稻田CH4和N2O的排放及养萍和施肥的影响

用箱法对我国东北稻田ＣＨ４和Ｎ２Ｏ排放进行观测研究表明,东北稻田的ＣＨ４排放通量比南方稻田小,平均日排放通量和生长季节排放总量分别为０．０７和７．４ｇ·ｍ－２．稻田淹水期几乎没有Ｎ２Ｏ的净排放,但在非淹水期内却有大量Ｎ２Ｏ排放（平均通量５９μｇＮ２Ｏ·ｍ－２·ｈ－１）．稻田养萍和施肥明显促进ＣＨ４和Ｎ２Ｏ排放．稻田ＣＨ４和Ｎ２Ｏ排放之间存在消长关系．制定稻田温室气体减排技术措施时应充分注意这一关系．     

栽培稻—紧穗野生稻双二倍体的产生及其细胞遗传学研究

从栽培稻与紧穗野生稻杂种Ｆ１的花培再生植株Ｈ１中,筛选到Ｅ１３和Ｅ２４两个抗褐飞虱的双二倍体,并对其遗传行为进行了研究。与杂种Ｆ１相比,双二倍体表现为植株变矮,每穗颖花数减少,穗长与花药长增加,颖花变大,并具有较低的自交育性,Ｈ１代的结实率分别为２．７２％和３．５５％,Ｈ２代分别为４．２９％和４．７２％。进一步对Ｅ１３和Ｅ２４的花粉母细胞染色体配对情况进行观察,发现两者中期Ｉ染色体构型分别为０．６９Ｉ＋２３．５４Ⅱ＋０．０６Ⅳ和０．５９Ⅰ＋２３．３６Ⅱ＋０．１４Ⅳ。本研究还发现,两个材料的Ｈ２和Ｈ３植株染色体数均为２ｎ＝４８,彼此形态表现相似,说明上述双二倍体具有相对高的遗传稳定性。     

固定化酵母细胞生产1,6—二磷酸果糖研究

本文研究了固定化酵母细胞制备果糖１,６二磷酸的方法及其生产。用卡拉胶包埋方法固定化酿酒酵母,对含葡萄糖１．０Ｍ,磷酸盐０．８Ｍ的糖磷液,ＰＨ６．５在３７℃下进行磷酸化反应。反复分批转化２０天以上,可达到平均产ＦＤＰＨ４ ２７．５８ｍｇ／ｍｌ。最高为５９．９４ｍｇ／ｍｌ。     

辽河三角洲湿地的景观格局分析

利用遥感,ＧＩＳ手段对辽河三角洲湿地景观的格局与异质性进行研究,结果表明,研究区空间格局的基本构型以大斑块与主体,破碎化程度较低,基本呈聚集型分布,构成景观主体的是稻田景观,苇田景观和滩涂景观,尤以稻田景观为最,聚集度指数人工湿地为０．９２４,自然湿地次之为０．８９７,半自然湿地为０．８７０,整个研究区共有斑块１２１３个,最大斑块为１４０１．３８ｋｍ＾２,最小斑块只有０．３９４ｋｍ＾２,其间相差３     

八倍体小滨麦与4D缺体杂交后代小染色体的传递与遗传效应

７２１８０ ４Ｄ缺体附加的１对小染色体（ｔｉ）为亚中部着丝点染色体,其大小为常染色体平均长度的１／３￣１／４。ＰＭＣ ＭＩ,染色体构型为１９．５９”（１８￣２０）＋０．４６’（０￣４）＋０．０９””（０￣１）＋０．９６ｔｉ”（０￣１）＋０．０８ｔｉ’（０￣２）,９６．１９％的细胞中,ｔｉ 色体联会成环状二价体,８２．３８％的ｔｉ”游离在赤道板两边,与常染色体不联会,且推后分离,与八倍体小滨麦杂交的     

向日葵CMS育性恢复的研究

向日葵细胞质雄性不育（Ｃｙｔｏｐｌａｓｍｉｃｍａｌｅｓｔｅｒｉｌｉｔｙ,ＣＭＳ）育性恢复的机理是非常复杂的。运用遗传学和分子生物学方法,分析了具代表性的４种不同细胞质类型的ＣＭＳ育性被恢复的频率和２０种向日葵自交系对１９种ＣＭＳ的恢复能力及个别ＣＭＳ植株自发恢复的原因。实验结果表明,４种ＣＭＳ品系育性被恢复的频率分别为５８．８％．５６．３％．１１．８％和０％．２０种自交系的恢复力为５．９－７５．０％。部分ＣＭＳ品系和大多数自交系含有恢复基因,恢复基因的数量及类型决定了ＣＭＳ品系被恢复的程度及自交系的恢复能力。同时,提出并证实了线粒体不育基因变异是导致ＡＲＧ１ＣＭＳ植株自发恢复育性的主要原因。     

红景天中药复方对低氧劳动能力的影响

我们研制了以藏产大花红景天为主要成分的中药复方用以提高机体的低氧劳动能力。在模拟海拔１００００ｍ的小鼠游泳实验中,药物组和对照组动物的存活时间分别为７３．２±３．８和６０．５±４．０ｍｍ（Ｐ＜０．０５）;游泳６０ｍｉｎ（相当于对照组的平均存活时间）以后死亡的百分数分别为５３．０％和３５．８％（Ｐ＜０．０５）。大鼠在模拟海拔５０００ｍ游泳１ｈ,药物组和对照组动物的血乳酸含量分别为１４．６±１．８和２１．１±１．９ｍｍｏｌ／Ｌ（Ｐ＜０．０５）。在模拟海拔４３００ｍ低压舱内人体运动负荷试验中,药物组和对照组受试者的ＰＷＣ１７０分别为９８０．４±５２．８和８６６．４±３０．０（Ｐ＜０．０１）。提示,红景天中药复方能明显提高低氧劳动能力。     

放线菌果胶酶产酶条件及酶促反应条件的研究

从埋麻土壤中分离到放线菌２９８株,经初筛和复筛得到产酶活性较高的一株放线菌５－７１。最适产酶条件是：果胶０．５％,葡萄糖０．５％,蛋白胨０．５％,酵母粉０．１％,Ｋ２ＨＰＯ４ ０．１％,ＫＨ２ＰＯ４ ０．１％,ＮａＣｌ０．１％,ＭｇＳＯ４·７Ｈ２Ｏ０．０５％,ｐＨ８．０。２５℃培养３天达产酶高峰。通气量对产酶影响不大。酶促反应最适条件是：ｐＨ９．６,４５℃,底物果胶浓度０．７５％,作用时间９０ｍｉ     

不同水平的丙型肝炎病毒感染者的生物学行为特征

用“巢式”－ＰＣＲ（聚合酶链反应）检测丙型肝炎病毒（ＨＣＶ）,可将感染病毒水平进行半定量;当一步扩增即可得阳性结果为高水平感染,需两步扩增才得阳性结果为低水平感染。有输血史的患者高水平感染占６８％,无输血史的患者高水平感染占３５．１％（ｐ＜０．０５）,高水平感染组肝功能损害严重,ＡＬＴ、ＡＳＴ分另１１为１１０．０±５９．９μ／Ｌ,９６．１±４９．３μ／Ｌ低水平感染组分别为５４．４±２８．１μ／Ｌ,５４．４±２０．０μ／Ｌ,（Ｐ＜０．０１,Ｐ＜０．０２）丙型肝炎抗体的检测情况与病毒感染水平无统计学意义。     

人参不同栽培群体遗传关系的RAPD分析

用随机扩增多态ＤＮＡ（ＲＡＰＤ）标记法对４个人参（Ｐａｎａｘ ｇｉｎｓｅｇ Ｃ．Ａ．Ｍｅｙｅｒ）栽培群体中存在较丰富的遗传多样性。分析一路参、三路参、系选品系５９号、北京参等４个人参栽培群体和１个西洋参（Ｐ．ｑｕｉｎｑｕｅｆｏｌｉｕｍ Ｌ．）群体的遗传分化指数值表明,三路参变异量最大（０．４１６９）,一路参降为０．２５６５,边条参系选品系５９号最低为０．１８８１,表明选择方式和选择代数的纯化作用十分     

Characterization of the Major Capsid Genes (g23) of T4-Type Bacteriophages in the Wetlands of Northeast China

To obtain genetic information and to evaluate the composition of T4-type bacteriophage (phage) communities in wetlands, environmental soil and water DNAs were obtained from two natural wetlands dominated by Carex lasiocarpa and Deyeuxia angustifolia plant species, and a neighboring paddy field in Sanjiang plain of northeast China. The biomarker gene of g23, which encodes the major capsid protein of T4-type phages, was amplified with primers MZIA1bis and MZIA6, and the PCR products were cloned and sequenced. In total, 96 and 50 different g23 clones were obtained from natural wetlands and a paddy field, respectively. A larger number of clones with low levels of identity to known sequences were found in water than in soil both in the natural wetlands and the paddy field, suggesting that many of T4-type phages in wetland water and paddy floodwater in Sanjiang plain are uncharacterized. Phylogenetic analyses showed that the g23 clones in natural wetlands, irrespective of water and soil, were distinctly different from those in marine waters, lake waters, and upland black soils, but were similar to those in paddy fields. The UniFrac analysis of g23 assemblages indicated that T4-type phage community compositions were different between soils and waters, and also were different between the natural wetlands and the paddy field. In general, the global analysis of g23 clone assemblages demonstrated that T4-type phage community compositions were different among natural wetlands, marines, lakes, paddy fields, and upland black soils.     

三江平原自然湿地与人工湿地双向演替动态过程研究

基于遥感和GIS技术,分析1986～2005年三江平原自然湿地(湖泊、河流、沼泽湿地)与人工湿地(水田)的双向演替过程,统计分析自然地理环境背景(土壤类型、海拔高度、坡度和地貌类型)对此过程的影响。研究结果表明,1986～2005年间三江平原湿地双向演替过程以沼泽湿地与水田之间的相互转化为主。1986～1995年、1995～2000年和2000～2005年三时段内沼泽湿地转化为水田的面积占同期沼泽湿地转出总面积的比例分别为7.61%、37.99%和28.81%,相反,水田转化为沼泽湿地的面积占同期水田转出总面积的4.83%、13.69%和4.84%。三江平原发生沼泽湿地与水田双向演替过程的主要自然地理环境背景为土壤类型为草甸土和沼泽土,海拔高度为0～100 m,坡度为0～1°,地貌类型为低河漫滩、高河漫滩、洼地和一级阶地。     

湿地甲烷代谢对氮输入响应的复杂性及其机制分析

氮素是影响湿地甲烷代谢过程的重要因素之一。氮输入是否影响湿地甲烷排放,增加全球气候变暖的风险,一直受到科学界的高度关注。目前关于氮输入对湿地甲烷排放影响的几篇meta-analysis文章的主要结论均为氮输入促进湿地甲烷排放,但是多篇研究性论文的结果为氮输入抑制或不影响湿地甲烷排放,由此可见氮输入对湿地甲烷排放的影响十分复杂。湿地甲烷代谢包括湿地甲烷产生、氧化和传输过程以及最终的甲烷排放,综述不同形态氮输入对水稻田、内陆湿地和滨海湿地甲烷排放通量影响的复杂性;分析湿地甲烷产生速率和途径、甲烷好氧氧化和硝酸盐/亚硝酸盐型厌氧甲烷氧化对不同形态氮输入的响应及机制。硝态氮输入对湿地甲烷产生具有抑制作用已成共识,然而其它形态氮输入对湿地土壤甲烷产生的影响具有较大的不确定性,氮输入影响湿地甲烷产生的机制主要包括电子受体-底物竞争机制、离子毒性机制、促进植物生长-碳底物供给增加机制以及pH调控机制等。氮输入对湿地好氧甲烷氧化影响的研究多集中在水稻田和泥炭湿地,影响的结果包括促进、抑制或影响不显著;氮输入促进湿地土壤硝酸盐/亚硝酸盐型厌氧甲烷氧化。着重分析氮输入对湿地甲烷代谢影响不确定性的成因,指出...     

Conversion from natural wetlands to paddy field alters the composition of soil bacterial communities in Sanjiang Plain,Northeast China

The Sanjiang Plain is the largest freshwater wetlands in Northeast China. In order to feed the growing population, about 84 % of the wetlands in this area have been converted to farmland, especially to paddy fields, since the 1950s. However, little is known about the influence of this conversion on soil microbial community composition. In this study, soil samples were collected from two natural wetlands dominated by plant species Carex lasiocarpa and Deyeuxia angustifolia and from a neighboring paddy field that was changed from wetland more than 10 years ago. The composition and diversity of bacterial communities in the soils were estimated by clone library analysis of nearly full length of 16S rDNA sequences. The results revealed that bacterial diversity was higher in paddy fields, and that the composition of bacterial communities differed among the three samples; the difference was more notable between the paddy field and two natural wetlands than between two natural wetlands. The distribution of clones into different bacterial phyla differed among soil samples, and the conversion from natural wetlands to paddy field increased the abundance of Proteobacteria and Firmicutes but decreased the abundance of Chloroflexi. About 63 % and 71 % of clones from two natural wetlands and 49 % of clones from the paddy field had <93 % similarity with known bacteria, suggesting that the majority of bacteria in natural wetland soils in the Sanjiang Plain are phylogenetically novel. In general, this study demonstrated that long-term conversion from natural wetlands to paddy field changes soil bacterial communities in the Sanjiang Plain.     

Effects of reclamation of natural wetlands to a rice paddy on dissolved carbon dynamics in the Sanjiang Plain,Northeastern China

Natural wetlands play an important role in the global carbon cycle, and loss of dissolved carbon through water has been indicated as one of the most important carbon sources for riverine ecosystems. During the last century, a large natural wetland area was reported to be converted to other land use types such as rice paddy land around the world. In this study, we explored the dynamics of dissolved organic carbon (DOC) and dissolved inorganic carbon (DIC) in two natural freshwater wetlands and a rice paddy field, which was reclaimed from the natural wetlands in the Sanjiang Plain, Northeastern China, during the growing season (May–October) of 2009. The DOC and DIC concentrations in the two ecosystems were significantly different (P < 0.05). The mean DOC concentrations during the growing season in the surface water of the Deyeuxia angustifolia and Carex lasiocarpa wetlands were 49.88 ± 5.44 and 27.97 ± 1.69 mg/L, respectively, while it was only 8.63 ± 2.54 mg/L in the rice paddy field. Specific ultra-violet light absorption at 254 nm (SUVA₂₅₄) of DOC increased by an average of 19.54% in the surface water from the natural wetlands to rice paddy, suggesting that DOC mobilized in the natural wetlands was more aromatic than that in the rice paddy field. The mean DIC concentration in surface water of the rice paddy was 5.25 and 5.04 times higher than that in the natural D. angustifolia and C. lasiocarpa wetlands, respectively. The average ratio of DIC to dissolved total carbon (DTC) for the water sampled from the artificial drainage ditch in the rice paddy field was 61.82%, while it was 14.75% from the nearby channel of natural wetlands. The significant differences in dissolved carbon concentration in surface water and channels originating from different land use types suggested that reclamation of natural wetlands to rice paddy field would reduce DOC runoff and increase the DIC concentration to adjacent watersheds. Our study results for the changed pattern in dissolved carbon after the natural wetland was transformed to paddy field could have important implications for studying the impacts of the large-scale land use change to carbon cycle and management.     

Organic and inorganic carbon in paddy soil as evaluated by mid-infrared photoacoustic spectroscopy

Paddy soils are classified as wetlands which play a vital role in climatic change and food production. Soil carbon (C), especially soil organic C (SOC), in paddy soils has been received considerable attention as of recent. However, considerably less attention has been given to soil inorganic carbon (SIC) in paddy soils and the relationship between SOC and SIC at interface between soil and the atmosphere. The objective of this research was to investigate the utility of applying Fourier transform mid-infrared photoacoustic spectroscopy (FTIR-PAS) to explore SOC and SIC present near the surface (0-10 μm) of paddy soils. The FTIR-PAS spectra revealed an unique absorption region in the wavenumber range of 1,350-1,500 cm(-1) that was dominated by C-O (carbonate) and C-H bending vibrations (organic materials), and these vibrations were used to represented SIC and SOC, respectively. A circular distribution between SIC and SOC on the surface of paddy soils was determined using principal component analysis (PCA), and the distribution showed no significant relationship with the age of paddy soil. However, SIC and SOC were negatively correlated, and higher SIC content was observed near the soil surface. This relationship suggests that SIC in soil surface plays important roles in the soil C dynamics.     

羊草草地枯枝落叶中N,P,K变化动态

羊草草地枯枝落叶中Ｎ、Ｐ、Ｋ变化动态郭继勋,祝廷成（东北师范大学国家草地生态工程实验室,长春１３００２４）ＤｙｎａｍｉｃｓｏｆＮ,ＰａｎｄＫｉｎｌｉｔｔｅｒｓｏｎＡｎｅｕｒｏｌｏｐｉｄｉｕｍｃｈｉｎｅｎｓｅｇｒａｓｓｌａｎｄ．￥ＧｕｏＪｉｘｕｎａｎｄ...     

湿地农田生态系统的特点及其调节

所谓湿地,系一个笼统的名称,直到目前并没有确切的定义。通常认为凡受地下水与地表水影响的土地均可称为湿地。它又可区分为两大类,即自然湿地与人工湿地,区别在于受不受人为活动干扰及其干扰程度。湿地包括沼泽型土壤、草甸型土壤与稻田土壤,稻田土壤在我国早期的土壤分类系统中也归为湿地族。近年来,国外对湿地研究十分活跃,从已有文献看其概念也欠确切,且因目的不同而有一定出入。例如在W.Z.Mitsh所著《湿地》一书中就引用了如下几种概念: 1.湿地系为浅水或间歇浅水层所淹没的低地,包括有植被着生的浅水湖区。2.水位接近或高于地表的土地,或者由于长期水分饱和形成的湿地,或者是具有水成土过程的土地,包括水成土以及适于水生植物     

哈尼梯田湿地土壤不同形态磷的时空分布特征

磷是湿地和农业生态系统中的重要元素之一,其中土壤磷形态的迁移转化广受关注。以哈尼梯田湿地为例,分别在哈尼梯田湿地的水稻生长期、收获期和休闲期,采集湿地不同海拔（梯田区上部、中部和下部）和不同深度的土壤（0-20 cm,20-40 cm,40-60 cm,60-80 cm）进行磷形态分析,研究了哈尼梯田湿地土壤中不同形态磷的时空分布规律和影响因素。结果表明：（1）哈尼梯田湿地土壤中总磷（TP）含量均值为318.74 mg/kg,在水稻收获期含量最高,无机磷（IP）含量均值在水稻休闲期最高（85.95 mg/kg）,湿地土壤磷总体呈缺乏状态。（2）受外源磷输入影响,铁铝结合态磷（NaOH-P）占无机磷比重最大,且季节差异性显著（P<0.05）;而钙结合态磷（HCl-P）在各季节无显著差异（P>0.05）,这与湿地生态环境和地质背景有关。（3）哈尼梯田湿地对磷的迁移有截留作用,表现为各形态磷含量总体呈现在上部梯田湿地较高,并随海拔的降低而降低;不同形态磷含量在20-40 cm土层富集。（4）除HCl-P外,其余形态磷与土壤粒径在不同土层表现为负相关;不同土层TP和有机磷（OP）与pH值呈正相关;土壤总有机碳（TOC）与不同形态磷在收获期呈显著负相关（P<0.05）。研究表明了哈尼梯田湿地立体空间结构和人为活动能影响湿地生态系统中磷的分布与迁移循环,该结论可为梯田湿地的可持续发展提供参考。     

有机肥氮投入比例对双季稻田根际土壤微生物生物量碳、氮和微生物熵的影响

为探明不同有机肥氮素占总氮投入的百分比对双季稻区早、晚稻各生育时期稻田根际土壤微生物的影响,本研究以大田定位试验为平台,应用氯仿熏蒸-K₂SO₄提取法和化学分析法系统分析了施用化肥N(M₁)、30%有机肥N(M₂)、50%有机肥N(M₃)、100%有机肥N(M₄)和无N对照(M₀)5个不同施肥处理双季稻田根际土壤微生物生物量碳(MBC)、微生物生物量氮(MBN)和微生物熵的差异.结果表明: 在早稻和晚稻各主要生育时期,施肥措施均能提高稻田根际土壤MBC、MBN和微生物熵,各施肥处理根际土壤MBC、MBN和微生物熵均随水稻生育期推进呈先增加后降低的变化趋势,均于齐穗期达到最大值,成熟期为最低值;其中,各处理双季稻田根际土壤MBC、MBN、MBC/MBN值和微生物熵一般均表现为M₄＞M₃＞M₂＞M₁＞M₀,M₂、M₃和M₄处理间均无显著差异,但均显著高于M₀处理.可见,单独施用化肥措施对提高根际土壤微生物生物量碳、氮和微生物熵效果有限,施用有机肥或有机无机肥配施提高根际土壤微生物生物量碳、氮和微生物熵的效果较好.