Studies on organolanthanide complexes .58. Syntheses of 1,1'-(3-oxa-pentamethylene)dicyclopentadienyl divalent organolanthanides (Ln=Sm, Yb) and X-ray molecular structure of O(CH2CH2C5H4)(2)Yb(DME)

The compounds O(CH2CH2C5H4)(2)Ln(THF)(2) [Ln = Sm(1), Yb(2)] were synthesized by the reduction of O(CH2CH2C5H4)(2)LnCl with sodium metal in tetrahydrofuran (THF) at room temperature. Recrystallization of 2 from dimethoxyethane (DME) produced the single-crystal O(CH2CH2C5H4)(2)Yb(DME) (3) whose structure has been determined by an X-ray diffraction study. The crystals are orthorhombic, space group Pcab, with a = 14.168(4), b = 13.541(6), c = 19.314(8) Angstrom, Z = 8, D-calc. = 1.66 g cm(-3).

CRYSTAL-STRUCTURE OF [YB (NO3)3 (PHEN) (H2O)]CENTER-DOT(12-CROWN-4)

The title complex was prepared by reacting Yb(NO3)3 (12-crown-4) with 1, 10-phenanthiroline (hereafter phen) in acetone. It crystallized in the triclinic space group P1BAR with a = 10.095(5), b = 17.415(4), c = 8.710(2) angstrom; alpha = 92.45(2), beta = 115.83(3), gamma = 74.08(3)degrees and D(c), = 1.85 g cm-3; Z = 2. The metal ion in this complex is nine-coordinated to three bidentate nitrate ions, two nitrogen atoms of a phen and a water molecule. The crown ligand is hydrogen bonded to the coordination water molecule. The symmetry change of the crown ether is also discussed.

STUDIES ON OLEFIN-COORDINATING TRANSITION-METAL CARBENE COMPLEXES .20. SYNTHESIS OF 1,3-CYCLOHEXADIENE(DICARBONYL) [ETHOXY(ARYL)-CARBENE]IRON COMPLEXES AND THEIR PHOSPHINE ADDUCTS - CRYSTAL-STRUCTURE OF C6H8(CO)2FEC(OC2H5)C6H4CH3-O

Reaction of 1,3-cyclohexadiene(tricarbonyl)iron (1) with ortho-substituted aryllithium reagents ArLi (Ar=o-CH3C6H4, o-CH3OC6H4, o-CF3C6H4) in ether at low temperature, and subsequent alkylation of the acylmetalates formed with Et3OBF4 in aqueous solution at 0-degrees-C or in CH2Cl2 at -60-degrees-C gave the 1,3-cyclohexadiene(dicarbonyl)[ethoxy(aryl)carbene]iron complexes (eta4-C6H8)(CO)2FeC(OC2H5)Ar (3, Ar = o-CH3C6H4; 4, Ar = o-CH3OC6H4), and the isomerized product (eta3-C6H8)(CO)2FeC(OC2H5)C6H4CF3-o (5), respectively, among which the structure of 3 has been established by an X-ray diffraction study. Complex 3 is monoclinic, space group P2(1) with a = 8.118(4), b = 7.367(4), c = 14.002(6) angstrom, beta = 104.09(3)-degrees, V = 812.2(6) angstrom3, Z = 2, D(c) = 1.39 g cm-3, R = 0.056, and R(w) = 0.062 for 976 observed reflections. Complexes 3 and 5 were converted into the chelated allyliron phosphine adducts(eta3-C6H8)(CO)2(PR31)FeC(OC2H5)Ar (6, Ar = o-CH3C6H4, R1 = Ph; 7, Ar = o-CH3C6H4, R1 = OPh; 9, Ar = o-CF3C6H4, R1 = Ph), by reaction with phosphines in petroleum ether at low temperatures.

YV_(1-x)B_xO_(4-x):Eu~(3+)(或Dy~(3+),Bi~(3+))的合成及光谱性质的研究

本文报道了Eu~(3+)、D~(3+)在YV_(1-x)B_xO_(4-x)中的光谱性质。实验表明:B~(3+)取代V~(5+)时,可使基质和Dy~(3+)的发射强度及黄兰比下降,并使基质的吸收带短移。而B~(3+)取代Y~(3+)时,则可提高Dy~(3+)的黄兰比。同时我们还研究了Bi~(3+)和温度对YV_(0.69)B_(0.31)O_(3.69):Dy~(3+)中Dy~(3+)发射强度的影响。

STRUCTURE OF 1,10-DIAMINODECANE TETRACHLOROZINCATE

[NH3(CH2)10NH3][ZnCl4], M(r) = 381.51, triclinic, P1BAR, a = 7.296 (1), b = 10.110 (3), c = 12.814 (4) angstrom, alpha = 90.84 (2), beta = 101.17 (2), gamma = 92.52 (2)-degrees, V = 926.13 angstrom 3, Z = 2, D(x) = 1.37 Mg m-3, lambda(Mo K-alpha) = 0.71073 angstrom, mu = 1.925 mm-1, F(000) = 396, T = 298 K, final R = 0.070 for 1237 unique reflections [I > 3-sigma(I)]. The structure is characterized by layers of inorganic ions sandwiched between layers formed by the paraffinic chains.

STRUCTURE OF CIS-DIAQUABIS(1,10-PHENANTHROLINE)ZINC SULFATE HEXAHYDRATE

[Zn(C12H8N2)2(H2O)2]SO4.6H2O, M(r) = 665.98, triclinic, P1BAR, a = 10.070 (4), b = 12.280 (3), c = 13.358 (2) angstrom, alpha = 109.12 (2), beta = 92.58 (2), gamma = 110.85 (2)-degrees, V = 1433.9 (7) angstrom 3, Z = 2, D(x) = 1.54 g cm-3, lambda(Mo K-alpha) = 0.71069 angstrom, mu = 10.1 cm-1, F(000) = 692, T = 293 K, R = 0.044 for 3985 observed reflections. The Zn atom is coordinated in a distorted octahedral geometry by four N atoms from two 1,10-phenanthroline (phen) ligands and two water molecules. The intermolecular ring-stacking interactions between the phen ligands occur in two forms: infinite chains and discrete dimers. Hydrogen bonds further stabilize the structure.

SYNTHESIS AND X-RAY CRYSTAL-STRUCTURE OF A MONOPENTAMETHYLCYCLOPENTADIENYL DERIVATIVE OF GADOLINIUM (NA(MU-2-THF)[(C5ME5)GD(THF)]2(MU-2-CL)3(MU-3-CL)2)2.6THF

The reaction of GdCl3 with 1 equiv of NaC5Me5 generates a neutral complex C5Me5GdCl2(THF)3 and a novel complex {Na(mu-2-THF)[(C5Me5)Gd(THF)]2(mu-2-Cl)3(mu-3-Cl)2}2.6THF whixh recrystallizes from THF in triclinic, the space group P1BAR with unit cell dimentions of a 12.183(4), b 13.638(6), c 17.883(7) angstrom, alpha-110.38(3), beta-94.04(3), gamma-99.44(3)-degrees, V 2721.20 angstrom-3 and D(calc) 1.43 g cm-3 for Z = 1. Least-squares refinement of 2170 observed reflections led to a final R value of 0.047. The title complex consists of two Na(mu-2-THF)[(C5Me5)Gd(THF)]2(mu-3-Cl)3(mu-3-Cl)2 units bridged together via two mu-2-THF to Na coordination. Each Gd ion is surrounded by one C5Me5 ligand, two mu-3-Cl, two mu-2-Cl and one THF in a distorted octahedral arrangement with average Gd-C(ring) 2.686(33), Gd-mu-2-Cl 2.724(7), Gd-mu-3-Cl 2.832(8) and Gd-O 2.407(11) angstrom. The sodium ion coordinates to two bridging THF, two mu-2-Cl and two mu-3-Cl to form a distorted octahedron with average Na-mu-2-O, Na-mu-2-Cl and Na-mu-3-Cl of 2.411(21), 2.807(15) and 2.845(12) angstrom, respectively.

An acidic polysaccharide with xylose branches from Porphyra yezoensis

An acidic polysaccharide (PY3) was isolated from the hot water extract of the red algae Porphyra yezoensis by successive column chromatographies over DEAE-cellulose and Sephadex G-200. PY3 with an average molecular weight of 1.8x10(5) was demonstrated to be composed of galactose (Gal), 3,6-anhydrogalactose (3,6-AnGal), 6-OSO3-galactose (6-OSO3-Gal) and xylose (Xyl) in an approximate molar ratio of 25 : 15, 10, 1. In view of Smith degradation and methylation and on the basis of spectral evidence including those of IR, GC, GC-MS, and H-1 and C-13 NMR, the most probable repeating unit of PY3 could be proposed as [(1-->3)beta -D-Gal(1 --> 4)alpha -L-3,6-AnGal](3)-[(1 --> 3)beta -D-Gal(1 --> 4)alpha -L-6-OSO3-Gal](2) with a xylose moiety at the C-6 of one of every twenty-five beta -D-Gal residues. To our knowledge, PY3 was shown to be the first porphyran possessing occasional xylose branches.

海洋聚磷菌Halomonas YSR-3的除磷特性研究

本论文报道从海洋中分离到的一株聚磷菌的分离、鉴定、在系统发育中的地位、除磷特性、菌体内多磷酸盐颗粒的研究、D-海因酶和核苷二磷酸激酶基因的克隆及序列分析，为海水系统的生物除磷提供部分基础资料。 从黄海海域分离到聚磷菌Halomonas sp. YSR-3，菌体呈杆状，大小为3.5 μm×1 μm，革兰氏阴性，好氧生长，能运动。透射电镜观察发现，菌体内有致密颗粒。经DAPI染色确定该致密颗粒是多磷酸盐，亦可称为异染粒、迂回体。16S rDNA鉴定结果表明，YSR-3与Halomonas属中的marine bacterium B5-7有较高的同源性，相似值99%。YSR-3的生理生化特性：对氯霉素和卡那霉素敏感；淀粉水解呈阳性；反硝化和几丁质降解呈阴性；能将葡萄糖作为唯一碳源和能源。 对YSR-3的培养条件进行优化。以海水2216培养基、24 ℃、180 rpm、pH 6.5的条件培养，更利于菌体生长和菌体内多磷酸盐的形成。 对YSR-3的除磷特性进行研究。无磷培养时，菌体不能生长；用磷酸钾盐作为磷源时，菌体生长较好，形成多磷酸盐的菌体比例较高；较适合YSR-3菌体生长和多磷酸盐形成的磷源是KH2PO4，较适磷浓度为1.5 mmol/L。pH的变化影响菌株的生长、多磷酸盐形成和除磷效果。pH值为5时，菌体的数量几乎不增加，体内多磷酸盐和培养基中磷含量变化不大；pH值为6、7和8时，菌体生长良好，95%以上的菌体内形成多磷酸盐，培养基中磷含量明显下降。YSR-3在不同培养基中除磷量和除磷率不同。在高磷培养基中除磷量为0.7 mmol/L(磷含量由1.84 mmol/L降到1.14 mmol/L)，除磷率为37.5%；在低磷培养基中除磷量为0.02 mmol/L(磷含量由0.028 mmol/L降到0.008 mmol/L)，除磷率为72.2%。 以海洋聚磷菌Halomonas sp. YSR-3的总DNA为模板，用PCR法扩增D-海因酶基因和核苷二磷酸激酶基因，将扩增片段克隆到pGM-T载体，转化E.coli TOP10菌株，经蓝白斑筛选、菌落PCR得到阳性克隆，测序后对序列进行Blast比对分析。得到的D-海因酶基因序列长度为1510 bp，与Pseudomonas entomophila L48的海因酶基因序列的相似性为77%。翻译后的序列与Pseudomonas fluorescens Pf-5，Marinomonas sp. MED121，Burkholderia vietnamiensis G4的海因酶蛋白序列相似性分别为75%，73%，70%。得到的核苷二磷酸激酶基因序列长度为420bp，翻译后的序列与Loktanella vestfoldensis SKA53，Jannaschia sp. CCS1，Roseobacter sp. CCS2的核苷二磷酸激酶蛋白序列相似性分别为89%，86%，85%。 聚磷菌能将外界环境中的磷吸收到体内，并以多磷酸盐的形式储存。多磷酸盐对于细胞的生存和生长有很重要的作用，但目前对于多磷酸盐的形成过程以及过程调控还不是很清楚。在今后可以通过构建高效表达的重组菌，提高与除磷相关的酶的纯度及活性。同时可以将相关酶的基因进行突变，对基因表达的调控以及酶的代谢以及功能结构等多方面进行基础研究，使聚磷菌在生物除磷中得到广泛应用。

Structural studies on a novel fucogalactan sulfate extracted from the brown seaweed Laminaria japonica

A low molecular weight fucogalactan, obtained from the brown seaweed Laminaria japonica, was separated into three fractions (LF1, LF2 and LF3) by DEAE-Sepharose FF column chromatography. All three fractions contained predominantly fucose, sulfate group and galactose. The results showed that the main fraction LF2 consisted of L-fucose, D-galactose and sulfate at a molar ratio 6:1:9. Structural study on the LF2 was carried out by NMR spectroscopy. The backbone of LF2 was primarily (1 -> 3)-linked alpha-L-fucopyranose residues (75%) and a few (1 -> 4)-alpha-L-fucopyranose linkages (25%). The branch points were at C-4 of 3-linked alpha-L-fucopyranose residues by beta-D-galactopyranose unites (35%, molar ratio) or at C-2 of 3-linked alpha-L-fucopyranose residues by non-reducing terminal fucose unites (65%, molar ratio). Sulfate groups occupied at position C-4 or C-2, sometimes C-2, 4 to fucose residues, and C-3 and/or C-4 to galactose residues. The structure of LF2 was supposed as following: [GRAPHICS] (C) 2010 Elsevier B.V. All rights reserved.

Separation and determination of flavone and xanthone glycosides in Tibetan folk medicinal species Swertia mussotii and S-franchetiana by capillary electrophoresis

The contents of five pharmacologically active flavone and xanthone glycosides, namely, swertianolin, swertisin, isoorientin, mangiferin, and 7-O-[alpha-L-rhamnopyranosyl-(1 -> 2)-beta-D-xylopyranosyl]-1,8-dihydroxy-3-methoxyxanthone, extracted from Tibetan folk medicinal species Swertia mussotii and S. franchetiana were determined by capillary electrophoresis with diode-array detection. The separation of five components has been optimized with a capillary column with a total length of 48.5 cm and effective length of 40 cm (50 mu m i.d). The influence of the running buffer, the sodium dodecyl sulfonate (SDS) concentration, organic modifier, etc. on the resolution was evaluated. The background electrolyte contained 30 mM borate buffer, 28 mM SDS, 1.0% (v/v) acetonitrile, and was adjusted to pH 9.0 with 0.1 M NaOH. A good baseline resolution was obtained for the separation of five components within 5 min with the working voltage of 24 kV and a column temperature of 25 degrees C. The established method was rapid and reproducible for the separation and determination of five flavone and xanthone glycosides from the extracts of S. mussotii and franchetiana plant samples.

压力和铁含量对铁方镁石(Mg1-xFex)O(x<=0.25)弹性常数影响的第一性原理研究

By first principle methods based on density functional theory (DFT),the equation of state(EOS) and elastic constants of both periclase and ferropericlase are calculated. The pressure and iron doping effects on the elastic constants of ferropericlase are investigated systematically. Firstly, we calculate the elastic constants of periclase and compare the obtained results with experimental data and other theoretical calculations, which shows a encouraging consistence and demonstrates the practicability of first-principle methods. Secondly, by adding iron into periclase crystal model, we build up ferropericlase with iron contents ranging from 0% to 25% mole percent. The corresponding elastic constants are calculated in a large pressure range(0~120GPa). Emphatically, the strong correlation of 3d electrons in transitional elements, such as iron, is difficult to treat in first-principle methods for a long time. The current solution is to make additional correction. During the initial stage of this study, the strong correlation of 3d electrons in iron is not considered, and we observed that addition of iron decreases the volume of ferropericlase, which is totally contradictory to the experimental data. By applying LDA+U approximation in order to solve the strongly correlated 3d electron of iron, we observed the expansion of volume by iron as expected. On the basis of the LDA+U approximation, the elastic constants of ferropericlase are calculated. After a detailed analysis of data obtained from theoretical calculations, we have reached the following conclusions:(1)pressure imposes positive effects on all elastic constants, and the degree of effects is C11>C12>C44. (2) Iron has no distinctive effects on C11 and C12, although some fluctuations are observed around 60GPa. However, iron has obvious softening effects on C44 The softening effects on C44 are intensified as pressure increases. Above the 100GPa, the effects increase greatly, even surpasses the pressure's positive effects in ferropericlase crystal models with iron mole percent of having 12.5%, 18.75% and 25% iron content. (3)As to the modulus deprived from elastic constants, iron has no effect on the adiabatic bulk module BS, only a little fluctuation around 60GPa. We find iron's softening effects on shear modulus G. (4)We find out that, compared with low iron content, elastic constants with iron content approaching 25mole% is consistently fluctuated，which may be caused by the limitations of the LDA+U approximation method itself. (5)We investigate the pressure and Fe doping effects on elastic anisotropy factor（A=(2C44+C12-C11)/C11） of ferropericlase and find out that iron contents will lower the critical isotropic pressure. At the same pressure, when the pressure is below the isotropic pressure, iron softens the anisotropy factor ; when pressure surpasses the isotropic pressure, iron increases the anisotropy factor.

珠江口盆地流花11-1油田储层非均质性及流体分布规律研究

In order to discover the distribution law of the remaining oil, the paper focuses on the quantitative characterization of the reservoir heterogeneity and the distribution law of the fluid barrier and interbed, based on fine geological study of the reservoir in Liuhuall-1 oil field. The refined quantitative reservoir geological model has been established by means of the study of core analysis, logging evaluation on vertical well and parallel well, and seismic interpretation and prediction. Utilizing a comprehensive technology combining dynamic data with static data, the distribution characteristics, formation condition and controlling factors of remaining oil in Liuhuall-1 oil field have been illustrated. The study plays an important role in the enrichment regions of the remaining oil and gives scientific direction for the next development of the remaining oil. Several achievements have been obtained as follows: l.On the basis of the study of reservoir division and correlation,eight lithohorizons (layer A, B_1, B_2, B_3, C, D, E, and F) from the top to the bottom of the reservoir are discriminated. The reef facies is subdivided into reef-core facies, fore-reef facies and backreef facies. These three subfacies are further subdivided into five microfacies: coral algal limestone, coralgal micrite, coral algal clastic limestone, bioclastic limestone and foraminiferal limestone. In order to illustrate the distribution law of remaining oil in high watercut period, the stratigraphic structure model and sedimentary model are reconstructed. 2.1n order to research intra-layer, inter-layer and plane reservoir heterogeneity, a new method to characterize reservoir heterogeneity by using IRH (Index of Reservoir Heterogeneity) is introduced. The result indicates that reservoir heterogeneity is medium in layer B_1 and B_3, hard in layer A, B_2, C, E, poor in layer D. 3.Based on the study of the distribution law of fluid barrier and interbed, the effect of fluid battier and interbed on fluid seepage is revealed. Fluid barrier and interbed is abundant in layer A, which control the distribution of crude oil in reservoir. Fluid barrier and interbed is abundant relatively in layer B_2,C and E, which control the spill movement of the bottom water. Layer B_1, B_3 and D tend to be waterflooded due to fluid barrier and interbed is poor. 4.Based on the analysis of reservoir heterogeneity, fluid barrier and interbed and the distribution of bottom water, four contributing regions are discovered. The main lies on the north of well LH11-1A. Two minors lie on the east of well LH11-1-3 and between well LH11-1-3 and well LH11-1-5. The last one lies in layer E in which the interbed is discontinuous. 5.The parameters of reservoir and fluid are obtained recurring to core analysis, logging evaluation on vertical well and parallel well, and seismic interpretation and prediction. Theses parameters provide data for the quantitative characterization of the reservoir heterogeneity and the distribution law of the fluid barrier and interbed. 6.1n the paper, an integrated method about the distribution prediction of remaining oil is put forward on basis of refined reservoir geological model and reservoir numerical simulation. The precision in history match and prediction of remaining oil is improved greatly. The integrated study embodies latest trend in this research field. 7.It is shown that the enrichment of the remaining oil with high watercut in Liuhua 11-1 oil field is influenced by reservoir heterogeneity, fluid barrier and interbed, sealing property of fault, driving manner of bottom water and exploitation manner of parallel well. 8.Using microfacies, IRH, reservoir structure, effective thickness, physical property of reservoir, distribution of fluid barrier and interbed, the analysis of oil and water movement and production data, twelve new sidetracked holes are proposed and demonstrated. The result is favorable to instruct oil field development and have gotten a good effect.

羊草繁殖生物学特性的研究

羊草(Leymus chinensis (Trin.) Tzvel. )又称碱草，隶属禾本科，赖草属，因其营养价值高，富含蛋白质，适口性好，抗旱，耐盐碱，耐贫瘠，抗逆性强，适应性广等优点，对我国发展草原畜牧业和退化草地、荒漠化治理方面具有举足轻重的作用。近年来，由于自然环境变劣，荒漠化加剧，以及过度放牧等不利影响，加之羊草本身固有的“三低”问题（即结实率低、出苗率低、产草量低）已对羊草生物多样性维持构成了严重的威胁，严重限制了我国人工草地建设和天然草地的改良和沙化治理的步伐。加强羊草生物学研究，开展羊草种质生物多样性保护，成为当前研究的紧迫课题。经对国内外相关文献的查新发现：国外发表的文献匮乏，国内的报导大多集中在草原生态等宏观领域，在羊草繁殖生物学方面缺乏系统的研究。本文以本课题组从国内外收集的羊草资源为材料，从以下几个方面进行了初步探索： 一、羊草繁殖性状与遗传多样性分子标记指标的相关分析。利用分子标记与形态标记对随机抽取的17份羊草种质进行了种质评估的比较研究。结果表明：两种方法均在17份供试材料中鉴别出9份羊草种质,说明分子标记方法用于羊草种质资源鉴定是可行的，并具有快速、准确、不受环境条件限制等优点。在40个10 Mer的随机引物当中筛选出21个有效引物，以之对9份羊草材料进行RAPD 分析，共扩增出115条带，其中95条带表现出多态性，多态比率82.61%，并筛选出S1213-900，S1213-1700，S1215-5500， S1396-1370，S1384-900，S1202-5180，S1220-2200，S1381-1580，S1211-1300，S1211-800为羊草种质所具有的10个特异性标记，据此可将羊草种质与披肩草、赖草加以区分。同时在羊草种内亦发现13条可区分供试羊草种质的特有标记。形态标记与分子标记相关性分析结果显示：羊草种质的小穗数，种子千粒重，叶色，有性繁殖量和结实率5个形态学指标与遗传多样性指标---特有带百分率及遗传距离之间，存在一定相关性。同时对羊草种质资源在收集和评价过程中存在的问题进行了探讨。 二、羊草不同基因型无性繁殖特性比较研究。以本课题组从吉林、内蒙古等省份收集的10个基因型羊草为供试材料，在相同的生态因子作用下，以吉生1号羊草为对照，对10个基因型羊草的叶数增量、芽数增量、芽高度、芽间距、芽重量、根量六个无性系形态性状指标进行测评。结果表明：基因型的差异也是影响羊草无性系生长发育的重要影响因子。因此，在今后的羊草无性繁殖生物学研究中，应综合考虑环境因子和基因型因子对羊草无性繁殖生长发育的影响。在所测评的10个基因型中，各基因型的形态性状指标差异很大，栽3基因型较其他基因型优于对照吉生1号，此结论可为今后培育羊草新种提供重要资料。 三、羊草幼穗离体培养方法的建立。其方法是取羊草幼穗为外植体，经0.1%升汞溶液表面消毒后，接种到含2mg/L的2,4-D的MS培养基上，置于恒温25℃条件下诱导愈伤组织。在加有1mg/L2,4-D的MS培养基上继代2次后，转移到含1mg/L KT和0.5mg/LNAA的MS培养基上分化培养得到再生芽。在除去激素后的基本培养基上获得了生根的试管苗。试管苗移栽到温室后生长正常。羊草试管苗的分化因基因型和外源激素条件的不同而异。 四、羊草有性生殖特性的研究。在自然条件下进行了羊草自交、异交结实性实验，采用FDA染色法检测羊草小孢子活性，并观测羊草雌蕊、雄蕊发育的时空特点。结果表明：在大田中羊草异交结实率远大于其自交结实率;成熟花药中有活性的花粉达到92.2%以上;同时，在发育时间顺序和空间结构上，羊草的雌蕊、雄蕊并不妨碍自体授粉。因此，初步结论认为羊草具自交不和性。

中国东北温带样带区域和景观尺度生态模型的研究

样带是沿全球变化某一驱动因素的主要梯度而设置的由一系列研究站点构成的区域，被认为是研究全球变化与陆地生态系统关系的最有效的途径。而模型研究是全球变化研究中不可或缺的手段。本文即采用模型研究方法研究中国东北温带样带(NECT)区域，试图揭示温带生态系统对于全球变化（尤其是降水）的反应机制。 中国东北温带样带（NECT)位于42°N - 46°N，108°E - 132°E，长约二千多公里，是最早被列入GCTE的四条样带之一，从东到西有明显的湿度梯度，被认为是温带区域研究水分梯度的代表性样带。本文研究主要集中在： 1．NECT中环境数据库的建立,本文采用EIS作为数据管理系统。由于EIS管理空间数据的特点是根据确定的地理坐标来提供空间定位，因而每一环境因子的属性值分布都有确定的地理坐标与其对应，特别适合于样带这种研究区域较大，同时又要求有精确空间定位的区域。NECT环境数据库包括地形、气候、植被、土壤、土地利用、水文、孢粉数据及社会经济等分库、本数据库力图提供各环境因子的各种属性值而代替仅仅提供类型值。 2．NECT中PFTs的划分PFTs的划分被认为是建立DGVM的前提。本文认为PFTs的划分是模型研究中一个尺度上升过程的结果，不同的尺度，不同的研究目标导致不同的PFTs的划分。在NECT区域中，考虑植被对全球变化中降水因子的不同反映机制，采用生活型、高度、耐旱特性、叶子大小、叶子季相、主根深度和木质化程度等指标根据- TWINSPAN和FCLUS进行划分，得到以下9种NECT区域中植被功能类型：常绿针叶树种、落叶针叶树种、落叶阔叶树种、落叶小叶灌木、落叶小叶半灌木、落叶强旱生半灌木、多年生中旱生草本、适应旱生环境的多年生草本和多年生强旱生草本。对NECT区域中PFTs的DCA分析表明降水是控制PFTs在NECT区域中分布的主要环境因子。在代表景观层次的长白山PFTs的划分中，则采用树种有记载的最大寿命、最大胸径、最大树高、各树种生长参数、树种自然分布区内>5℃的有效积温的最小值和最大值、耐阴、耐旱、喜肥特性、树种的扩散更新，就地下种更新和萌条更新能力参数及叶子大小和类型等指标采用上述软件得到的以下PFTs:即不耐荫阔叶树种、耐荫阔叶树种、耐荫针叶树种和不耐荫的阳生针叶树种。 3.NECT中BCM模型的建立和预测 本文认为土壤水是决定SPC系统水分状况的直接指标。而均衡土壤水分剖面代表了土壤水的多年平均状态，因而本文以Watershed模型为基础，模拟NECT区域中任意一点的均衡土壤水分剖面（精度为每经纬网格32×48个点）;然后根据这个均衡水分剖面用计算LAI子模型确定该水分剖面所能支持的LAI;进而根据这个LAI由Biome等模型划分出Biome在NECT中的分布。全球变化的结果将改变区域中任意一点的土壤水分状况，从而影响植被的LAI，进而导致Biome的改变。本模型成功的模拟了LAI和Biome在NECT区域中的分布，利用85-90生长季每月平均的NDVI作相关检验表明除5月份以外，相关系数都>0.7，而5月份也达到0,6457，都达到了极显著的程度。尤为重要的是，模型对于不同植被类型的NDVI与LAI的对应关系有良好的模拟，如针叶林的LAI在相同的NDVI值下明显比阔叶林小，因而模型模拟的LAI在NECT东部针叶林分布区LAI值比针阔混交林明显偏小，而与Spanmen等(1990)所提出的针叶林叶面积指数与NDVI关系非常一致。模型的预测显示：(1) T+20C (PET+15%)，Precipitation+20%，LAI总体上变化不大，且空间变化呈现复杂性，总体上表现出草原植被LAI减少，而森林的LAI增加;Biome层次表现出针阔混交林和矮草原面积扩大，针叶林和森林草原面积减少，其中对于该情形下变化最为明显的是针叶林和森林草原。NECT东部区域发育在沙性土上的植被的LAI明显增加，而科尔沁沙地植被的LAI则维持不变。(2)T+40C (PET+30%)，Precipitation+20%，LAI总体上将减小0.14，但空间分布不均。东部森林区域LA1将维持不变或增加（主要为针叶林），草原植被LAI仍表现出减少趋势;在Biome层次上则表现出草原面积的扩大。对于第一种情形下LAI有增有减的森林革原地区则表现出减小的一致性，总体来说，第二种情形比第一种情形表现出相当的干旱性。从对两种全球变化情形的反应来看，针叶林和森林草原是NECT中对全球变化驱动因子温度和降水的敏感植被类型;丽科尔沁沙地植被表现出相当的稳定性，表明该沙地的敏感性主要是由于人类活动这个因子造成的。 4.NECT中景观层次NPP模型的建立和预测 景观层次之所以成为模型研究中一个独特的层次，是由于地形效应的存在。地形效应对于水、热。营养物质的进行重新分配，从而进一步控制了生态系统的分布。本文选择NECT区域中森林生态系统的代表性分布小流域一二道白河小流域为研究区域。首先，应用Sunlight模型来模拟小流域任意一点所截取的能用于光合作用的太阳辐射能。Sunlight模型充分考虑了由于栅格的坡度、坡向和遮蔽度对可照时间和太阳直射辐射的影响以及坡度和可祝度对太阳散射辐射的影响，并提供了消除大气状况从站点观察数据推测的方法，即太阳直射辐射转换系数Rb和太阳散射辐射转换系数R，结合植被的分布特性，得到IPR在小流域中的分布。结果表明，IPR在小流域中相差不大，与高程呈正相关。进而利用温度修正模型得到温度修正系数，平均为0.446，表明温度对NPP的限制效应比较大;而水分修正系数则通过Topmodel模拟每一栅格的地下水位，由这个地下水位通过前述Waterbalance模型模拟均衡土壤水分剖面，进而求出水分修正系数，平均为0.86，表明该流域水分状况良好，水分状况对NPP的限制性不强。模拟结果显示：海拔1700m的岳桦林平均NPP为7.31t.ha-l年“两实测的NPP值分别为20.19 t.ha-l年 13.45 t.ha-l年‘1和5.15 t.ha-1年”。可见模型模拟的整个NPP的分布趋势与现实NPP分布一致。模型的预测表明：(1)．T+2℃( PET+15%)，P+20%时整个小流域的平均NPP将从14.60 t.ha-1年-1增加到16.65 t.ha_l年，且不同生态系统的增加幅度大致类似。以岳桦林生态系统稍高，增加幅度为15.3%，引起该小流域NPP增加的主要原因是温度状况的改善，而水分状况与变化前一致。(2)T+4℃( PET+30%)，P+20%的变化前景下NPP的增加幅度更大，整个小流域的平均NPP将达到18.63 t.ha-1年，且不同生态系统变化幅度不同．阔叶红松林、暗针叶林和岳桦林生态系统NPP增加幅度将分别达到25.8%，28.3%和32.8%.引起整个小流域NPP增加的主要原因仍旧是温度状况的大幅度提高，平均从变化前的0.477提高到0.610，而水分状况则仍保持相当的稳定性。