59 resultados para Salustio Crispo, Cayo, 83-35 a. C.


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Rates of maximum food consumption and growth were determined for immature mandarin fish Siniperca chuatsi (47.2-540.2 g) and Chinese snakehead Channa argus (45.0-546.2 g) at 10, 15, 20, 25, 30 and 35 degrees C. The relationship between maximum rate of food consumption (C-max), body weight (W) and temperature (T) was described by the multiple regression equations: lnC(max) = -4.880 + 0.597 lnW+0.284T - 0.0048T(2) for the mandarin fish, and lnC(max)= -6.718 + 0.522 lnW+0.440T-0.0077T(2) for the Chinese snakehead. The optimum temperature for consumption was 29.6 degrees C for the mandarin fish and 28.6 degrees C for the Chinese snakehead. The relationship between growth rate (G), body weight and temperature was ln(G+0.25)= - 0.439 - 0.500 lnW+0.270T - 0.0046T(2) for the mandarin fish, and ln(G+0.25)= - 6.150+ (0.175 - 0.026T) lnW+0.571T - 0.0078T(2) for the Chinese snakehead. The weight exponent in the growth-weight relationship was -0.83 for the mandarin fish, but decreased with increasing temperature for the Chinese snakehead. The optimum temperature for growth was 29.3 degrees C for the mandarin fish, but tended to decrease with increasing weight for the Chinese snakehead, being 30.3 degrees C for a 45-g fish, and 26.1 degrees C for a 550-g fish. (C) 1998 The Fisheries Society of the British Isles.

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工业革命以来,由于人口的快速增加和人类活动的强烈干扰(主要包括煤炭、石油等石化燃料的燃烧、化肥生产和使用)导致土地利用/覆被变化、大气CO2浓度升高、N沉降等一系列全球环境变化问题。有关陆地生态系统生物地球化学循环,尤其是陆地生态系统CN循环及其耦合过程方面的研究成为全球变化科学研究领域的重要内容。 干旱/半干旱地区占地球陆地总面积的1/3。与湿润地区相比较,干旱/半干旱地区生态系统稳定性比较差,往往属于生态脆弱区。因此,全球变化对干旱/半干旱地区生态系统影响更加敏感。科尔沁沙地位于我国北方干旱/半干旱地区,是我国典型的农牧交错区和生态脆弱区。科尔沁沙地是世界上人口密度最高的干旱/半干旱地区之一,人类活动对其影响剧烈。然而,有关科尔沁沙地生态系统CN元素生物地球化学循环过程对土地利用/覆被变化、N沉降等全球变化响应及其反馈机制的研究非常缺乏。因此,本文以科尔沁沙地退化沙质草地、农田、不同年龄樟子松和杨树人工林等生态系统为对象,开展了造林、模拟N沉降和凋落物管理对生态系统CN元素循环过程影响的研究。 在科尔沁沙地东南缘,以退化沙质草地、樟子松(Pinus sylvestris var. mongolica)人工林(15、24和30年生)、杨树(Poplus xiaozhuanica)人工林(7、11和15年生)为对象,研究草地转变为林地对生态系统CN储量影响;以退化草地、榆树疏林草地和32年生樟子松人工林为对象,比较草地造林对土壤CN循环过程及其土壤微生物性状的影响;以农田和5、10、15年生杨树人工林为对象,研究退耕还林对生态系统CN储量和循环过程影响;以35年生樟子松人工林为对象,模拟研究N沉降和凋落物管理对生态系统CN循环过程影响。通过上述研究,得到以下主要结果: (1)草地生态系统总C量为34.38 Mg ha-1,15、24和30年生樟子松人工林生态系统总C量分别为43.56、60.45和66.59 Mg ha-1,7、11和15年生杨树人工林生态系统总C量分别为34.54、48.26和78.77 Mg ha-1;与农田相比,退耕5年的杨树人工林生态系统总C储量下降13%,而10年和15年杨树人工林分别增加了176%和5倍;随着人工林年龄的增加,地上植被生物量C储量占生态系统总C储量的比例逐渐增加,并主要分配在树干。草地生态系统总N库储量为2.54 Mg ha-1,15、24和30年生樟子松人工林生态系统总N库储量分别为1.96、2.10和2.19 Mg ha-1,7、11和15年生杨树人工林生态系统总N库储量分别为2.27、1.84和2.60 Mg ha-1;与农田相比,退耕5年的杨树人工林生态系统总N库储量下降32%,而10年和15年杨树人工林分别增加了47%和76%;农田和草地造林后生态系统N储量依然主要分配在土壤中。 (2)草地和农田造林后土壤CN库储量的变化受多因子的影响,例如林龄、树种种类以及立地条件等。农田和草地造林初期,土壤CN库储量表现出下降趋势,随着林龄的增加,土壤CN储量逐渐恢复。草地营造樟子松人工林30年后,0–60 cm深度土壤CN储量依然显著低于草地;与草地相比,15年生杨树人工林土壤CN储量差异不显著。在立地条件较好的情况下,10年杨树人工林土壤CN储量已显著高于农田;然而,在立地条件相对较差的情况下,15年杨树人工林土壤CN储量仍然与农田相比差异不显著。 (3)土地利用变化能够强烈地改变土壤CN循环过程。与草地或疏林草地相比,32年生樟子松人工林土壤CN、P含量显著降低;土壤CN矿化过程发生显著变化,并且受季节变化的影响;在不同季节,土壤微生物量碳含量、代谢熵(qCO2)、微生物熵(MBC/TOC以及土壤酶活性等在不同土地利用条件下表现出规律不一致。同样,农田退耕杨树人工林能够显著影响土壤CN矿化过程,土壤无机氮(铵态氮+硝态氮)含量,土壤微生物量碳含量以及土壤微生物活性。草地造林在一定程度上导致土壤质量下降。而农田造林有利于土壤质量改善,尤其在在立地条件较好情况下。 (4)N添加增加对沙地樟子松人工林地上和地下CN元素含量影响不大;N添加1年后,仅林下植被CN含量显著增加,高氮处理(N15)凋落物N含量显著增加。N添加抑制了沙地樟子松人工林凋落物的早期分解和N、P元素释放。5、6、8和9月份土壤无机N含量均随着N输入增加表现出一定程度的增加,然而,7月份N添加导致土壤无机N含量降低。N添加对土壤潜在N矿化速率影响不显著。7和8月份N添加影响土壤C化速率,而其它月份影响不显著。低氮处理(N5)有利于增加土壤微生物量碳含量,而高氮处理(N15)在一定程度上降低土壤微生物量碳含量。 (5)凋落物输入变化(凋落物添加和凋落物移出)在一定程度上改变了35年生沙地樟子松人工林生态系统CN循环过程。凋落物移出(C0)增加了林下植被C量,降低了树木叶片N含量。凋落物移出抑制了凋落物分解和P元素的释放,而增加了C素的早期释放速率,对N元素释放过程影响不显著。凋落物输入变化对不同月份土壤无机N含量和土壤N矿化过程影响均不显著。仅在6月份凋落物移出显著抑制了土壤C化速率,其它月份差异均不显著。凋落物管理对土壤微生物量碳含量影响不显著。 以上研究结果表明,土地利用变化、N沉降和凋落物输入改变等能够影响半干旱地区沙地生态系统CN储量和循环过程。尤其是土地利用变化强烈改变沙地生态系统CN储量、分配格局和循环过程,并且受到多因子的影响。科尔沁沙地樟子松人工林生态系统CN元素生物地球化学循环存在密切的耦合关系。今后有必要进一步结合3S技术、同位素技术、模型模拟以及分子生物学技术等,从微观-宏观不同尺度上,研究半干旱地区沙地生态系统CN循环过程对全球变化的响应及其反馈机制。

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In view of the growing interest in endohedral lanthanide fullerenes, Ce, as a typical +4 oxidation state lanthanide element, has been systematically studied. The synthesis, extraction and electronic structure of Ce@C-2n are investigated. Soot containing Ce@C-2n was synthesized in high yield by carbonizing CeO2-containing graphite rods and are back-burning the CeC2-enriched cathode deposit in a DC are plasma apparatus. Ce@C-2n, dominated by Ce@C-82, can be efficiently extracted from the insoluble part of the soot after toluene Soxhlet extraction by pyridine at high temperature and high pressure in a closed vessel. About 60% Ce@C-2n (2n = 82,80,78,76) and 35% Ce@C-82 can be enriched in the pyridine extract. This fact is identified by desorption electron impact mass spectrometry (DEI MS). The electronic structure of Ce@C-2n is analyzed by using X-ray photoemission spectroscopy (XPS) of pyridine-free film. It is suggested that the encapsulated Ce atom is in a charge state close to +3 and was effectively protected from reaction with water and oxygen by the enclosing fullerene cage. Unlike theoretical expectation, the electronic state of Ce@C-82 is formally described as Ce+3@C-82(3-). (C) 1997 Elsevier Science Ltd.

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油蒿(Artemisia ordosica Krasch.)是内蒙古鄂尔多斯高原特有的半灌木,构成该地区沙地优势植被类型。主要分布在固定、半固定沙丘,同时在流动沙丘也有少量分布。它在当地经济价值、防风固沙环保方面均处于无以取代的地位。在毛乌素沙地沙漠化日益扩大的严峻态势下,研究其群落地上、地下过程对生境变化的响应不仅对维持干旱、半干旱区生态系统稳定的管理措施上有所帮助,而且也有助于了解全球变化背景下物种对环境条件的长期变化适应策略。 为此,本项研究以毛乌素沙地为研究区域,利用异速生长关系确立不同生境油蒿生物量最佳回归方程,并调查、比较了毛乌素沙地固定沙丘、半固定沙丘和流动沙丘三个生境油蒿灌丛地的生物量、土壤和植被的碳储量、生产力和细根周转、土壤微生物生物量碳、氮和土壤呼吸。具体结果如下: 1. 建立并比较了油蒿枝、株两个水平上各部分(不含细根)生物量异速生长关系式,其中枝形态指标(枝直径BD、枝长BL、叶枝长LBL)与油蒿叶、枝、果各部分生物量的异速关系最好;株水平上冠层面积CA与其叶、枝干、果、粗根各部分生物量的回归效果较好。不同生境生物量与其生长变量的异速生长关系存在差异。2004年调查的油蒿灌丛生物量从固定沙丘、半固定沙丘到流动沙丘分别是354.8,178.3和30.4 g m-2;各部分(叶、枝干、果、粗根、不同径级细根的)生物量都呈递减趋势。地下根与总生物量比值排序为固定>半固定>流动沙丘。不同生境细根生物量垂直分布存在差异,在固定沙丘根可至100 cm,半固定沙丘达90 cm,而在流动沙丘仅为60 cm,这些结果有助于使了解不同生境中的相同物种如何通过自身形态及其生物量调整来适应生境的差异。 2. 不同生境油蒿灌丛地植被碳储量和土壤碳储量在P < 0.05水平上差异显著,其中固定沙丘植被碳储量和土壤碳储量分别为224.04和7521 g C m-2,半固定沙丘是119.27和3029 g C m-2,流动沙丘是16.83和2300 g C m-2。可见沙区土壤有机碳远大于植被碳量。 3. 利用最大值减最小值方法、标准取样法和内生长土芯法研究了不同生境油蒿灌丛地的地上、粗根生产力和地下细根生产力。发现各生境生产力、细根周转都随着植被盖度增加而增加,地下根生产力与总生产力之比随着植被盖度增加而减少;不同生境油蒿灌丛地生产力在P < 0.05水平上存在显著差异,2005年总生产力范围在18.23-293.82 g m-2 yr-1之间;细根总周转率在0.16-0.54 yr-1之间。 4. 利用异速生产关系确立不同生境不同水平上油蒿叶面积的最佳回归关系式并对不同生境的比叶面积(SLA进行了比较,其中枝水平上各生境叶面积与枝直径、枝叶长、枝长相关关系在P < 0.001水平上显著;株水平上各生境叶面积与株高、冠层面积相关关系在P < 0.001水平显著;从固定沙丘、半固定沙丘到流动沙丘SLA大变小,这可能与生境养分差异有关。 5. 不同生境油蒿灌丛地土壤微生物碳、氮和土壤呼吸范围分别在117.99-153.99 mg kg-1、1.49-3.31mg kg-1和0.54-1.96 μmol m-2 s-1之间,它们从固定沙丘、半固定沙丘到流动沙丘依次下降。

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草地生态系统中,放牧对调节物质流动和营养循环起着关键的作用。内蒙古地区已有上千年的游牧历史,放牧是该地区重要的草地利用方式之一。然而,近50年来,由于人口的剧增以及对草原的不合理利用与管理,使得内蒙古草原发生了严重的退化与沙漠化。理解放牧对氮循环的定量影响,对我们更合理地利用草地、防治生态系统的进一步退化以及探求最佳恢复途径都具有重要的意义。中国科学院内蒙古草原生态系统定位站精准设置的5种放牧强度处理(0.00, 1.33, 2.67, 4.00, 5.33 羊/公顷)为我们的研究提供了理想的平台。2005、2006年生长季期间,在经过16年不同放牧强度处理的一个典型草原样地上,我们测定了氮素输入(氮沉降、生物固氮)、转化(净氮矿化)、输出(反硝化及氨气挥发)速率等N循环的重要参量。同时,测定了微生物生物量碳、氮(CmicNmic及微生物呼吸(Rmic,研究了微生物在氮循环中的作用。另外,还测定了植物、土壤、固氮体中的15N自然丰度值,探讨了其对不同放牧强度的响应格局与机理。 结果表明,干湿混合沉降物全氮浓度最高达11.53 mg N l–1,沉降量最高为1.77 kg N ha1m–1。月均氮沉降量与浓度正相关,它们与降水量均关系密切,前者更密切。结皮面积所占比例很小,不超过8%。结皮含氮量为1.01-1.43 g N kg–1,受放牧的影响不显著,但随放牧强度的增加有降低的趋势。土壤结皮能固氮,但固氮量不超过土壤氮含量的1倍。地耳的固氮量为结皮的10-20倍,故是主要的固氮体。尽管地耳含氮量受放牧影响不显著,但放牧是不放牧条件下地耳氮含量的1.58倍。 土壤NH4+-N浓度随季节变化范围为1.71-9.45 µg N g–1,它们在各放牧处理之间的差异不显著。土壤NO3–-N浓度变幅为0.27-11.21 µg N g–1。总无机氮浓度在不放牧条件下的变幅为2.69-14.57 µg N g–1,占总氮的0.49-2.6%;放牧条件下的变幅为2.49-8.66 µg N g–1,占总氮的0.35-1.21%。总无机氮浓度随季节和放牧强度的变化趋势与硝态氮相似,表现为2005年夏季期间有逐渐增加的趋势,而在2006年整个生长季期间有逐渐降低的趋势。不放牧比放牧条件下含氮量高,但在4个放牧处理之间的差异不显著。净氮矿化速率的变幅为–0.61-0.27 µg N g–1d–1,峰值通常出现在7月。净氮矿化速率在各处理间没有一致性差异,但中牧(2.67、4.00 羊/公顷)通常比重牧(5.33 羊/公顷)下的值高。净氮硝化速率通常很低,波动在–0.32-0.16 µg N g–1之间,2005年夏季及2006年春秋季的值相对较高。净氮硝化速率在各放牧处理之间差异不显著,但重牧条件下的值通常最低。累积净氮转化量在年际间差异大,2005年总体上遵循正态分布模式,而2006年随着放牧强度的增加有直线下降的趋势,2006年比2005年的累积量高。土壤温度和湿度比放牧强度对净氮矿化的影响更加显著。放牧强度通过调节这两个土壤因子对氮动态而产生间接影响。 反硝化和N2O的释放速率低,前者变幅为0.33-6.21µg N kg–1 d–1,后者为0.42-11.28 µg N kg–1 d–1。释放量夏季较强,春秋较弱。放牧对反硝化释放影响不显著,只在2005年对N2O释放影响显著。尽管如此,反硝化和N2O释放速率整体表现出在不放牧比放牧条件下高的趋势,且比最高放牧强度5.33 羊/公顷下的反硝化速率显著高。然而,它们在4个放牧处理之间的差异始终不显著。累积反硝化和N2O释放存在年际变化,2006年的值显著高。它们随着放牧强度的递增有逐渐降低的趋势,这在2006年表现得尤为明显,这种结果主要归因于土壤总氮量在长期放牧条件下随放牧压力的增加而逐渐降低。 氨气挥发速率变幅为0.88-3.52 g N ha1d–1,高峰值出现在5月,2005比2006年同期的速率大。两年间放牧强度对氨气挥发的影响都较弱,2005年影响更弱。不放牧条件下的氨气挥发量通常最低,这在生长季的前期表现得更为明显,中牧及重牧条件下通常最高。放牧能影响氨气挥发与氨态氮,硝态氮及总无机氮浓度之间的关系,即不放牧条件下相关性显著,而放牧条件下相关性不显著。年际间氨气挥发速率与无机氮浓度之间的关系趋势相反,2005年负相关,2006年正相关。在水分充足的2006年,所有处理条件下氨气挥发与土壤水分及温度之间显著相关,但在单独每个放牧处理下,相关性不显著。 Cmic幅大,为13.97-350.45 μg C g–1,占土壤总有机碳的1.58-8.35%。最高和最低值分别出现在夏季和春季。它们在各处理间差异不显著,不放牧下的值相对偏高。Cmic土壤有机C全N、前期的立枯、凋落量及含N量、优势种前期的地上生物量、根系生物量、土壤温度以及水分之间关系密切。氮素状态如氨态氮、总无机氮含量、反硝化以及N2O释放速率,氨气挥发速率与Cmic间关系密切。Nmic土壤全氮的0.41-2.74%,不受季节和放牧强度的显著影响。Nmic可溶性N,表土层根系全N,立枯有机C地上生物量之间关系密切。氮循环过程中氨气挥发速率受Nmic影响。Rmic季节而变化,通常5月份值最高。Rmic着放牧强度的增加有稍降低的趋势。Rmic土壤可溶性C有机C不同土层根系有机C凋落物、立枯量及其CN含量、全N,地上生物量,优势种前期的生物量,土壤温度之间关系密切。土壤氮循环动态如氨态氮、硝态氮、总无机氮浓度及反硝化速率与Rmic间关系密切。 土壤、植物、地耳、生物结皮的δ15N值与放牧强度之间相关关系不显著。然而,放牧有增加表层土和植物的δ15N值而降低表土、地耳、结皮的δ15N值的趋势。表层土δ15N值与前一年生长季末期硝态氮及总无机氮浓度,反硝化速率及累积氨气挥发之间密切相关。 土壤碳含量的变幅为10.44-17.19 g C kg–1,全氮量的变幅为0.54-0.82 g N kg–1。长期的高强度放牧降低了土壤碳、氮储量。根系碳、氮含量分别为土壤碳、氮含量的40-50和10倍。立枯和凋落物有机碳含量变幅为446.94-507.01 g C kg–1,与放牧强度之间关系不密切;氮含量变幅为4.58-7.18 g N kg–1,与放牧强度之间显著负相关。优势种木地肤、冷蒿的含碳量与放牧强度之间相关不显著,但含氮量与之显著相关。 综述以上结果,不同放牧强度对内蒙草地生态系统氮循环中不同过程产生影响的程度各不相同,这种影响主要是通过它与土壤环境因子如温度、水分的联合作用而间接产生。

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Sertoli cells play a central role in the control and maintenance of spermatogenesis. Isolated Sertoli cells of mouse and rat testes have been shown to secrete plasminogen activator (PA) and a plasminogen activator inhibitor type-1 (PAI-1) in culture. In this study, we have investigated the hormonal regulation of PA and PAI-1 activities in cultured monkey Sertoli cells. Sertoli cells (5x10(5) cells/well) isolated from infant rhesus monkey testes were preincubated at 35 degrees C for 16 h in 24-well plates precoated with poly(D-lysine) (5 mu g/cm(2)) in 0.5 mi McCoy's 5a medium containing 5% of fetal calf serum and further incubated for 48 h in 0.5 mi serum-free medium with or without various hormones or other compounds, PA as well as PAI-1 activities in the conditioned media were assayed by fibrin overlay and reverse fibrin autography techniques respectively. The Sertoli cells in vitro secreted only tissue-type PA (tPA), no detectable amount of urokinase-type PA (uPA) could be observed, Monkey Sertoli cells were also capable of secreting PAI-1, Immunocytochemical studies indicated that both tPA and PAI-1 positive staining localized in the Sertoli cells, spermatids and residual bodies of the seminiferous epithelium; Northern blot analysis further confirmed the presence of both tPA and PAI-1 mRNA in monkey Sertoli cells. Addition of follicle-stimulating hormone (FSH) or cyclic adenosine monophosphate (cAMP) derivatives or cAMP-generating agents and gonadotrophin-releasing hormone (GnRH) agonist or phorbol ester (PMA) to the cell culture significantly increased tPA activity. PAI-1 activity in the culture was also enhanced by these reagents except 8-bromo-dibutyryl-cAMP, forskolin and 3-isobutyl-1-methylxanthin (MIX) which greatly stimulated tPA activity, whereas decreased PAI-1 activity, implying that neutralization of PAI-1 activity by tile high level of tPA in the conditioned media may occur. These data suggest that increased intracellular signals which activate protein kinase A (PKA), or protein kinase C (PKC) can modulate Sertoli cell tPA and PAI-1 activities, The concomitant induction of PA and PAI-1 by the same reagents in the Sertoli cells may reflect a finely tuned regulatory mechanism in which PAI-1 could limit the excession of the proteolysis.

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There were large losses of exotic species Elodea nuttallii during summer in eutrophic lakes of the middle and lower reaches of the Yanatze River, China. To investigate the main causes, the heat tolerance of E. nuttallii was studied and compared with that of native species Ceratopkyllum demersum by using an aquaria system in the laboratory. Under 4500 lx light intensity and 12-h L/12-h D cycle, E. nuttallii cultured in 1/5 Hoaglands solution at 39 degrees C showed a positive growth rate during the first 15 days, and the growth rate was higher than that at 35 degrees C. But after 15 days, the growth rates became negative for those cultured both at 39 and 35 degrees C. However, the growth rate was positive for more than 20 days for those cultured at 25 degrees C. Under the same conditions, the growth rate, productivity and chlorophyll content of E. nuttallii were significantly higher than that of C. demersum. Heat tolerance of E. nuttallii was also stronger than that of C. demersum. The optimal temperature for the growth of the two plants depended on the experimental period: both plants grew at an optimal rate at higher temperature if the experimental period was short; nevertheless the plants achieved optimal growth at a lower temperature if the experiment was conducted for a longer period. At the same light intensity, the heat tolerance of C. demersum in tap water with sediment was markedly stronger than that of E. nuttallii at 39 degrees C. Average growth rate of C. demersum was 4.5 times higher than that of E. nuttallii within 25 days. The positive growth period lasted for less than 25 days for E. nuttallii and for more than 25 days for C. demersum. When they were cultured in 1/5 Hoaglands solution and in tap water with sediment, the growth rate of C. demersum increased from 0.4 to 79.4 mg/d.g fresh weight (FW) within 20 days. E. nuttallii increased from 8.3 to 24.4 mg/d-g FW within 20 days. Both grew better in tap water with sediment than in 1/5 Hoaglands solution. The results demonstrated that the nutritional status of the water other than the high temperature affected the heat tolerance of E. nuttallii during summer. E. nuttallii has great ecological safe risk in China.

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Effects of water temperature (17, 21, 25, 30 and 35 degrees C) and body size (14.75-281.41 g initial body weight) on food consumption, growth, feed conversion, and dry matter content in orange-spotted grouper fed to satiation were investigated. The combined effect of temperature (T, degrees C) and body weight (W, g) on maximum food consumption (C-max, g/day) was described as: InCmax= -7.411+0.828 lnW+0.317T-0.004 7T(2), and the optimum feeding temperature was 33.9 degrees C. The combined effect of temperature and body weight on growth (G) was described as: InG= -4.461-0.208lnW+0.394T-0.006 3T(2). The optimum growth temperature was 31.4 degrees C, whereas overall growth rates were high at 25, 30 and 35 degrees C. Feed conversion efficiencies (FCE, %), increasing first and then decreasing with increasing temperature, averaged from 1.8 to 2.1 in terms of dry weight of food fish. The optimum temperature for FCE tended to be lower than that for growth or feeding. Dry matter content increased with both increasing water temperature (17, 25, 30 and 35 degrees C) and body weight, and the combined effect of temperature and body weight on dry matter content (DM, %) was described as: lnDM =3.232+0.01 4 lnW-0.004 4T+0.001 2TlnW.

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Photosynthetic activity during rehydration at four temperatures (5, 15, 25, 35 degrees C) was studied in a terrestrial, highly drought-tolerant cyanobacterium, Nostoc flagelliforme. At all the temperatures, the optimum quantum yield F-v/F-m increased rapidly within I It and then increased slowly during the process of rehydration. The increase in F-v/F-m at 25 and 35 degrees C was larger than that at 5 and 15 degrees C. In addition, the changes of initial intensity of fluorescence (F-0) and variable fluorescence (F-v) were more significant at 25 and 35 degrees C than those at 5 and 15 degrees C. Chlorophyll a content increased with the increase of temperature during the course of rehydration, with this being more pronounced at 25 and 35 degrees C. The photosynthetic rates at 25 and 35 degrees C were higher than those at 5 and 15 degrees C. Induction of chlorophyll fluorescence with sustained rewetting at 5 and 15 degrees C had two phases of transformation, whereas at 25 and 35 degrees C it had a third peak kinetic phase and showed typical chlorophyll fluorescence steps on rewetting for 24 h, representing a normal physiological state. A comparison of the chlorophyll fluorescence parameters, chlorophyll a content, and the chlorophyll fluorescence induction led to the conclusion that N. flagelliforme had a more rapid and complete recovery at 25 and 35 degrees C than that at 5 and 15 degrees C, although it could recover its photosynthetic activity at any of the four temperatures. (c) 2007 Published by Elsevier Ltd.

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Our studies investigated the physico-chemical properties of alkaline phosphatase excreted by D. magna. This cladoceran mainly released alkaline phosphatase, though it also released a small amount of acid phosphatase. The alkaline phosphatase showed a broad pH optimum (8.05-10.0), and had a broad optimum temperature (30-35 degrees C) with a temperature coefficient (Q(10)) of 2.45. The K-m of the enzyme is 0.15 +/- 0.02 mM when p-nitrophenyl phosphate is used as a substrate, and the V-max is 0.43 +/- 0.01 mu M pNP mg(-1) DW h(-1). Even though alkaline phosphatase had been incubated in chloroform saturated with WC medium for 13 days, its activity was 54% that of the original. The enzyme was strongly inactivated by EDTA, and appeared to be zinc dependent. The alkaline phosphatase activity remained constant when D. magna was fed different quantities of Chlorella sp. The sensitivity of D. magna phosphatase activity to phosphate was time-dependent. During the first 16 hrs, the enzyme was insensitive to phosphate addition, after 24 hrs incubation the enzyme became sensitive to phosphate addition.

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A new triplexing filter based on a silica direction coupler and an arrayed waveguide grating is presented. Using a combination of a direction coupler and an arrayed waveguide grating, a 1310-nm channel is multiplexed and 1490- and 1550-nm channels are demultiplexed for fiber-to-the-home. The direction coupler is used to coarsely separate the 1310-nm channel from the 1490- and 1550-nm channels. Subsequently, an arrayed waveguide grating is used to demultiplex the 1490- from 1550-nm channel. The simulated spectra show the 1-dB bandwidth of 110 nm for the 1310-nm channel and 20 and 20.5 nm for the 1490- and 1550-nm channels. The insertion loss is only 0.15 dB for 1310 nm and 5 dB for 1490 and 1550 nm. The crosstalk between the 1490- and 1550-nm channels was less than -35 dB. (C) 2009 Society of Photo-Optical Instrumentation Engineers. [DOI 10.1117/1.3065508]

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本研究通过一系列生物学手段系统阐述了结核分枝杆菌尼克酰胺酶/吡嗪酰胺酶(PncA酶)的生物化学特征,并鉴定了酶当中的关键氨基酸。结果表明体外表达的结核分枝杆菌PncA酶是一个分子量为22.4 KDa单体酶,其最适pH值和温度分别为6.6 ~ 7.4和35 ~ 45 °C电感耦合等离子原子发射光谱结果表明PncA酶是一种含有Mn2+和Fe2+的蛋白,二者的比率为1:1。通过运用高效液相色谱和耦联氨酶试验的方法对纯化的PncA酶进行了动力学分析,结果表明PncA酶拥有相同的吡嗪酰胺酶和尼克酰胺酶活性。通过定点突变得到了9个突变,圆二色谱数据证明突变并没有引起PncA酶的二级结构的改变。对这9个突变的酶活性和金属离子含量分析的结果表明,D8、K96和C138是PncA酶结合和催化底物的关键氨基酸残基,D49、H51、H57和H71是金属离子结合的关键氨基酸,而Y103和S104则有可能与底物的结合稳定有关。我们的结果也表明,尽管与Pyrococcus horikoshii PncA酶的序列同源性很高,但二者在对金属离子的结合方式上存在明显差异, 并有可能导致两者在催化机制上的差异, 值得进一步研究。 通过筛选抗吡嗪酰胺药物的临床分离结核分枝杆菌19株,并对其pncA基因序列进行测序分析。结果再一次表明结核分枝杆菌PncA酶的突变与吡嗪酰胺耐药性密切相关,检测的准确性为78.9 %,并发现了一个在16位的甘氨酸突变为丝氨酸的新突变。

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Using meteorological data and RS dynamic land-use observation data set, the potential land productivity that is limited by solar radiation and temperature is estimated and the impacts of recent LUCC processes on it are analyzed in this paper. The results show that the influence of LUCC processes on potential land productivity change has extensive and unbalanced characteristics. It generally reduces the productivity in South China and increases it in North China, and the overall effect is increasing the total productivity by 26.22 million tons. The farmland reclamation and original farmlands losses are the primary causes that led potential land productivity to change. The reclamation mostly distributed in arable-pasture and arable-forest transitional zones and oasises in northwestern China has made total productivity increase by 83.35 million tons, accounting for 3.50% of the overall output. The losses of original farmlands driven by built-up areas invading and occupying arable land are mostly distributed in the regions which have rapid economic development, e.g. Huang-Huai-Hai plain, Yangtze River delta, Zhujiang delta, central part of Gansu, southeast coastal region, southeast of Sichuan Basin and Urumqi-Shihezi. It has led the total productivity to decrease 57.13 million tons, which is 2.40% of the overall output.

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The stability constants and species distributions of complexes of two lanthanide ions, Eu (III) and Tb(III), with a macrocyclic ligand, 3,6, 9, 17 20, 23-hexaazo-29, 30-dihydroxy-13, 27-dimethyl-tricylco-[23,3,1,1(11,15)] triaconta-1 (28) 11,13,15 (30), 25 26-hexane (BDBPH), in 1: 1 and 2: 1 system, were determined potentiometrically in 50% ethanol solution, at 35.0 degrees C and I = 0.100 mol/L (KCl). The two metal ions could form deprotonated mono- or dinuclear complexes with BDBPH with high stability after the three protons of the ligand completely neutralized. At higher pH values, Eu(M) could not form hydroxo complexes with BDBPH, while Tb(III) could form hydroxo complexes in the types of M2L(OH) M2L(OH)(2) and M2L (OH)(2). The kinetic study on the hydrolysis reaction of his (4-nitrophenyl) phosphate (BNPP) catalyzed by Tb-BDBPH system (2:1) was carried out in aqueous solution (pH 7.0 similar to 10.0) at 35 degrees C with I = 0.1000 mol/L (KCl). The second-order rate constant k(BNPP) (2.3 x 10(-3) (mol/L)(-1)center dot s(-1)) was determined. The dinuclear monohydroxo species, L-Tb-2-OH, is kinetically active species.

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The isothermal crystallization and melting behavior of the poly(epsilon-caprolactone) (PCL)/poly(ethylene oxide)(PEO) diblock copolymer has been studied by WAXD, SAXS, and DSC methods. Only the PCL block is crystallizable; the PEO block of weight fraction 20% cannot crystallize, although its corresponding homopolymer has strong crystallizability. The long period, amorphous layer, and crystalline lamella of the PCL/PEO block copolymer all increase with the rise in the crystallization temperature, and the thickness of the amorphous layer is much larger than that of crystalline lamella due to the existence of the PEO block in the amorphous region. The isothermal crystallization of the PCL/PEO block copolymer is investigated by using the theory of Turnbull and Fischer. It is found that the amorphous PEO block has a great influence on the nucleation of PCL block crystallization, and the extent of this influence depends on crystallization conditions, especially temperature. The outstanding characteristics are the phenomenon of the double melting peaks in the melting process of the PCL/PEO block copolymer after isothermal crystallization at different temperatures and the transformation of melting peaks from double peaks to a single peak with variations in the crystallization condition. They are related mainly to the existence of the PEO block bonding chemically with the PCL block. In summing up results of investigations into the crystallization and melting behavior of the PCL/PEO block copolymer, it is interesting to notice that when the PCL/PEO block copolymer crystallizes at three different crystallization temperatures, i.e., below 0 degrees C, between 0 and 35 degrees C, and above 35 degrees C, the variation of peak melting temperature is similar to that of overall crystallization rates in the process of isothermal crystallization. The results can be elucidated by the effect of the PEO block on the crystallization of the PCL block, especially its nucleation. (C) 1996 John Wiley & Sons, Inc.