纳米二氧化钒薄膜的制备及红外光学性能

采用双离子束溅射方法在Si_3N_4/SiO_2/Si基底表面沉积氧化钒薄膜,在氮气气氛下热处理获得二氧化钒薄膜.利用x射线衍射(XRD)、扫描电子显微镜(SEM)和X射线光电子能谱(XPS)研究了热处理温度对氧化钒薄膜晶体结构、表面形貌和组分的影响,利用傅里叶变换红外光谱(FT-IR)对二氧化钒薄膜的红外透射性能进行了测试分析.结果表明,所制备的氧化钒薄膜以非晶态V_2O_5;和四方金红石结构VO_2为主,经400℃、2 h热处理后获得了(011)择优取向的单斜金红石结构纳米VO_2薄膜,提高热处理温度至450℃,纳米结构VO_2薄膜的晶粒尺寸减小.FT-IR结果显示,纳米VO_2薄膜透射率对比因子超过0.99,高温关闭状态下透射率接近0.小晶粒尺寸纳米VO_2:薄膜更适合在热光开关器件领域应用.

Architecture research and hardware implementation on simplified neural computing system for face identification

This paper describes a special-purpose neural computing system for face identification. The system architecture and hardware implementation are introduced in detail. An algorithm based on biomimetic pattern recognition has been embedded. For the total 1200 tests for face identification, the false rejection rate is 3.7% and the false acceptance rate is 0.7%.

Thermally induced evolution of phase transformations in gas hydrate sediment

Thermally induced evolution of phase transformations is a basic physical-chemical process in the dissociation of gas hydrate in sediment (GHS). Heat transfer leads to the weakening of the bed soil and the simultaneous establishment of a time varying stress field accompanied by seepage of fluids and deformation of the soil. As a consequence, ground failure could occur causing engineering damage or/and environmental disaster. This paper presents a simplified analysis of the thermal process by assuming that thermal conduction can be decoupled from the flow and deformation process. It is further assumed that phase transformations take place instantaneously. Analytical and numerical results are given for several examples of simplified geometry. Experiments using Tetra-hydro-furan hydrate sediments were carried out in our laboratory to check the theory. By comparison, the theoretical, numerical and experimental results on the evolution of dissociation fronts and temperature in the sediment are found to be in good agreement.

水合物沉积层中考虑相变的热传导分析

水合物沉积层中含相变的热传导是沉积物中水合物热分解的最基本的物理化学过程,热传导引起的相变区域扩展,气液渗流和土体软化变形很可能导致地层失稳,造成工程结构物的破坏或者环境灾害.本文对沉积物中水合物热分解问题进行了解耦,提出了热分解引起地层失稳问题的简便分析方法.在相变阵面假定的基础上,提出了新型的热传导模型,得到了一维自相似理论解,同时建立了相应的数值模拟方法.在实验室内进行了四氢呋喃水合物沉积物热分解模型试验,通过对比,理论分析,数值计算与试验结果吻合较好

中国沙棘(Hippophae rhamnoides subsp. sinensis)天然群体的遗传变异分析

近十年，植物群体遗传学的研究飞速发展，然而与海拔相关的植物群体遗传结构和遗传变异研究却相对较少。到目前为止，还不清楚遗传变异与海拔之间是否有一个通用的格局。在山区，各种生态因子，如温度、降水、降雪、紫外线辐射强度以及土壤成分都随海拔梯度急剧变化，造成了即使在一个小的空间区域，植被类型变化显著，这种高山环境的异质性和复杂性为我们研究植物群体遗传结构和分化提供了方便。沙棘(Hippophea)属于胡颓子科(Elaeagnaceae)为多年生落叶灌木或乔木，雌雄异株，天然种群分布极为广泛。中国沙棘(H. rhamnoides subsp. sinensis)是沙棘属植物中分布较广的一个亚种，种内形态变异非常丰富，加之其具有独特的繁育系统和广泛的生态地理分布，是研究沙棘属植物遗传变异和系统分化的理想材料。本文从1,800 m 到3,400 m 分5 个海拔梯度进行取样，用RAPD 和cpSSR 分子标记研究了卧龙自然保护区中国沙棘天然群体的遗传结构和遗传变异。5 个取样群体依次标记为A、B、C、D 和E，它们分别代表分布在海拔1,800，2,200，2,600，3,000 和3,400 m 的5 个天然群体。RAPD实验用11 条寡核苷酸引物，扩增得到151 个重复性好的位点，其中143 个多态位点，多态率达94.7%。在5 个沙棘群体中，总遗传多样性值(HT)为0.289，B群体内的遗传多样性值为0.315，这完全符合沙棘这种多年生、远交的木本植物具有高遗传变异的特性。5 个群体内遗传多样性随海拔升高呈低－高－低变异趋势，在2,200 m海拔处的B群体遗传多样性达最大值0.315，3,400 m海拔处的E群体则表现最小仅0.098。5 个群体间的遗传分化值GST＝0.406，也即是说有40.6%的遗传变异存在于群体间，1,800 m海拔处的A群体与其它群体的明显分离是造成群体间遗传分化大的原因。UPGMA聚类图和PCoA散点图进一步确证了5 个群体间的关系和所有个体间的关系。最后，经过Mantel检测，遗传距离与海拔表现了明显的相关性(r = 0.646, P = 0.011)。cpSSR 实验中，经过对24 对cpSSR 通用引物筛选，11 对引物能扩增出特异性条带，只有2 对引物(ccmp2 和ARCP4)呈现多态性。4 个等位基因共组合出4 种单倍型，单倍型Ⅰ出现在A 群体的所有个体和B 群体的8 个个体中，C、D、E 三个群体均不含有，而单倍型Ⅱ出现在C、D、E 三个群体的所有个体及B 群体的18 个个体中，A 群体不含有。另外两种单倍型Ⅲ和Ⅳ为稀有类型，仅B 群体中的4 个个体拥有。这种单倍型分布模式和TFPGA 群体聚类图揭示了，C、D、E 群体可能来源于同一祖先种，而A 群体却是由另一祖先种发展起来的，B 群体则兼具了这两种起源种的信息，这可能是因为在历史上的某一时期，在中国沙棘群体高山分化的过程中，B 群体处某个或者某些个体发生了基因突变，具备了适应高海拔环境的能力，产生了高海拔沙棘群体的祖先种。 In recent ten years, studies about population genetics of plants developed rapidly,whereas their genetic structure and genetic variation along altitudinal gradients have beenstudied relatively little. So far, it is uncleared whether there is a common pattern betweengenetic variation and altitudinal gradients. In the mountain environments, importantecological factors, e.g., temperature, rainfall, snowfall, ultraviolet radiation and soil substratesetc., change rapidly with altitudes, which cause the vegetation distribution varying typically,even on a small spatial scale. The mountain environments, which are heterogeneous andcomplex, facilitate and offer a good opportunity to characterize population genetic structureand population differentiation.The species of the genus Hippophae L. (Elaeagnaceae) are perennial deciduous shrubs ortrees, which are dioecious, wind-pollinated pioneer plants. The natural genus has a widedistribution extending from Northern Europe through Central Europe and Central Asia toChina. According to the latest taxonomy, the genus Hippophae is divided into six species and12 subspecies. The subspecies H. rhamnoides ssp. sinensis shows significant morphologicalvariations, large geographic range and dominantly outcrossing mating system. Thesecharacteristics of the subspecies are favourable to elucidate genetic variation and systemevolution. To estimate genetic variation and genetic structure of H. rhamnoides ssp. sinensisat different altitudes, we surveyed five natural populations in the Wolong Natural Reserve at altitudes ranging from 1,800 to 3,400 m above sea level (a.s.l.) using random amplifiedpolymorphic DNA markers (RAPDs) and cpSSR molecular methods. The five populations A,B, C, D, and E correspond to the altitudes 1,800, 2,200, 2,600, 3,000 and 3,400 m,respectively.Based on 11 decamer primers, a total of 151 reproducible DNA loci were yielded, ofwhich 143 were polymorphic and the percentage of polymorphic loci equaled 94.7%. Amongthe five populations investigated, the total gene diversity (HT) and gene diversity within population B equaled 0.289 and 0.315, respectively, which are modest for a subspecies of H.rhamnoides, which is an outcrossing, long-lived, woody plant. The amount of geneticvariation within populations varied from 0.098 within population E (3,400 m a.s.l.) to 0.315within population B (2,200 m a.s.l.). The coefficient of gene differentiation (GST) amongpopulations equaled 0.406 and revealed that 40.6% of the genetic variance existed amongpopulations and 59.4% within populations. The population A (1,800 m a.s.l.) differed greatlyfrom the other four populations, which contributes to high genetic differentiation. A UPGMAcluster analysis and principal coordinate analyses based on Nei's genetic distances furthercorroborated the relationships among the five populations and all the sampling individuals,respectively. Mantel tests detected a significant correlation between genetic distances andaltitudinal gradients (r = 0.646, P = 0.011).Eleven of the original 24 cpSSR primer pairs tested produced good PCR products, onlytwo (ccmp2 and ARCP4) of which were polymorphic. Four total length variants (alleles) werecombined resulting in 4 haplotypes. The haplotype was present in all individuals of Ⅰpopulation A and 8 individuals of populations B, the other three populations (C, D and Epopulations) did not share. The haplotype was present in all individuals of populations C, D Ⅱand E and 18 individuals of populations B, population A did not share. The other twohaplotypes and were rare haplotypes, which were only shared in 4 individuals of Ⅲ Ⅳpopulation B. The distribution of haplotypes and TFPGA population clustering map showedthat the populations C, D and E might be origined from one ancestor seed and population Amight be from another, whereas population B owned information of the two ancestor seeds. Itwas because that gene mutation within some individual or seed in the location of population Bwas likely to happen in the history of H. rhamnoides, which was the original ancestor of thehigh-altitude populations.

一株嗜杂醇油细菌的分离、鉴定和特性研究

为结合一般白酒存在的杂醇油含量偏高或超标问题，作者试图寻找能嗜高醇类(含杂醇油)的有效菌株加以开发利用。本文研究了一株从富集分离、定向诱导得到的嗜异戊醇的W-2菌，该菌能以异戊醇或其它某些多碳醇作为唯一的碳源和能源进行生长。该菌在PH8.5的环境条件下，异戊醇的利用率可高达84.4%。此外，该菌还能广泛利用糖类、醇、有机酸、酯、盐等有机物作为唯一的碳源和能源。一般不利用—碳化合物。该菌具单极生鞭毛，呈杆状，适宜生长温度范围4℃—43℃。最适生长温度36℃，在PH4.0—11.0均能生长，最适生长PH为8.5—9.0，在培养基产生蓝绿色色素。W-2菌经形态，生理生化鉴定为假单胞菌属中的铜绿假单胞菌的一个变种。初步定名为Pseudomonas aeruginosa W-2。本文最后讨论了该菌的开发应用前景。

Synthesis, photophysical properties, and theoretical studies on pyrrole-containing bromo Re(I) complex

Two bromo rhenium(I) carbonyl complexes with the formula of [Re(CO)(3)(L)Br], where L = 1,10-phenanthroline (Phen-Re) and 5-(1H-pyrrol-1-yl)-1,10-phenanthroline (Pyph-Re), were successfully synthesized with the aim to analyze the effect of the pyrrole (Py) moiety on the photophysical properties of Pyph-Re. It was found that the triplet metal-to-ligand charge-transfer d pi (Re) --> pi*(N-N) emission of Phen-Re and Pyph-Re centered at ca. 527 nm with the luminescence quantum yield (LQY) of 0.015 and ca. 578 nm with the LQY of 0.011, respectively. At the same time, the geometrical structures of the ground state and the absorption spectral properties of Phen-Re and Pyph-Re were also calculated with the 6-31G* basis set employed on C, H, N, O, and Br atoms, and LANL2DZ adopted on Re atom.

Synthesis and characterization of a novel hybrid single crystal [Ga-3(PO4)(3)F-2]H3O center dot (H3NCH2CH2)(2)NH2

A novel three-dimensional fluorinated gallium phosphate has been hydrothermally,synthesized by using diethylenetriamine as an organic structure-directing agent. X-ray single crystal structure analysis indicates this compound crystallizes in the orthorhombic space group P-bca, a = 1. 605 6 (7) nm, b = 1.011 4 (4) nm, c=1. 854 6(5) nm, V=3. 011 6(19) nm(3), Z=4. The three-dimensional framework based on linkage of corner-sharing polyhedron PO4, GaO4F and GaO4F2 delimit ten-ring channels along b axis in which the triply protonated amines are located serving as charge compensating guests and supporters.

A nickel molybdenum phosphate with tunnel: Hydrothermal synthesis and structure of (NH3CH2CH2NH3)(4)center dot(NH3CH2CH2NH2)center dot Na center dot[Ni2Mo12O30(PO4)(HPO4)(4)(H2PO4)(3)]center dot 6H(2)O

A nickel molybdenum phosphate, (NH3CH2CH2NH3)(4).(NH3CH2CH2NH2). Na .[Ni2Mo12O30(PO4)(HPO4)(4)(H2PO4)(3)]. 6H(2)O, invoicing molybdenum present in V oxidation, has been hydrothermally synthesized and structurally characterized by single crystal X-ray diffraction. Deep brown-red crystals are formed in the triclinic system, space group P (1) over bar, a = 12,011(2), b = 14,612(3), c = 21.252(4) Angstrom, alpha = 80.54(2)degrees, beta = 83.10(2)degrees, gamma = 76.29(2)degrees, V = 3561.4(12) Angstrom(3), Z = 2, lambda(MoK alpha) = 0.71073 Angstrom (R(F) = 0.0529 for 9880 reflections), Data mere collected on a Siemens P4 diffractometer at 20 degrees C in the range of 1.75 degrees < theta < 23.02 degrees using the omega-scan technique. The structure was solved by direct methods using the program SHELXTL-93 and refined with the method of fun-matrix least-squares on F-2. The structure of the title compound may be considered to be two [Mo6O15(HPO4)(H2PO4)(3)](5-) units bonded together with a nickel atom, although several P-O groups are not protonated on account of coordination with a Na+ cation, The one-dimensional tunnels were formed in the solid of the title compound. A probe reaction of the oxidation of acetaldehyde with H2O2 using the title compound as catalyst was carried out in a liquid- solid system, showing that the title compound had high catalytic activity in the reaction, (C) 1999 Academic Press.

Synthesis, electrical properties and crystal structure of a new radical-ion salt based on pi-extended bis(TTF) and a Keggin heteropolymolybdate

By electrocrystallization of 2,6-[4,5-bis(n-butylsulfanyl)-1,3-dithiol-2-ylidene]-4,8-bis(6-iodo-n-hexyloxy)-1,3,5,7-tetrathia-s-indacene (BHBDTI) and [NBu4](4)[SiMo12O40] in the mixed solvent CHCl2CH2Cl and CH3CN, the new radical-ion salt [C42H60Cl2O2S12](2)[SiMo12O40] was prepared. It was characterized by means of IR and ESR spectroscopy and X-ray diffraction. In the crystal structure, organic radical dications and silicomolybdate anions are alternatively arranged along the a axis to form a 1-D conducting layer. The organic layer consists of two isolated groups of BHBDTI divided by the (011) plane without short interatomic contacts. However, in each group, BHBDTI molecules associate with each other in a head to tail manner running along the [011] direction and face-to-face overlapping with a relative shift by approximately one TTF subunit along the long axis of the molecule and a slight shift along the short axis of the molecule with significantly short S ... S contacts. The room-temperature d.c. conductivity determined by the two-probe method is 10(-4) S cm(-1), suggesting that the compound is a semiconductor.

Studies on water-swellable elastomers .2. Thermal properties and crystalline behavior of amphiphilic graft copolymers with poly(ethylene glycol) side chains

The thermal properties and crystalline structure of the amphiphilic graft copolymers CR-g-PEG600, CR-g-PEG2000, and CR-g-PEG6000 using chloroprene rubber (CR) as the hydrophobic backbone and poly(ethylene glycol) (PEG) with different molecular weights as the hydrophilic side chains were studied by DSC and WAXD. The results showed that a distinct phase-separated structure existed in CR-g-PEGs because of the incompatibility between the backbone segments and the side-chain segments. For all the polymers studied, T-m2, which is the melting point of PEG crystalline domains in CR-g-PEG, decreased compared to that of the corresponding pure PEG and varied little with PEG content. For CR-g-PEG600 and CR-g-PEG2000, T-m1, which is the melting point of the CR crystalline domains, increased with increasing PEG content when the PEG content was not high enough, and at constant PEG content, the longer were the PEG side chains the higher was the T-m1. The crystallite size L-011 of CR in CR-g-PEGs increased compared to that of the pure CR and decreased with increasing PEG content. (C) 1997 John Wiley & Sons, Inc.

藻类有机物在富含粘土海洋沉积物中的氧化还原降解研究

研究海洋沉积有机物的早期成岩过程是海洋地球化学的重要内容，也是研究全球碳循环不可缺少的核心课题。本文通过模拟有机物在沉积物－海水界面的降解实验，研究了海洋藻类有机物在富含粘土沉积物中不同氧化还原条件下的降解过程及有机物稳定碳同位素比值的变化。通过为期245天的培养实验，我们分析测定了总有机碳（TOC）、脂肪酸、长链烷烃的含量随时间的变化以及总有机碳和单一脂肪酸化合物同位素组成的变化。结果表明粘土、沉积物氧化还原环境、微生物活动，化合物分子结构、有机物来源等是影响有机物降解的重要因素。藻类有机物在富含粘土沉积物中的降解是一个快速过程，其降解速率可以用简单的早期成岩公式（-dGt / dt = ∑kiGi）很好的描述。应用该模型计算了脂肪酸和长链烷烃的降解速率常数。其中脂肪酸的降解速率常数为0.011-0.119 d-1，低于已报道的用未添加粘土的海洋沉积物培养实验得到的速率常数值。该研究实验显示，粘土对沉积有机物有一定的吸附作用，从而对有机物的降解过程起到不同程度的保护作用。长链烷烃的降解速率常数比脂肪酸稍高，为0.013-0.158 d-1，该值与已报道的经水体降解后沉降到海洋沉积物中残余长链烷烃的降解速率常数相当。TOC，脂肪酸和长链烷烃的降解在氧化环境下比在还原环境下快。脂肪酸和长链烷烃的降解不仅受到环境因素的影响，其自身分子结构特征也是很重要的控制因素。脂肪酸化合物双键数目越多，降解的越快；长链烷烃的碳链越短，降解越快。沉积有机物的早期成岩过程对总有机碳及不同化合物的稳定碳同位素比值具有不同的影响。在245天的培养实验过程中，总有机碳稳定同位素比值（δ13C）有所降低，但变化范围不大且受环境影响较小。而几种主要脂肪酸的δ13C值有不同程度的变化趋势。14：0和16：1的δ13C值降低，18：1的δ13C值升高，而16：0和20：5的δ13C值基本保持不变。因此，在利用沉积物中的生物标志化合物碳稳定同位素研究有机物来源及古海洋生物地球化学过程时，应考虑到早期成岩作用对其同位素比值的影响。

中国近海浮游细菌生物量与生产力的生态分布特点

本论文研究了胶洲湾、东海和渤海的蓝细菌（Synechococcus）、生物量、异养细菌生物量和生产力的生态学特点。并在汇泉湾、渤海和东海用分极增减法对海洋蓝细菌在微型食物环（the microbial loop）中的作用进行了初步研究。在以上海区调查研究的时间如下：胶州湾：1993年2月、5月、9月11月，1996年5月、1999年3月、5月和12月。汇泉湾：1996年4月至1998年4月。东海：1997年2-3月，1998年7月。渤海1998年9-10月，1999年4-5月。研究结果如下：胶州湾：蓝细菌生物量的变化范围是11.4-0.03 mgC/m~3，季节变化是夏季>秋季和春季>冬季。其水平分布是除夏季蓝细菌生物量是沿岸浅水区向湾外递减外，其它三季（春、秋和冬季）是由湾外向湾内至沿岸浅水区递减。蓝细菌生物量与海水温度周年变化正相关，与季节海水温度的关系是秋、冬季分布变化一致，春、夏季分布变化相反。海水温度是影响胶州湾蓝细菌生物量分布变化的主要原因。异养细菌生物量和生产力的变化范围分别是29.8-1.62 mgC/m~3; 129.12-1.92 mgC/m~3.d。季节变化都是夏季>秋季、春季>冬季。夏季的异养细菌生物量和生产力水平分布趋势与蓝细菌生物量的分布变化相同。海水温度对异养细菌生产力的影响较对异养细菌生物量的影响大。异养细菌生产力相比（BP:PP）的变化在0.58-0.02之间，季节分布变化是夏季>秋季、春季>冬季。夏季表层的BP:PP由沿岸浅水区向湾心、湾口和湾外递减。东海：蓝细菌生物量的变化范围是46.72-0.011 mgC/m~3，夏季高平均是23.59 mgC/m~3，冬季低平均是3.61 mgC/m~3。冬季蓝细菌生物量的水平分布明显受黑潮的影响，在表面和20米层是由东南向西北方向递减。其垂直分布是冬季表层和20米层>底层，夏季是20米层>表层>底层；在连续站冬111站和410站变化都是中层>底层>表层。异养细菌生物量和生产力的变化范围分别是17.2-4.4 mgC/m~3（1997.2）；376.8-7.2 mgC/m~3.d。异养细菌生产力夏季高平均是35.1 mgC/m~3.d。异养细菌生物量的水平分布是由沿岸向外海递增（1997.2），异养细菌生产力的水平分布是冬季异养细菌生产力在32度断面有由沿岸向外递减趋势，PN断面的变化与冬季相似。垂直分布，冬季和夏季的异养细菌生产力的垂直变化在2断面是底层大于表面，PN断面则是表层大于底层，32度断面大多断站是底层大于表层。在连续站冬季111站异养细菌生产力的变化是底层>中层>表层，409站的变化是中层>底层>表层，夏季111站和410站都是中>底层>表层。异养细菌生物量（1997.2）表层分布变化与海水温度分布变化相似，底层变化相反。异养细菌生产力与初级生产力相比（BP:PP），冬季在0.04-0.30之间，平均为0.17；夏季在0.20-0.43之间平均0.32。冬季在长江口附近BP：PP有一个高值区是0.30，夏季在111站附近有一个高值区是0.43。从连续站111站和409’站观测发现底层的BP：PP明显高于表层。渤海：蓝细菌生物量秋季（16.6-0.37 mgC/m~3）比春季（0.44-0.015 mgC/m~3）高。其秋季的水平分布与海水盐度水平分布相同，与海水温度水平分布相反。异养细菌生产力秋季（189-62.2 mgC/m~3.d）与春季（193.2-49.8 mgC/m~3.d）相当。但秋季捕层BP普遍小于底层，而春季是表层普遍大于底层。根据颗粒分级培养实验结果，海洋蓝图细菌在微型食物环中的作用如下：在汇泉湾的春季和秋季蓝细菌可能主要被小型浮游动物（microzooplankton 20-200 μm）捕食。在渤海的春季和秋季也是同样结果。但在东海夏季的111站和410站附近（东海大陆架中部）微型浮游动物（nanozooplankton 2-20 μm）对蓝细菌的捕食压力明显。

海带、裙带菜和羊栖菜的遗传分析

利用AFLP标记对海带在太平洋西北沿岸的6个主要栽培品系和6个野生地理隔离种群进行遗传多样性和亲缘关系分析。通过10对选择性引物总共检测到547个位点。在品系和种群水平，多态性位点比例（P），基因多样性（H）和香农指数（I）在大连野生种群中最高（P: 59.05%; H: 0.2057; I: 0.3062），而在连江栽培品系中最低（P: 9.87%; H: 0.0331; I: 0.0497）。在物种水平（即对所有品系和种群来说），P, H 和I 的值分别是85.01%，0.1948和0.3096。以个体间的相似系数（Dice）和种群间的遗传距离为基础，用非加权类平均法（UPGMA）分别构建个体和种群间的系统树图。AMOVA分析显示，大部分的遗传变异（60.21%）存在于品系和种群间，少部分（39.79%）存在于品系或种群内。遗传分化系数GST的值是0.6226，与FST的值（0.6021）非常接近，基因流（Nm）的值是0.1515，这三个值表明种群（品系）间存在高度的遗传分化。Mantel检验发现6个野生种群的遗传距离或遗传分化与地理距离呈正相关性（相关系数分别是r=0.8870, P=0.007 和 r=0.7962, P=0.011），符合“距离隔离（isolation by distance, IBD）”模型。总体来说，种群（品系）内的遗传多样性处于低到中等水平（大连种群除外），而它们之间的遗传分化程度非常高。 用AFLP和微卫星标记对裙带菜配子体克隆单一交配组合的孢子体后代的遗传一致性进行分析。在这项研究中，建立了2个配子体克隆单一交配系（M1和M2），2个自交系（S1和S2）并采集1个野生种群（W）。11组AFLP引物总共检测到318个位点。M1, M2, S1, S2 和W的多态性位点比例分别是4.7%，0.3%，17.9%，16.4%和36.5%。M1和M2个体间的遗传相似度（95.6-100%）要高于S1和S2（87.7-98.4%）以及W（81.5-92.1%）。在微卫星分析中，用了6个位点。M1在其中的5个位点基因型一致，而在Up-AC-2B2位点显示出不同的基因型。M2在所有6个微卫星位点的基因型都一致。而S1, S2和W都在2个以上的位点检测到不同的基因型。总之，AFLP与微卫星的分析结果一致，即配子体克隆单一交配组合的孢子体后代呈现高度遗传相似性，但也存在细微的差异。 对中国羊栖菜主产区浙江省洞头县的12个羊栖菜养殖品系的重要形态特征进行了比较研究，并利用AFLP技术对一个典型养殖种群的遗传多样性进行了分析。结果显示，这12个品系在全长、全湿质量、侧枝长、侧枝湿质量、侧枝密度等方面存在显著或极显著差异（P<0.05或P<0.01）。8组AFLP引物在这个典型养殖种群中扩增出198个片段，其中多态性片段为166个，多态性位点比例为83.8%。根据个体间的遗传距离，以UPGMA法构建了个体间的系统树图，27个羊栖菜个体聚为一枝，作为对照的铜藻为另一枝。本研究从形态和DNA分子水平说明了浙江洞头羊栖菜养殖种群具有高度遗传多样性。