浙江天童土地利用方式对土壤有机碳矿化的影响

以浙江天童地区的栲树群落为参照,选择了木荷林、灌丛、马尾松林、杉木林、金钱松林、竹林、茶园和裸地等土地利用类型,测定了土壤有机碳含量,以及在25 ℃和60%饱和含水量条件下培养33 d的有机碳矿化速率.结果表明:土壤有机碳含量与矿化速率均以常绿阔叶林最高,针叶林、竹林和茶园次之,裸地最低;相反,土壤有机碳矿化释放的CO2-C比例以栲树林最低.可见,常绿阔叶林土壤的固碳能力高于其它类型,常绿阔叶林被改为其它类型后,土壤有机碳含量和矿化速率显著下降.     

武夷山不同海拔典型植被带土壤酶活性特征

在武夷山自然保护区不同海拔4个典型植被带(常绿阔叶林、针叶林、亚高山矮林以及高山草甸)采集土壤样品,分析了脲酶、蔗糖酶、酸性磷酸酶和过氧化氢酶4种主要土壤酶活性的变化.结果表明:除磷酸酶外,武夷山不同海拔植被带土壤酶活性没有显著的季节差异,磷酸酶活性秋季显著高于其他季节;不同海拔土壤酶活性差异显著,海拔与季节对土壤酶活性无交互影响;土壤酶活性随海拔升高总体上呈上升趋势,高海拔草甸的土壤酶活性显著高于低海拔林地土壤;土壤酶活性具有明显的垂直分层分布,土层越深酶活性越低;4个植被带土壤脲酶活性为1.28 ～3.87 mg·g-1·24h-1,高山草甸＞常绿阔叶林＞亚高山矮林＞针叶林;蔗糖酶活性为36.18 ～244.08 mg·g-1·24 h-1,高山草甸＞针叶林＞常绿阔叶林＞亚高山矮林;磷酸酶活性和过氧化氢酶活性分别为0.18～0.62 mg·g-1 ·2 h-1和1.78 ～1.98 ml·g-1·20 min-1,高山草甸＞针叶林＞亚高山矮林＞常绿阔叶林;土壤酶活性与土壤总有机碳、全氮显著正相关;与土壤温度、湿度、pH相关性比较复杂.     

常绿阔叶林与杉木林的土壤碳矿化潜力及其对土壤活性有机碳的影响

采用室内土壤培养法,比较分析了湖南省会同地区常绿阔叶林、杉木纯林土壤有机碳的矿化速率和累计矿化量,分析了有机碳矿化量与土壤活性有机碳初始含量的关系。结果表明:常绿阔叶林土壤有机碳矿化速率和累计矿化量均显著高于杉木纯林。在培养的第21天,在培养温度为9℃和28℃条件下,常绿阔叶林0～10和10～20cm土层的土壤有机碳累计矿化量为杉木纯林的1.7～2.7倍。常绿阔叶林土壤有机碳矿化释放的CO2-C分配比例高于杉木纯林。林地土壤有机碳矿化量受土壤微生物碳、可溶性有机碳初始含量的影响(P<0.01)。土壤有机碳矿化使土壤微生物碳增加而可溶性有机碳下降,但变化幅度均不大。温度从9℃升高到28℃后,林地土壤有机碳矿化速率提高3.1～4.5倍;2林地有机碳矿化对温度的敏感性无显著差异。     

武夷山不同海拔土壤呼吸及其主要调控因子

2005年4月-2006年3月,选择福建武夷山不同海拔高度上的常绿阔叶林、针叶林、亚高山矮林和高山草甸4个不同的群落作为实验地,每月测量1次土壤呼吸,测定影响土壤呼吸变化的土壤生物与非生物因子(包括土壤温度,土壤湿度,土壤有机碳、氮、硫含量,凋落物量,微生物量以及细根生物量等),研究了土壤呼吸的空间异质性.结果表明:随着海拔的升高,年均土壤呼吸速率显著降低,而土壤碳、氮、硫含量,土壤微生物量以及细根生物量等却增大;常绿阔叶林土壤呼吸速率是高山草甸的1.82倍;土壤呼吸的空间变化只与土壤温度呈显著的相关性;证明在影响土壤呼吸的土壤因子中,土壤温度是调控其在海拔高度上变化的主导因子.     

南亚热带森林植被恢复演替序列的土壤有机碳氮矿化

采用室内培养的方法,分析了南亚热带鼎湖山森林植被恢复演替序列不同阶段代表性森林—马尾松林、针阔叶混交林和季风常绿阔叶林土壤(0~10cm)CO2、CH4排放/吸收和有机氮矿化的差异.结果表明:3种森林土壤培养52周的CO2-C累积排放量分别为(30.66±3.36)、(58.17±7.25)和(59.31±13.58)mg·kg-1,而其中的65.12%、64.41%和64.12%均在前9周被排放;马尾松林土壤的CO2-C累积排放量一直显著小于针阔叶混交林和季风常绿阔叶林;用相符的二库动力学模型模拟的活性库和惰性库的碳矿化速率均呈递减趋势;土壤培养52周吸收CH4的累积量、培养20周有机氮净矿化量和净硝化量均为马尾松林<针阔叶混交林<季风常绿阔叶林(P<0.05),净矿化的有效氮以硝态氮为主.说明森林植被类型的变化改变了土壤有机碳的分解速率,这是其影响土壤有机碳含量的一种内在方式.     

武夷山不同海拔高度土壤活性有机碳变化

采用连续熏蒸 培养法，测定了福建武夷山自然保护区不同海拔高度具有代表性的中亚热带常绿阔叶林、针叶林、亚高山矮林以及高山草甸土壤中有效碳含量，分析了土壤有效碳（LOC）与微生物量碳（MBC）、土壤总有机碳（TOC）、细根生物量（FRB）和土壤全氮（TN）之间的关系.结果表明：土壤有效碳占总有机碳的3.40%～7.46%；微生物量碳只是土壤有效碳中的一部分,占土壤有效碳26.87%～80.38%； 不同林分土壤有效碳含量随海拔增高而显著增大，随土层深度的增加而降低；土壤有效碳与微生物量碳、土壤总有机碳、细根生物量、土壤全氮之间呈极显著的相关关系.高海拔土壤有效碳含量显著高于低海拔土壤.     

武夷山不同海拔高度土壤活性有机碳变化

采用连续熏蒸-培养法,测定了福建武夷山自然保护区不同海拔高度具有代表性的中亚热带常绿阔叶林、针叶林、亚高山矮林以及高山草甸土壤中有效碳含量,分析了土壤有效碳（LOC）与微生物量碳（MBC）、土壤总有机碳（TOC）、细根生物量（FRB）和土壤全氮（TN）之间的关系.结果表明：土壤有效碳占总有机碳的3.40%～7.46%;微生物量碳只是土壤有效碳中的一部分,占土壤有效碳26.87%～80.38%;不同林分土壤有效碳含量随海拔增高而显著增大,随土层深度的增加而降低;土壤有效碳与微生物量碳、土壤总有机碳、细根生物量、土壤全氮之间呈极显著的相关关系.高海拔土壤有效碳含量显著高于低海拔土壤.     

六盘山林区几种土地利用方式对土壤有机碳矿化影响的比较

 应用土壤培养法,比较分析了六盘山林区天然次生林（杂灌林、山杨（Populus davidanda）和辽东栎（Quercus liaotungensis）林）、农田、草地和人工林（13 a、18 a和25 a华北落叶松（Larix principis-rupprechtii））土壤在30℃和60%田间饱和含水量条件下培养180 d有机碳矿化速率的差异（以180 d累计释放的CO2-C计）。结果显示：农田和草地土壤碳矿化释放的CO2-C含量（180 d释放的gCO2-C·kg-1干土）分别比天然次生林低65%和23%,差异主要在0～40土层;人工林比农田和草地分别高155%和 17%,差异主要在0～70 cm土层。农田土壤碳矿化释放的CO2-C分配比例（即180 d释放CO2-C/土壤 C）比天然次生林平均低12%,草地比天然次生林平均高18%,差异主要在0～40 cm土层;人工林比农田平均高29%,草地比人工林平均高9%,差异主要在0～50 cm土层。不同土地利用方式土壤碳矿化释放的CO2-C含量的差异比其分配比例的差异大。土壤碳矿化释放的CO2-C含量和分配比例总体上都随土层加深而递减。分配比例随土层加深而递减的幅度方面,不同土地利用方式间的差异不大;含量随土层加深而递减的幅度方面,天然次生林和人工林比农田和草地中大;随土层递减的幅度方面,土壤碳矿化释放的CO2-C含量比其分配比例大。这主要由不同土地利用方式土壤碳输入和稳定性等差异所致。结果说明土壤碳矿化速率随天然次生林变成农田或草地而下降,随在农田或草地上造林而增加, 矿化速率变化幅度比分配比例的变化幅度大。另外,土地利用变化也使不同土层土壤碳矿化速率和分配比例差异改变,其中速率改变的幅度比分配比例改变的幅度大。     

贡嘎山树线过渡带土壤有机碳矿化和温度敏感性

树线过渡带作为高山地区重要的生态过渡带之一,是响应温度变化的敏感区域。树线过渡带内土壤碳储量丰富,其碳周转在全球碳循环方面扮演着重要角色。探究树线过渡带土壤有机碳矿化及其温度敏感性,对于预测气候变化背景下高山地区土壤碳循环过程具有重要的指导意义。为此以青藏高原东南部贡嘎山树线过渡带(森林、树线、灌丛)的土壤为对象,在室内开展90 d不同温度(15℃和20℃)的培养实验,测定土壤有机碳矿化速率,计算单位土壤有机碳累积矿化量、温度敏感性,并分析影响它们的相关因素。结果表明：土壤有机碳矿化速率受温度和样地类型的显著影响。升温显著增加土壤有机碳矿化速率,而不同样地类型间矿化速率差异显著,矿化速率大小表现为森林>树线>灌丛。本研究用单位土壤有机碳累积矿化量表征土壤有机碳的稳定性,经90 d的培养,15℃下树线过渡带从森林、树线到灌丛单位土壤有机碳累积矿化量分别为12.33 mg/g、12.99 mg/g和10.53 mg/g, 20℃下则分别为19.16 mg/g、21.14 mg/g和16.26 mg/g,灌丛土壤单位土壤有机碳累积矿化量显著低于森林和树线土壤,这表明灌丛土壤具备更...     

武夷山不同海拔梯度土壤微生物生物量微生物呼吸及其商值(qMB,qCO2)

土壤微生物生物量、土壤微生物呼吸及微生物商值(微生物商(qMB)、微生物呼吸商(qCO2))是土壤质量的敏感性指标.本文对武夷山不同海拔梯度具有代表性的中亚热带常绿阔叶林、针叶林、亚高山矮林以及高山草甸土壤微生物生物量、土壤微生物呼吸及其qMB、qCO2进行了研究.结果表明:土壤微生物生物量、土壤微生物呼吸均随海拔梯度的升高而加大,随土层深度的加深而降低,qMB、qCO2没有表现出随海拔变化的规律,qMB的最大值(2.23%±0.28%)出现在高山草甸0～10 cm土层的土壤,最小值(0.51%±0.09%)为常绿阔叶林25～40 cm土层土壤,针叶林的值大于亚高山矮林;qCO2的最大值(5.88%±0.94%)为针叶林25～40 cm土层土壤,最小值(1.38%±0.09%)为高山草甸0-10 cm土层的土壤.在同一林分,qMB值随土层加深而减小,qCO2值在亚高山矮林和高山草甸无此规律.土壤微生物生物量、微生物呼吸及其qMB、qCO2与土壤总有机碳、全氮、全磷具有显著的线性相关关系(P<0.05),可用来评价土壤质量.     

In memoriam: Francisc Schneider (1933‐2017)

This is the obituary for Francisc Schneider, who introduced clinical physiology in Romania and mentored generations of scientists.     

Responses of Nitraria tangutorum to water and photosynthetic physiology in rain enrichment scenario

Under the global warming conditions, great attention has been paid to the effects of precipitation on ecophysiological characteristics in desert plants. Nitraria tangutorum is one of the dominant shrubs distributes in desert outside Minqin oasis, Gansu Province. The artificial simulated rainfall experiments were carried out in four consecutive years from 2008 to 2011, in an attempt to understand the mechanisms of the photosynthetic response in desert plant to the variation of future precipitation pattern. The water and photosynthetic physiological characteristics of leaves in N. tangutorum were examined from July 24 to 26 in 2011 under different simulated rainfall increase gradients (increased 0%, 25%, 50%, 75% and 100% of mean annual precipitation, respectively). We measured leaf traits that could reflect both leaf water status (e.g., leaf water content and leaf water potential) and photosynthetic physiology (e.g., maximum net photosynthetic rate). The results showed that leaf water content and leaf water potential of N. tangutorum increased with increasing rainfall. Leaf water content and leaf water potential of N. tangutorum in the 100% increased rainfall treatment were significantly greater by 8.51% and 12.07% than the control (0% increased rainfall treatment). But leaf dry matter content and specific leaf weight gradually decreased with increasing rainfall. Leaf dry matter content and specific leaf weight in the 100% increased rainfall treatment were significantly lower by 6.92% and 25.93% than the control. Leaf maximum net photosynthetic rate (A_max), apparent quantum yield (AQY) and light saturation point (LSP) increased with increasing rainfall, while light compensation point (LCP) gradually decreased with increasing rainfall. AQY in the 100% increased rainfall treatment was significantly greater by 70.00% than the control. However, there were no significant differences in LSP and LCP between different treatments. A_max, transpiration rate (T_r), stomatal conductance (G_s) in the 100% increased rainfall treatment were significantly greater by 81.91%, 166.07% and 110.47% than the control, respectively. On the contrary, water use efficiency (WUE) in the 100% increased rainfall treatment was significantly less 48.28% than the control. There were no significant differences in intercellular CO₂ concentration (C_i) and stomatal limitation value (L_s) between different treatments. The correlation analysis showed that there were significantly positive correlations between leaf water content, leaf water potential, T_r and G_s. However, there were significantly negative correlations between leaf dry matter content, leaf specific mass and T_r, G_s, leaf water content and leaf water potential, suggesting that leaf gas exchanges were regulated by leaf water status. Therefore, N. tangutorum could adapt to the tendency of future increasing precipitation by the coordination of water physiology and photosynthesis.     

不同生态稻区覆膜旱作稻氮营养生理及抗逆生理特性探讨

不同生态稻区生态环境和栽培管理方式不同,覆膜旱作稻氮营养生理和抗逆生理与常规水作稻有些异同,尤其是体内NO₃^--N和NH₄⁺-N含量及分布差异很大.杭嘉湖平原区覆膜旱作稻生长前期受干热天气影响,其分蘖期、拔节期、孕穗期体内NO₃^--N含量较水作稻有不同程度的降低,而NH₄⁺-N含量则极显著提高;金衢盆地覆膜旱作稻孕穗期体内NO₃^--N含量比常规水作稻高,根部NH₄⁺-N含量则显著降低,茎基部和叶片NH₄⁺-N含量有一定增加.正常气候条件下两生态稻区覆膜旱作稻孕穗期叶片硝酸还原酶(NR)活性和谷氨酰胺合成酶(GS)活性较水作稻均有不同程度的提高;丙二醛(MDA)、可溶性糖及脯氨酸(Pro)含量与水作稻相差不大,表明不同生态稻区的覆膜旱作稻可以通过不同的栽培管理模式,促进生长发育,达到高产目的.     

木麻黄逆境生理研究进展(综述)

本文综述水分、盐分、重金属和酸雨等逆境条件对木麻黄生长发育及生理生化等方面的影响,指出木麻黄造林的主要逆境因素是水分和盐分,并对今后的研究工作提出建议。     

试析世纪之交植物生理学研究的动向

简要介绍了当今植物生理学研究中值得注意的四个动向,它们是从研究生物大分子到阐明复杂生命活动——基因组学、基因结构与功能的研究;实现生命整体性的重要环节——信号传递的研究;生命活动的能量和物质基础——代谢及其调节的研究;植物与环境(非生物和生物环境)的相互关系——生物的协同进化和适应的研究。     

杨桃果实采后生理研究(综述)

概述了国内外对杨桃果实采后主要营养成分的分析、呼吸、乙烯释放、主要生理病害,并介绍了不同贮藏条件或处理对杨桃果实采后贮藏性影响的研究概况。     

柽柳的水分生理特性研究进展

研究和了解柽柳的水分生理特性,是对柽柳合理利用和科学管理的重要前提。在对柽柳水分生理特性多年综合研究（P－V曲线、清晨水势及水势日变化和蒸腾速率）的基础上,对国内外研究柽柳水分生理特性的一些方法和手段进行了评述,以期尽快掌握柽柳的生态特性,为干旱、半干旱区域柽柳的恢复和保护提供一定的理论依据。     

Physiological and biochemical energetics of larvae of Teredo navalis L. and Bankia gouldi (Bartsch) (Bivalvia : Teredinidae)

The biochemical composition of larvae of Teredo navalis L. and Bankia gouldi (Bartsch) (Bivalvia: Teredinidae) was examined throughout larval development at 23°C and 30–32%. salinity in the presence of the phytoplankton food Isochrysis aff. galbana (clone T-ISO), during a delay of metamorphosis in the presence of food but absence of a wood substratum and during periods of enforced starvation. Newly released Teredo navalis larvae had a mean length (L) and height (H) of 89.3 and 76.1 μm respectively. The first appearance of pediveliger larvae at 212.1 μm L and 230.0 μm H occurred 27 days after release. Larval dry weight increased from 0.29 μg to 1.96 μg during this period. Newly formed straight hinge larvae of Bankiagouldi had dimensions of 62.8 μm L and 49.8 μm H. Metamorphically competent B. gouldi larvae had dimensions of 230.0 μm L and 282.9 μm H and were first observed 20 days after fertilization. Larval dry weight increased from 0.06 μg to 2.20 μg during this period. During enforced delay of metamorphosis the ash-free dry weight of Teredo navalis larvae decreased whereas the ash free dry weight of Bankia gouldi larvae increased. During the early period of shelled larval development both species showed similar decreases in lipid, protein and carbohydrate levels (μg·mg dry weight^?1); however, this was reflected in a decrease in biochemical content (μg·larva^?1) only in Teredo navalis. During enforced starvation the major proportion of both the weight and caloric losses were due to protein. Lipid also contributes significantly to these losses whereas the contribution of carbohydrate was small. Larval oxygen consumption rates were determined directly by manometry and indirectly by estimates of decrease in caloric content during periods of enforced starvation. Direct and indirect determinations for T. navalis are described by the relationships R = 1.16 W^1.05 and R = 0.98 W^1.24 respectively where R is the respiration rate in nl O₂ · larva^?1 · h^?1 and W is dry weight inclusive of shell in μg. Direct and indirect determinations for Bankia gouldi are described by the relationships R = 1.37 W^1.25 and R = 1.81 W^1.25 respectively. When data for both assay procedures are combined for each species the relationships R = 1.10 W^1.07 and R = 1.44 W^1.18 are obtained for Teredonavalis and Bankia gouldi respectively.     

黄鳝血液生理参数的研究

报道了健康黄鳝血液的几项生理参数。结果 ,红细胞 2 .37× 10 12 L ,白细胞 4.16× 10 9L ,血栓球 6 1.6× 10 9L ,血红蛋白 134 .5 gL ,红细胞最大脆性 0 .35 % (NaCL溶液 ) ,血沉 1.0 5mmh ,凝血时间 1.75min。并将黄鳝的血液生理参数与其它几种鱼类作了对比分析