和有效P则可能是由于森林中旺盛的生命活动,尤其是微生物的活动,而大量被植物和微生物固持,因而,即使在森林土壤中有较高的矿化速率,但仍具有较低的NH4+-N和有效p的含量. 不同类型的森林土壤之间各化学成分并没有发现有明显的变化趋势,即使森林类型差异较大的落叶阔叶林和针叶林之间也并没有发现十分显著的差异,这说明各森林类型土壤之间养分特征的一致性。两种针叶林均为人工林,林龄不超过30,而在这之前推测也是以落叶阔叶林为主,森林土壤在这30年间并没有发生十分明显的变化。 在l100m至I500m之间的各种森林类型的土壤也没有表现出十分明显的与海拔高度的相关性。同一森林土壤在不同时间的采样之间,各化学成分也没有表现出明显的差异。 2、降水引起的树干茎流水分中全N的含量在降水季节的初期的含量略高于大量降水期间的。而在降水季节后期,随着每次降雨量的减少,降水间隔时间的增加,树干茎流中N的含量明显地有很大幅度的升高。NO3-N在树干茎流中的含量也同样受到了降水量的影响,表现在后期也发生显著的升高,但升高的幅度没有全N的大。受到降水量影响的元素还有S。 全p在树干茎流水分中含量随降水时间的变化,在各个树种之间有很大的差异。 其它几种元素的可交换态在茎流水分中的含量以K的含量为最高;其次是S、ca、Mg,AI在所有分析的元素中含量最低。不过,AI在降水初期(6月22日)的取样中,含量在几个树种的茎流水分样品中普遍较高,Ca和Mg也被发现有类似的情形。 穿透雨中全N的含量在降水初期略高于降水中期的,而至降水末期时又略有升高,这种格局与树干茎流水分中的具有一致性。全P、K、Ca、Mg、S.AI等包括全N及其无视成分与树干茎流中的含量的差异并不显著. 地表径流中的全N含量在去除枯枝落叶层的径流场的变化格局与树干茎流和穿透雨中的较为一致.表明这三者之间存在一定的相关性.但与未去除枯枝落叶层的径流场的径流水分中全N和NO3-N的含量并不十分一致,全N和NO3-N的含量有时较高. 取自马牙石沟流水堰口的集水区水样中全N和NO3-N的含量均变化在l~3mg/L之间;而取自南沟流水堰口的集水区水样中的全N和N03-N的含量均在l~2mg/L之间,但在这两者之间并没有十分显著的差异,说明取自两个集水区溪流水分中的全N和N03-N的含量基本一致。 3、通过对三个森林立地乔木层生物量的两次调查(相隔6年),发现尽管以辽东栎为主要优势树种的暖温带落叶阔叶混交林(91- 03)第一次调查的生物量低于辽东栋林(91 - 02)和桦木林(91 - 04)的,但在生长6年后,该立地的乔木层生物量已明显超过桦木林的,其增长速率在三个样地中为最高。 根据两次调查的结果,三个样地中出现的11种乔木树种胸径的增加可以分成两组,第一组包括北京花楸、糠椴、白桦和辽东栎,另一组则由山杨、五角枫、棘皮桦、大叶白蜡、蒙椴、黄花柳和沙涞组成。6年中,第一组树种的胸径增加量在1.O~l.4em之间,而第二组的增量在0.2~O.9cm之间,两者之间具有显著的差异。 常用的生物量预测模型包括两个因子,即胸径(D)和树高(H)。D通常可以实测得到,但H大部分只能估计得到。本研究通过比较6年前后两次树高的实际估测结果,证明用D和H共同建立的模型预测结果可能会产生较大的人为误差,建议改用D的单因子预测模型。 无论是实测结果还是树木年轮分析结果,都表明处于目前径级水平的暖温带地区分布的这几个树种还处在不断生长的过程中,随着年龄的增加,表现为胸径还有很大程度的增加,因为这些树种目前的大径级个体的年平均增加速率大于小径级的. 树木年龄与胸径的相互关系的分析结果表明,树木年龄和胸径可以很好地用饱和模型Y=a-be-cx来拟合. 4、通过近5年对辽东栎枝条( D<0.5cm)和叶片凋落物分解的观察和分析,发现辽东栎枝条的总失重率达到了43%,分解速率常数k为2.713x10-3/周,而叶的总失重率则可以达到70%,分解速率常数k为6.234xl0-3/周. 枝条分解过程中的有机质含量变化可以分为三种类型,一种是单调上升型的,如蛋白质,其含量从3.5%增加到约6%;-种是单调下降型的,如半纤维素,约从15%降低至7%;另一种则是相对变化不大,如粗纤维(包括纤维素和木质素),粗纤维的含量变化在58%±3%,木质素变化在56%±2.5%,纤维素则变化在1%~3%之间。 用Olson指数方程拟合,结果表明粗纤维、木质素和半纤维素三者的分解以半纤维素为最快,分解速率常数为5.693xl0-3/周,其次是木质素和粗纤维,分别为2.461x10-3/周和2.352xl0-3/周.而蛋白质和纤维素的拟合结果较差或根本无法拟合. 用Olson指数方程拟合的结果表明,有些元素在凋落物分解过程中可以很好地用该方程拟合,如K,Na、Mn和C,p和N,Mg,Zn,而一些元素如Ca和Cu没有取得很好的拟合效果。 几种元素在叶片凋落物分解过程过程的丢失速率也以K为最快,其它元素的顺序为,e,N,p,Na,Mn,Mg和Ca(Ca的拟合效果较差),而Cu、Zn也不能很好地用Olson指数方程拟合。 5、根据对东灵山地区6年(199l~1997)的气象观测结果,可得到该地区的年平均降水量和总降水量,用1994年分析的降水中养分含量的数据可以近似计算得东灵山地区每年通过降水进入该暖温带落叶阔叶林生态系统的几种养分输入量。同理可以计算降水输入养分在树干茎流和穿透雨中的分配,还可以计算养分从地表径流中的输出。通过对这几个水分循环的主要环节中养分输入或输出量的计算,发现每年通过降水而进入系统的养分,大部分将积累在系统中,而输出份额只占很小的一部分。 K和Mg两种养分元素在降水通过林冠和树干表面时,将产生大量的淋溶,而Ca的淋溶较小.N、P和AI则产生少量的吸附或吸收。对于S来说,淋溶和吸收或吸附作用相当,或两者都很小。 通过生物量的年平均增量和生物量中的养分含量可以计算得到每年积累在生物量中的养分量即存留量,同理可以计算年凋落物中的养分量、归还量及生物系统从土壤中吸收的养分量,每年养分的存留率.通过以上计算,发现该落叶阔叶林对养分的存留率较低,这可能是由于该落叶阔叶林森林生态系统每年具有较高的养分归还量,对于一些元素来说,还具有较高的淋溶量,尤其是K和Mg.

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研究了稀有的鮈鲫鱼肌、性腺的生化组成,肌肉中水分含量为79.12-79.65%,蛋白质为68.39-70.20%,脂肪为20.11-20.65%,灰分为15.88-16.04%,能值为19.91-20.84Kj/gdm。鱼肌中含17种氨基酸,必需氨基酸占19.45-20.13%,极性氨基酸占17.23-17.45%,非极性氨基酸占17.51-18.16%,鱼肌中Ca、Na、P、Mg、Zn、Fe含量均较高,此外还测定了稀有的鮈鲫的活饵-水蚯蚓及人工饲料的生化组成。

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The hole effective-mass Hamiltonian for the semiconductors of wurtzite structure is established, and the effective-mass parameters of GaN and AlxGa1-xN are given. Besides the asymmetry in the z and x, y directions, the linear term of the momentum operator in the Hamiltonian is essential in determining the valence band structure, which is different from that of the zinc-blende structure. The binding energies of acceptor states are calculated by solving strictly the effective-mass equations. The binding energies of donor and acceptor for wurtzite GaN are 20 and 131, 97 meV, respectively, which are inconsistent with the recent experimental results. It is proposed that there are two kinds of acceptors in wurtzite GaN. One kind is the general acceptor such as C, substituting N, which satisfies the effective-mass theory, and the other includes Mg, Zn, Cd etc., the binding energy of which deviates from that given by the effective-mass theory. Experimentally, wurtzite GaN was grown by the MBE method, and the PL spectra were measured. Three main peaks are assigned to the DA transitions from the two kinds of acceptor. Some of the transitions were identified as coming from the cubic phase of GaN, which appears randomly within the predominantly hexagonal material. The binding energy of acceptor in ALN is about 239, 158 meV, that in AlxGa1-xN alloys (x approximate to 0.2) is 147, 111 meV, close to that in GaN. (C) 2000 Published by Elsevier Science S.A. All rights reserved.

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The energy bands of zinc-blende and wurtzite GaN are calculated with the empirical pseudopotential method, and the pseudopotential parameters for Ga and N atoms are-given. The calculated energy bands are in agreement with those obtained by the ab initio method. The effective-mass theory for the semiconductors of wurtzite structure is established, and the effective-mass parameters of GaN for both structures are given The binding energies of acceptor states are calculated by solving strictly the effective-mass equations. The binding energies of donor and acceptor are 24 and 142 meV for the zinc-blende structure, 20 and 131, and 97 meV for the wurtzite structure, respectively, which are consistent with recent experimental results. It is proposed that there are two kinds of acceptor in wurtzite GaN. One kind is the general acceptor such as C, which substitutes N, which satisfies the effective-mass theory. The other kind of acceptor includes Mg, Zn, Cd, etc., the binding energy of these accepters is deviated from that given by the effective mass theory. In this report, wurtzite GaN is grown by the molecular-beam epitaxy method, and the photoluminescence spectra were measured. Three main peaks are assigned to the donor-acceptor transitions from two kinds of accepters. Some of the transitions were identified as coming from the cubic phase of GaN, which appears randomly within the predominantly hexagonal material. [S0163-1829(99)15915-0].

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  制备了Mg-4.5wt%Zn-1~5wt%RE系合金(RE元素包括轻稀土:La、Ce、Nd、Sm;重稀土:Gd和Y),研究了铸态和热处理态合金的组织和性能。(1)适量的稀土元素均可细化合金晶粒,其中轻稀土元素的细化效果好于重稀土元素;(2)含轻稀土元素合金中的析出相主要为(Mg,Zn)17RE2和Mg4Zn7,而含重稀土元素的合金中的析出相主要为MgZnxREy(Mg3Zn6RE, Mg3RE2Zn3)和Mg4Zn7;(3)加入稀土元素后,合金的强度提高;稀土含量相同时,含轻稀土元素的强化效果较好。Mg-4.5Zn-1Ce合金具有最高的强度。T5处理态合金的抗拉强度、屈服强度和伸长率分别为236 MPa、111 MPa和15.8%,T6处理态合金分别为233 MPa、131 MPa和8.9%。强度提高的主要原因是合金中生成了大量的纳米级Mg4Zn7强化相,以及晶界沉淀相的连续性降低;(4)含重稀土元素合金的时效硬化效果高于含轻稀土元素的合金,经T6处理后,含重稀土元素合金的断裂强度和屈服强度均提高,而含轻稀土元素合金只有屈服强度提高。   研究了挤压变形Mg-4.5Zn-1Ce合金的组织和性能。473 K时效后峰值态合金具有较高抗拉强度和屈服强度,其值分别为291 MPa和239 MPa,比铸态分别提提高了55 MPa和128 MPa。高强度产生的原因是合金中生成了大量棒状和点状混合结构的纳米级Mg4Zn7强化相和晶粒的细化。   应用Edge-to-edge匹配模型成功预测了MgZn2/α-Mg体系中的位相关系,扩大了该模型的应用范围。并对模型进行了改进,主要体现在:1)确定匹配方向的平面上所有原子的中心位置需在平面上;2)匹配方向之间可任意配对。应用优化后的模型预测了Mg17Al12/α-Mg体系中的位相关系,预测结果与实验结果的吻合率为4/6,好于原模型预测的吻合率4/8。另外,使用优化后的模型,成功的预测出了理想的Burgers位相关系,从而证实了该位相关系是确实存在的,而不是near Burgers位相关系测定的误差。使用优化后的模型还成功的解释了该合金体系中稀土元素的晶粒细化机制和沉淀强化机制。

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采用高温固相反应合成了稀土离子激活的碱土硼磷酸盐MBPO_5:RE(M=Ca, Sr, Ba;RE=Sm, Eu, Tb, Dy), Ba_3BPO_7:RE和Ba_3BP_O_(12):RE、稀土硼磷酸盐Ln_7BP_2P_(17):RE (Ln=La, Gd)、碱土(稀土)磷酸盐M_3(PO_4)_2:RE (M=Sr, Ba),ABLa(PP_4)_2:Ce,Tb (A=K, Na;B=Mg, Zn)、碱土(稀土)硼酸盐SrB_4O_7:RE(Re=Sm, Eu),BaB_8O_(13):Eu,SrB_6O_(10):Sm, M_3Gd_2(BO_3)_4:RE (M=Ca, Sr),B_3O6:Eu(RE=La, Gd)和稀土硼钨酸盐Cd_3BWO_9:Eu。通过XRD、IR光谱和Raman光谱等表征了其结构。测定了上述19个基质的数十个发光体的UV佩VUV光谱和RE-L_3(RE=Sm,Eu, Gd)边的XANES和EXAFS。碱土硼磷酸盐Ba_3BPO_7和Ba_3BP_3O_(12)、稀土硼磷酸盐Ln_7BP_2O_(17) (Ln=La, Gd)和稀土钨硼酸盐Gd3Bwo9等6个基质中稀土离子的UV-VUV光谱和除个别基质(REB_3O_6等)外的VUV光谱均属首次报道。发现土稀土离子激活的这些发光体在VUV范围有丰富的基质吸收带。认为基质中阴离子的结构和基质的晶体结构可能是影响基质的吸收带位置的重要因素。通过XANEs和UV-VUV光谱的联系,结合经验公式首次确证了一些复合氧化物基质中一些RE~(3+)在vuv范围的f-d跃迁位置。根据VUV光谱测定结果推测了一些基质中RE~(3+)的CTB位置。首次应用RE-L_3边的XANES和UV-VUV光谱两种方法分析比较了RE~(3+)(RE=Eu, Sm)离子在空气条件下在碱土硼磷酸盐、硼酸盐和磷酸盐基质中的还原。首次应用高分辨发射光谱和RE-L_3边的EXAFS研究了在一些基质中发光中心的配位数、键长和格位对称性等结构因素。

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PDP(等离子平板显示器)是一种最有前途的大屏幕壁挂式彩电,而它需要VUV激发下的高效荧光粉,同时由于VUV荧光粉也是无汞荧光灯的需求,所以研究VUV激发的稀土激活的荧光粉是实际应用的需要.对于光谱分析该工作采用了理论计算与光谱数据分析相结合的方法,对所测光谱各个谱峰进行了详细的指认.得到了以下的结论和成果:1.得到了大量的含氧酸盐中稀土离子的VUV光谱数据.2.首次系统地应用两种方法预测了三价稀土离子的f-d跃迁位置,并首次系统地通过计算预测了三价稀土离子在含氧酸盐中的电荷迁移带的位置.3.首次实验观察到Ce<'3+>的电荷迁移带,观察到了Tb<'3+>的电荷迁移带.4.在所有含Dy<'3+>的样品中都观察到Dy<'3+>的f-d跃迁.5.LaPO<,4>和ABLa(PO<,4>)<,2>(A=K,Na;B=Mg,Zn)基质中,观察到了Ce<'3+>的5个f-d跃迁,指认了Tb<'3+>的5个f-d跃迁,指认了掺杂Ce、Tb的VUV光谱中的所有谱峰.6.对所研究基质中的稀土离子的f-d跃迁和电荷迁移带进行了系统地预测和指认.7.通过总结不同稀土离子在相同基质中的VUV光谱,并参考文献的相关报导,总结了所研究基质的基质吸收位置.8.通过Eu<'3+>的灾光探针作用和ce<'3+>的发射光谱等,确证三价稀土离子在La<,2>CaB<,10>O<,19>基质中同时取代了八配位的Ca<'2+>和十配位的La<'3+>,占据了两种格位.9.合成了一种新型绿色长余辉材料,具有亮度高,余辉时间长,可用日光激发等优点.10.合成了一种UV激发下性能优异的掺Eu<'3+>的红色荧光粉,亮度可以跟商业红粉Y<,2>O<,3>:Eu相比拟,而基质材料与Y<,2>O<,3>相比降低了成本.

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Cd in GaAs is an acceptor atom and has the largest atomic diameter among the four commonly-used group-II shallow acceptor impurities (Be, Mg, Zn and Cd). The activation energy of Cd (34.7 meV) is also the largest one in the above four impurities, When Cd is doped by ion implantation, the effects of lattice distortion are expected to be apparently different from those samples ion-implanted by acceptor impurities with smaller atomic diameter. In order to compensate the lattice expansion and simultaneously to adjust the crystal stoichiometry, dual incorporation of Cd and nitrogen (N) was carried out into GaAs, Ion implantation of Cd was made at room temperature, using three energies (400 keV, 210 keV, 110 keV) to establish a flat distribution, The spatial profile of N atoms was adjusted so as to match that of Cd ones, The concentration of Cd and N atoms, [Cd] and [N] varied between 1 x 10(16) cm(-3) and 1 x 10(20) cm(-3). Two type of samples, i.e., solely Cd+ ion-implanted and dually (Cd+ + N+) ion-implanted with [Cd] = [N] were prepared, For characterization, Hall effects and photoluminescence (PL) measurements were performed at room temperature and 2 K, respectively. Hall effects measurements revealed that for dually ion-implanted samples, the highest activation efficiency was similar to 40% for [Cd] (= [N])= 1 x 10(18) cm(-3). PL measurements indicated that [g-g] and [g-g](i) (i = 2, 3, alpha, beta,...), the emissions due to the multiple energy levels of acceptor-acceptor pairs are significantly suppressed by the incorporation of N atoms, For [Cd] = [N] greater than or equal to 1 x 10(19) cm(-3), a moderately deep emission denoted by (Cd, N) is formed at around 1.45-1.41 eV. PL measurements using a Ge detector indicated that (Cd, N) is increasingly red-shifted in energy and its intensity is enhanced with increasing [Cd] = [N], (Cd, N) becomes a dominant emission for [Cd] = [N] = 1 x 10(20) cm(-3). The steep reduction of net hole carrier concentration observed for [Cd]/[N] less than or equal to 1 was ascribed to the formation of (Cd, N) which is presumed to be a novel radiative complex center between acceptor and isoelectronic atoms in GaAs.

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The hole effective-mass Hamiltonian for the semiconductors of wurtzite structure is established, and the effective-mass parameters of GaN and AlxGa1-xN are given. Besides the asymmetry in the z and x, y directions, the linear term of the momentum operator in the Hamiltonian is essential in determining the valence band structure, which is different from that of the zinc-blende structure. The binding energies of acceptor states are calculated by solving strictly the effective-mass equations. The binding energies of donor and acceptor for wurtzite GaN are 20 and 131, 97 meV, respectively, which are inconsistent with the recent experimental results. It is proposed that there are two kinds of acceptors in wurtzite GaN. One kind is the general acceptor such as C, substituting N, which satisfies the effective-mass theory, and the other includes Mg, Zn, Cd etc., the binding energy of which deviates from that given by the effective-mass theory. Experimentally, wurtzite GaN was grown by the MBE method, and the PL spectra were measured. Three main peaks are assigned to the DA transitions from the two kinds of acceptor. Some of the transitions were identified as coming from the cubic phase of GaN, which appears randomly within the predominantly hexagonal material. The binding energy of acceptor in ALN is about 239, 158 meV, that in AlxGa1-xN alloys (x approximate to 0.2) is 147, 111 meV, close to that in GaN. (C) 2000 Published by Elsevier Science S.A. All rights reserved.

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揭示苔藓植株元素含量及其时空差异性是深入开展利用苔藓植物指示环境和筛选理想监测藓种的科学基础。采用微波消解(ICP-AES)方法对九寨沟自然遗产地原始林景点停车场周围三个采样带:I为停车场植被小岛(PS),向外约120 m半径为II带(D120),再向外距离约1,000 m为III带(D1000)和3个方向上的大羽藓和毛尖青藓2种苔藓中13种元素(A1, S, Ca, P, Cu, Fe, K, Mg, Mn, Pb, Ni,Zn和Cd)含量进行了测定和比较,并对采自边坡方向(PS-3)上2005和2007年的4种苔藓植物(南木藓、大羽藓、平藓和厚角絹藓)也进行了13种元素含量的测定和比较。同时对九寨沟自然遗产地、黄龙自然遗产地、夹金山和梦笔山的冷杉原始林4个地区的3种苔藓中(大羽藓、锦丝藓和塔藓)的A1、Ca、Cu、Fe、K、Mg、P、Zn、C和N 10种元素含量进行测定和比较。 对大羽藓和毛尖青藓2种苔藓植物内13种元素的测定发现:1)同种苔藓对不同元素的富集能力不同。A1、Ca、K、Mg和P的元素含量在苔藓中的富集较其他元素的要高。2)不同种苔藓植物对同种元素的富集能力不同,毛尖青藓较大羽藓能够监测出更多的元素;对于被检测出的元素,毛尖青藓监测出的累积量大于大羽藓,其中累积量最大的元素是Ca为10 874.286 μg.g-1.year-1,最小的是Cu元素为5.438 μg.g-1.year-1。对05年和07年的平藓、大羽藓、南木藓和厚角絹藓元素含量的测定表明:元素在两年中的积累量是不同的。综合分析表明,苔藓生物监测方法可有效监测景点停车场机动车尾气中排放出的典型元素(如Cu、Pb、Ni、Zn、Cd等)含量,而毛尖青藓较大羽藓能更可靠的监测九寨沟自然遗产地单景点汽车尾气金属元素种类及其排放量。 对4个地区3种苔藓10种元素监测发现:1)Ca、Mg、Zn、K和Cu元素在黄龙地区的含量高于在其它地区的含量;P元素在梦笔山地区的含量为最高;Fe和Al元素在夹金山地区的含量高于在其它地区的含量。2)C元素在其它因素一致的情况下,进行不同年龄间的元素含量比较,结果显示元素含量在各年龄间并不存在明显的差异性;N元素含量与年龄的差异出现在黄龙林下及林窗的塔藓、九寨沟林下的锦丝藓及塔藓和梦笔山的塔藓中,而在锦丝藓中未出现元素含量与年龄的差异性;塔藓能检测出更多的元素种类其含量与年龄间存在显著差异,锦丝藓检测到的元素种类次之;除锦丝藓(锦丝藓在林窗中几乎检测不到元素含量与年龄间的差异性)外,其他两种藓在林窗中能检测出的元素种类大于在林下的检测种类。3)元素含量与生境间存在差异性的元素分别有:黄龙大羽藓中的Ca、P和Mg元素;九寨锦丝藓中的Zn元素;夹金山塔藓中的Al、Fe和Zn元素;梦笔山大羽藓中的Al、Fe和Mg元素及锦丝藓中的Ca元素。4)区域、年龄和生境因素对苔藓植株元素含量均达到了显著水平,但两两之间及三者之间的交互作用由于元素种类的不同存在差异。综合分析表明,苔藓植物中的元素含量受年龄、区域的影响较生境的更大。 The revelation of mosses elements content and its spatiotemporal differences is the scientific foundation of moss monitoring. To determine the feasibility of moss monitoring metal depositions derived from travel bus emiss ions in scenic spot, we collected one year-growth samples of two mosses Brachythecim piligerum and Thuidium cymbifolium with different distance (island center, 120m,1000m ) and different direction (north, south and east) far from parking site island from Yuanshilin Spot at Jiuzhaigou World Nature Heritage in the Western Sichuan of China and determined thirteen element (A1, S, Ca, P, Cu, Fe, K, Mg, Mn, Pb, Ni, Zn, Cd)contents by ICP-AES analysis method. And picked 4 kinds of mosses (Macrothamnium macrocarpu m(Reinw. etHornsch.)Fleisch.,Thuidium cymbifolium,Entodon concinnus (De Not.) Par., Neckera pennata) from the direction PS-3 in 2005 and 2007, determined 13 element contents. Collected 3 kinds of moss (Thuidium cymbifo lium, Actinothuidium Hookeri (Mitt.) and Hyolcomium splendens (Hedw.) from Jiuzhaigou natural heritage, Huanglong natural heritage, Mt. Jiajin and Mt. Mengbi in primeval forest with two habitat (undergrowth and forest gap), determined element contents of A1, Ca, Cu, Fe, K, Mg, P, Zn, C and N. We found that, 1) The elements content are difference in same type of moss. Content of A1, Ca, K, Mg and P are higher than others. 2) While the contents of A1, S, Ca, P, Cu, Fe, K and Zn had significant correlation with the different distances from parking site, the nearer the distance was, the more accumulation was; 2) Comparing to Thuidium cymbifolium, Brachythecium piligerum can test more elements which contents show the significant correlation with distances. And Brachythecium piligerum can have greater element accumulation than Thuidium cymbifolium. The element contents in two years (2005 and 2007) are different. The present study found that moss can reliably bio-indicate metal deposition from traffic emissions in one scenic spot and Brachythecium piligerum is a good moss for bio-indicating element content from traffic emissions at Jiuzhaigou World natural Heritage. Determined the 10 element contents in 4 areas through 3 kinds of moss we found that, 1) Ca, Mg, Zn, K and Cu element content is higher in the Huanglong area than in other areas, The P element content in Mt. Jiajin is higher than other areas, Fe and Al element content is higher in the Mt. Jiajin than in other areas. 2) The content of C had no significant correlation with age. As for N, this significant correlation found in Hyolcomium splendens (Hedw.) with 2 habitat in Huanglong, Actinothuidium Hookeri (Mitt.) and Hyolcomium splendens (Hedw.) with undergrowth in Jiuzhai, Hyolcomium splendens (Hedw.) in Mt. Mengbi. The types of elements which content showt he significant correlation are most in Hyolcomium splendens (Hedw.) and least in Thuidium cymbifolium. Except Actinothuidium Hookeri (Mitt.), the types of elements that content had significant correlation with age in forest gap are more than in undergrowth. 3) The elements which content had significant correlation with habitat are P, Ca and Mg in Thuidium cymbifolium in Huanglong, Zn in Actinothuidium Hookeri (Mitt.) in Jiuzhai, Al, Fe and Zn in Hyolcomium splendens (Hedw.) in Mt. Jiajin, in Mt. Mengbi Al, Fe and Mg in Thuidium cymbifolium and Ca in Actinothuidium Hookeri (Mitt.). 4)The region, the age and the habitat factor has coeffect element content. The correlationship between element contents and the age, the region is closer than habitat.