长白赤松和红松土壤微生物活性对高浓度CO_2的响应(英文)

研究了2003 年夏季长白赤松和红松土壤微生物活性对高浓度CO2的响应规律。结果表明,长白赤松和红松土壤细菌数量受高浓度CO2影响显著(p < 0.05)减少;与对照箱(350 μmol ·mol-1 CO2)和裸地(350 μmol ·mol-1 CO2)相比,红松土壤淀粉酶和转化酶活性降低,而长白赤松土壤淀粉酶和转化酶活性却表现为增加;同时发现受700 μmol ·mol-1 CO2处理的红松和长白赤松土壤微生物生物量碳均表现为显著降低。DGGE 结果表明:受高浓度CO2 的影响,长白赤松和红松土壤细菌群落结构发生了明显的变化。研究结果表明土壤微生物对高浓度CO2的响应规律与所研究的的树种有关。图2 表2 参29。

Low-temperature heat capacity and thermodynamic properties of crystalline carboxin (C12H13NO2S)

Carboxin was synthesized and its heat capacities were measured with an automated adiabatic calorimeter over the temperature range from 79 to 380K. The melting point, molar enthalpy (Delta(fus)H(m)) and entropy (Delta(fus)S(m)) of fusion of this compound were determined to be 365.29 +/- 0.06K, 28.193 +/- 0.09 kJ mol(-1) and 77.180 +/- 0.02 J mol(-1) K-1, respectively. The purity of the compound was determined to be 99.55 mol% by using the fractional melting technique. The thermodynamic functions relative to the reference temperature (298.15 K) were calculated based on the heat capacity measurements in the temperature range between 80 and 360 K. The thermal stability of the compound was further investigated by differential scanning calorimetry (DSC) and thermogravimetric (TG) analysis. The DSC curve indicates that the sample starts to decompose at ca. 290degreesC with the peak temperature at 292.7degreesC. The TG-DTG results demonstrate the maximum mass loss rate occurs at 293degreesC corresponding to the maximum decomposition rate. (C) 2003 Elsevier B.V All rights reserved.

长白山北坡暗针叶林倒木贮量和分解的研究

对长白山北坡海拔 12 6 0m和 16 2 0m暗针叶林中倒木蓄积、生物量和倒木的分解进行了比较研究 ,结果表明 ,暗针叶林中倒木的蓄积为 180 .87m3·hm-2 ,占林分蓄积的 2 1.83 % .低海拔的倒木蓄积和生物量均比高海拔的低 ,海拔 12 6 0m的倒木蓄积为 5 2 .5 7m3·hm-2 ,生物量为 2 6 .2 1t·hm-2 ;海拔 16 2 0m的倒木蓄积为 193.85m3·hm-2 ,生物量为 5 3 .33t·hm-2 .用单项指数衰减模型对倒木的分解进行模拟可知 ,倒木的分解常数随树种和海拔高度的不同而不同 .冷杉倒木的分解常数比云杉倒木大 ;倒木在低海拔的分解常数比在高海拔的大 ,表明云杉倒木完全分解需要较长的时间 .

合理施用沼渣对土壤钾素有效性影响

通过室内干湿交替培养研究了沼渣对沈阳地区耕地棕壤和草甸土中速效钾含量及其对外源钾固定的影响,结果发现(1)加入沼渣可以明显促进供试土壤中钾素的释放,棕壤和草甸土对照中速效钾含量分别在高于99.24和83.23mg·kg-1时,干燥导致速效钾含量降低,含6%沼渣的棕壤和草甸土速效钾含量低于130.53和139.29mg·kg-1时,干燥就会引起层间钾的释放;(2)加入沼渣可以减少土壤对外源钾的固定量,含2%和6%沼渣的棕壤在干湿交替培养15天后,固钾量分别比对照减少了12.51和54.81mg·kg-1,相应的草甸土分别比对照减少固钾量达62.57和137.66mg·kg-1,固钾率分别降低了12.93%和28.46%。

The Synthesis and Characterization of a Novel (E,E)-Dioxime and its Mono- and Heterotrinuclear Complexes Containing an 18-Membered Dioxadithiadiazamacrocycle

The novel (E,E)-dioxime, 5,6:17,18-dibenzo-11,12-(4-nitrobenzo)-2,3-bis(hydroxyimino)-7,16-dithia-10,13-dioxa-1,4-diazacyclooctadecane) (H2L), has been synthesized from reaction of (E,E)-dichloroglyoxime (1) with 2,3:14,15-dibenzo 8,9-(4-nitrobenzo)-4,13-dithia-7,10-dioxa-1,16-diazahegzadecane (2). The mononuclear Co(III) complex (4) of this dioxime was prepared by oxidation of the cobalt (II) complex. The -capped Co(III) complex (5) was synthesized by using a precursor Co(III) complex and boron trifluoride dietherate. The heterotrinuclear complexes (6) and (7) were prepared by reaction of (5) with NiCl2·6H2O and CdCl2·H2O, respectively. In addition, the homotrinuclear Cu(II) complex (8), has also been prepared by the reaction of this dioxime with CuCl2·H2O. The structures of the dioxime and its complexes were identified by using elemental analysis, 1H- and 13C-NMR, IR, and mass spectral data.

Positive interactions in communities

Current concepts of the role of interspecific interactions in communities have been shaped by a profusion of experimental studies of interspecific competition over the past few decades. Evidence for the importance of positive interactions — facilitations — in community organization and dynamics has accrued to the point where it warrants formal inclusion into community ecology theory, as it has been in evolutionary biology.

黄土丘陵区土壤水资源评价指标与分析

在总结土壤水研究现状和对土壤水的资源特性认识的基础上,重新定义了土壤水资源,土壤水资源是指植物根系可吸收利用的范围,其补给主要来源于大气降水,即能被植物(包括农作物)及土壤微生物所利用并可以恢复和更新的土壤水的数量;并阐述了土壤水资源的特征,它具有对降水依赖性与相关性,不易保存性或易耗散性,不可开采性与就地利用性,有效性和无效性,可调控性的特征;提出了土壤水资源的评价指标,包括土壤水资源最大存储量、可利用量、无效水资源量和实际存储量;根据评价指标初步计算了黄土丘陵区典型地区的土壤水资源。

a dynamic model to handle defect-oriented processes

Tongji Univ, Inst Dev Study, Syst Engn Soc China, Comm Syst Dynam, Syst Dynam Soc, China Chapter, Shanghai Inst Foreign Trade, Syst Dynam Soc, Chapters Asia Pacific Area

人工降雨条件下谷子地留茬的水土保持效应研究

通过人工模拟降雨试验研究了谷子地不同留茬高度及不同坡度的水土保持效应。结果表明,15cm留茬高度相对于未留茬处理径流量减少了18.6%,留茬5cm与10cm无显著减少径流作用;留茬能够减小产沙量14.36%～19.47%;5,10,及15cm留茬高度对产流时间没有显著影响,坡度的变化对产流时间无显著影响;坡度为10°时,径流对土壤的侵蚀最明显;留茬高度为15cm的处理水土保持效应最佳。

水体质量综合评价的物元模型

对水体的可拓性做了充分地分析和研究,说明了利用可拓学方法对水体质量进行分析评价的适宜性。并且应用可拓学的理论和方法,对水体的物征和质量特性进行了全面分析,建立了相应的物元模型,为水体的质量评价提供了一种新的科学方法。

黄土高原典型土壤矿物固定态铵变化的南北差异

采集从北向南依次分布的干润砂质新成土(神木)、黄土正常新成土(延安)和土垫旱耕人为土(杨陵)等典型土壤剖面0—200 cm土层土样,通过测定土样全氮和矿物固定态铵,以阐明黄土高原典型区域土壤全氮和矿物固定态铵及二者比率随地理位置和土层的变异规律,为全面了解黄土高原土壤相对稳定氮库累积提供科学数据。结果表明,不同地理位置、不同土层全氮和矿物固定态铵含量存在显著差异。从南到北全氮和矿物固定态铵呈下降趋势,但各土壤全氮和矿物固定态铵的分布显著不同,全氮含量在0—60 cm随土层深度增加下降很明显,60—120 cm有一定下降,120 cm以下低而稳定。矿物固定态铵在全剖面上的分布比较均匀,随土层深度的变化差异不显著,不同土层间的差异基本在误差范围内,土垫旱耕人为土、黄土正常新成土和干润砂质新成土表层(0—10 cm)矿物固定态铵平均含量分别为215.80±7.45、165.80±8.73和146.50±1.83 mg/kg,表层以下(10—200 cm)平均含量分别为193.40±9.67、157.14±5.75和142.02±5.47 mg/kg。从地理位置分析,干润砂质新成土、黄土正常新成土和土垫旱耕人为土表层...

干旱和复水条件下转基因甘薯的光合特性

以转铜锌超氧化物歧化酶(Cu/Zn SOD)和抗坏血酸过氧化物酶(APX)基因甘薯(TS)及未转基因甘薯(NT)为实验材料,研究在旱后复水条件下转基因甘薯及未转基因甘薯抗氧化酶活性和光合特性变化。结果显示,连续36 h胁迫条件下,TS和NT的SOD活性都先降低后升高,但TS的SOD活性始终高于NT。胁迫至24 h时,TS的SOD活性约为NT的1.2倍,复水后二者SOD活性都下降。持续胁迫,TS的APX活性先升高后降低,NT与之相反,复水后TS和NT的APX活性都是先升高后降低,复水12 h,TS的APX活性是NT的1.5倍。水分胁迫条件下TS的膜质受伤害程度要轻于NT,胁迫24 h,复水12 h,NT的MDA含量均约为TS的1.2倍。胁迫12 h,TS和NT净光合速率都下降,继续胁迫,TS净光合速率开始上升,NT几乎保持不变,胁迫36 h,TS的净光合速率约为NT的1.5倍。复水后二者净光合速率都开始上升,复水12 h,TS净光合速率约为NT的3倍。胁迫时TS、NT胞间CO2浓度(Ci)都逐渐增大,胁迫36 h时NT胞间CO2浓度显著高于TS,是其1.4倍。实验结果表明,同时转入SOD、APX抗氧化基因后,在...