模拟N沉降对太岳山油松人工林和天然林草本群落的影响

由于人类活动氮沉降呈逐年增加的趋势,进而增加了陆地生态系统氮的输入,从而影响陆地生态系统多样性、物种组成和功能。为揭示氮沉降增加对油松林草本群落的影响,于2009年7月在太岳山油松人工林和天然林,设计4个施氮水平:对照(CK,0 kg N hm-2a-1),低氮(LN,50 kg N hm-2a-1),中氮(MN,100 kg N hm-2a-1)和高氮(HN,150 kg N hm-2a-1),研究草本群落的生物多样性、生物量以及草本元素含量对模拟N沉降的响应。研究结果表明:模拟N沉降未能显著影响人工林草本群落的生物多样性(P0.05),而中氮、高氮显著降低了天然林草本群落的生物多样性(P0.05);从Jaccard指数和Sorensen指数分析得出人工林不同氮水平之间草本群落差异性较小,而天然林不同氮水平之间草本群落差异性较大。模拟N沉降没有显著改变人工林草本群落生物量(P0.05),而高氮明显促进天然林草本群落生物量的增加(P0.05)。与对照相比,模拟N沉降提高了人工林和天然林羊胡子苔草叶根中的全N含量(P0.05),而降低了全Mg的含量(P0.05),并且根部元素含量变化与土壤养分含量变化较为一致。施氮提高了N/K、N/Ca、N/Mg(P0.05)的比值。说明油松林下草本群落对氮沉降的响应因林分土壤N饱和程度以及林地利用历史的不同而产生差异,其中天然林响应最为敏感。     

长白山森林生态系统大气氮素湿沉降通量和组成的季节变化特征

2009—2010年期间,利用雨量计收集法在长白山森林生态系统定位站开展定位观测,分析降水中氮素浓度,研究了该区域大气氮素湿沉降通量和组成的季节变化特征。结果表明,各形态氮素月均浓度之间差别较大,具有明显的季节性;其降水中浓度主要受降水量和降水频次的影响。全年氮素湿沉降中TN、TIN和TON的沉降量分别为27.64 kg N hm-2a-1、11.05 kg N hm-2a-1和16.59 kg N hm-2a-1,TON为沉降主体,占60.02%;其大气氮沉降量主要由降水量和降水中氮素浓度共同决定。该地区氮湿沉降量已处于我国中等水平,考虑到氮素的干湿沉降比例,本区域的年氮沉降量已接近或超过本区域的营养氮沉降临界负荷,存在一定的环境风险。该地区生长季(5—10月)的氮沉降量(16.59 kg N hm-2a-1)占全年氮沉降量的比例达到73.20%。生长季的氮沉降对于促进植物生长直接生态意义重大,而非生长季的氮沉降对于大量补充次年植物生长初期所需养分的间接生态意义明显。     

模拟氮沉降对杨树人工林土壤微生物群落结构的影响

在杨树人工林中,采用随机区组设计、野外定位模拟氮沉降试验,研究氮沉降对土壤微生物群落结构的影响。设计5个氮沉降水平,分别为:空白对照N0(0 kg·hm-2·a-1)、低氮N1(50 kg·hm-2·a-1)、中氮N2(100 kg·hm-2·a-1)、高氮N3(150 kg·hm-2·a-1)、超高氮N4(300 kg·hm-2·a-1)。从2012年5月开始在生长季(5—10月)每月进行施氮处理。施氮2年后,运用磷脂脂肪酸(PLFA)方法对0~10 cm土层中的微生物群落结构进行了测定。结果表明,施氮处理未改变微生物PLFAs总量水平,但使细菌和革兰氏阳性细菌PLFAs含量上升;中氮处理使真菌PLFAs含量显著下降,其他水平的氮处理对其影响则不显著;中氮、高氮和超高氮处理使丛枝菌根真菌和原生动物的PLFAs含量减少。除低氮处理外,其他施氮处理样地中的土壤微生物结构都发生了改变。这些结果表明,短期氮沉降会影响杨树人工林土壤微生物群落结构,并最终可能对生态系统功能产生影响。     

模拟氮沉降条件下木荷幼苗光合特性、生物量与C、N、P分配格局

设置模拟氮沉降的控制试验,以NH4NO3作为外加氮源,设计CK(0kg N hm-2·a-1)、LN(50 kg N hm-2·a-1)、MN(100 kg N hm-2·a-1)、HN(150 kg N hm-2· a-1)4个处理,历时9个月,测定木荷(Schima superba)幼苗的光合特性、生物量和C、N、P含量及其分配格局对氮沉降的响应.结果表明:(1)木荷幼苗的最大净光合速率和光饱和点随着氮处理水平增加呈先增加后减小的特点,在中氮处理下极显著增加(P＜0.01).氮处理降低了幼苗的光补偿点和暗呼吸速率,光补偿点在低氮处理下显著降低(P＜0.05),暗呼吸速率在低中氮处理下极显著降低(P＜0.01),高氮处理下显著降低(P＜0.05).未见氮处理对表观量子效率产生显著影响.(2)氮处理促进了木荷的全株生物量以及各部分生物量的增长.随着氮处理水平的增加,叶重比呈升高的趋势,而根重比和根冠比呈降低的趋势,在高氮处理下叶重比的增加和根重比、根冠比的降低都达到了显著水平(P＜0.05).(3)氮沉降促进各器官N含量的增加,在高氮处理下根和茎中N含量极显著增加(P＜0.01),叶中N含量显著增加(P＜0.05).而各器官C含量随着氮沉降程度的增加呈先增加后降低的趋势,在中氮处理下根和茎中C含量极显著增加(P＜0.01),叶中C含量显著增加(P＜0.05).但各器官P含量变化趋势各不相同,随着氮的增加,根中P含量是呈先增加后降低的趋势,而茎和叶中P含量是呈降低的趋势.氮沉降一定程度上降低了木荷各器官的C/N比值而增加了N/P比值.     

氮磷添加对内蒙古温带典型草原土壤微生物群落结构的影响

选取内蒙古温带典型草原,进行连续6a氮磷添加试验,采用土壤特征微生物PLFA生物标记技术,研究6个氮添加水平N0(0 kg N hm-2a-1)、N1(56 kg N hm-2a-1)、N2(112 kg N hm-2a-1)、N3(224 kg N hm-2a-1)、N4(392 kg N hm-2a-1)、N5(560 kg N hm-2a-1)和6个磷添加水平P0(0 kg P hm-2a-1)、P1(15.5 kg P hm-2a-1)、P2(31 kg P hm-2a-1)、P3(62 kg P hm-2a-1)、P4(93 kg P hm-2a-1)、P5(124 kg P hm-2a-1)对土壤特征微生物PLFA生物标记数量和土壤微生物群落结构的影响。结果表明:(1)随氮添加量增加,土壤微生物总磷脂脂肪酸(PLFA)含量和土壤细菌PLFA生物标记数量、放线菌PLFA生物标记数量呈上升趋势,土壤G+/G-呈增加趋势;各氮添加水平对土壤真菌PLFA生物标记数量无显著差异,随氮添加量增加,土壤真菌/细菌比降低。(2)随磷添加量增加,土壤总磷脂脂肪酸(PLFA)含量、土壤细菌PLFA生物标记数量、放线菌PLFA生物标记数量、真菌PLFA生物标记数量及真菌/细菌比值呈先上升后下降趋势,均以P3水平(62 kg P hm-2a-1)处理最高,说明适宜的磷添加对内蒙古温带典型草原土壤微生物繁殖和菌落结构有显著影响。     

氮添加与降雨变化对红砂幼苗非结构性碳水化合物的影响

非结构性碳水化合物(NSC)在植物体内的含量及分配对植物生长和存活至关重要。开展氮沉降和降雨变化对幼苗NSC影响的研究,为揭示干旱导致幼苗死亡机理及预测气候变化背景下幼苗自然更新及培育提供依据。本研究以1年生红砂幼苗为对象,测定了不同降雨(降雨减少(W-)、自然降水(W)和降雨增多(W+))和氮添加(N0(0 g N·m^-2·a^-1)、N1(4.6 g N·m^-2·a^-1)、N2(9.2 g N·m^-2·a^-1)、N3(13.8 g N·m^-2·a^-1))条件下红砂幼苗各器官NSC及其组分含量。结果表明:红砂幼苗各器官NSC含量为28.8~71.8mg·g-1,叶片含量最高,茎含量最低。氮添加和降雨变化对红砂幼苗叶片和根系淀粉及总NSC含量有显著影响,而对茎无显著影响。各降雨条件下,氮添加均促进了红砂幼苗叶片淀粉和总NSC累积,在降雨增加30%的条件下氮的促进效应更显著,中高氮(N2和N3)叶片淀粉与总NSC含量显著高于低氮水平(N1和N0);在低氮降雨减少30%(N1W-)处理下,红砂叶片淀粉和NSC含量最小,而根系淀粉和NSC含量最大,即低氮干旱胁迫下红砂可通过NSC在不同器官的重新分配来适应胁迫环境。在自然降雨和降雨增加30%情况下,根系淀粉和NSC的含量随氮添加的增加而减小,且中高氮处理(N2和N3)显著低于对照(N0)。可见,叶片是红砂NSC的源,氮添加会促进红砂幼苗叶片NSC的累积,且这种促进效应与水分紧密相关,在降水增加情况下其效应更显著;而过量的氮添加会抑制根系NSC含量的积累,在低氮干旱胁迫下红砂也可通过叶片NSC向根系转移来适应逆境胁迫。     

模拟氮沉降对长白山岳桦林下草本植物和土壤肥力的短期影响

选取长白山岳桦林中的岳桦-蟹甲草群落(Comm. Betula ermanii-Parasenecio forrestii)、岳桦-藜芦群落(Comm. Betula ermanii-Veratrum nigrum)和岳桦-小叶章群落(Comm. Betula ermanii-Deyeuxia purpurea)开展野外模拟氮沉降实验,采用野外原位模拟实验方法,设置对照(0 kg·hm-2·a-1)、低氮(30 kg·hm-2·a-1)、中氮(50 kg·hm-2·a-1)和高氮(100 kg·hm-2·a-1)4个氮处理水平,测定草本植物生长状况和土壤肥力,研究岳桦林下草本层植物和土壤肥力对氮沉降的短期响应。结果显示:(1)岳桦林下草本植物随氮沉降量的增加而加速生长,小叶章对氮沉降的响应较为敏感,藜芦次之,蟹甲草最弱;(2)氮添加造成林下土壤肥力发生变化,有机质含量下降,特别是岳桦-小叶章群落下的土壤有机质含量下降最明显;土壤总氮和速效氮含量增大,岳桦-蟹甲草群落下的土壤总氮和速效氮增加最多;土壤总磷和速效磷含量减小,岳桦-小叶章群落下的土壤总磷和速效磷含量的减少最多。本研究结果表明氮添加在短期内会促进长白山岳桦林下草本植物生长,尤其是小叶章的生长,加快土壤有机质的分解和磷的释放,逐步改变土壤肥力并反馈给植物,促使其进一步变化。     

模拟氮沉降对鼎湖山森林土壤酸性磷酸单酯酶活性和有效磷含量的影响

采用野外原位试验模拟氮(N)沉降,研究了其对鼎湖山马尾松林、混交林和季风林3种森林类型土壤酸性磷酸单酯酶活性(APA)和有效磷(AP)含量的影响.在季风林中设置对照(0 kg N·hm-2·a-1)、低N(50 kg N·hm-2·a-1)、中N(100 kg N·hm-2·a-1)和高N(150 kg N·hm-2·a-1)处理,在马尾松林和混交林中只设置对照、低N和中N处理.结果表明:随着土层加深,土壤APA和AP含量降低.土壤APA在季风林中最高,而AP含量在3种林型中没有显著差异.N沉降增加对土壤APA的作用与林型有关.季风林中适度N沉降可使APA升高,且低N处理的APA(19.52 μmol·g-1·h-1)最高;马尾松林和混交林中,中N处理的APA最高,分别为12.74和11.02 μmol·g-1·h-1.3种林型的AP含量均在低N处理下最高,但各N处理之间的差异并不显著.土壤APA与AP含量之间呈显著正相关关系.     

模拟氮沉降对太岳山油松林土壤酶活性的影响

为研究土壤酶活性对氮沉降增加的响应,以山西太岳山油松人工林和天然林为研究对象,于2009年8月开始实施模拟氮沉实验,试验设置对照(CK,0 kg N hm-2a-1);低氮(LN,50 kg N hm-2a-1);中氮(MN,100 kg N hm-2a-1);高氮(HN,150 kg N hm-2a-1)4种氮处理,自2012年起每年5、7、9月在各处理样方采集表层0—20 cm土壤,测定土壤酶活性(过氧化物酶、多酚氧化酶、纤维素酶、蔗糖酶、脲酶、中性磷酸酶)。研究结果表明:施氮处理下的脲酶与中性磷酸酶活性均有所提高,而低氮处理下天然林中的多酚氧化酶与人工林中的蔗糖酶显著低于对照,中氮、高氮处理下过氧化物酶、多酚氧化酶、天然林中的纤维素酶以及人工林中的蔗糖酶显著降低。总的来说,人工模拟氮沉降促进了土壤中脲酶和中性磷酸酶的活性,抑制了过氧化物酶和多酚氧化酶的活性,并降低了天然林土壤中的纤维素酶活性和人工林中的蔗糖酶活性,但对天然林中蔗糖酶和人工林中的纤维素酶无影响。主导木质素降解的多酚氧化酶活性与纤维素酶、蔗糖酶活性显著相关,纤维素酶与蔗糖酶活性的下降可能是由木质素降解受到抑制,土壤微生物可利用碳源减少所引起。另外,受到天然林土壤含氮量较高的影响,与人工林相比,天然林的多酚氧化酶活性对模拟氮沉降更敏感。由于被抑制的酶均与土壤有机质降解密切相关,氮沉降增加将减缓山西油松林土壤有机质的降解,有利于有机质在土壤中的积累。     

模拟氮沉降下去除凋落物对太岳山油松林土壤呼吸的影响

凋落物是土壤呼吸的重要碳源,氮沉降将改变其输入数量和质量,进而影响土壤呼吸。为揭示氮沉降和去除凋落物对土壤呼吸的影响,以太岳山油松林为研究对象,对林地分别作2种凋落物处理:去除凋落物(LR)、对照(CK1),设计4个施氮水平:不施氮(CK2,0 kg N·hm-2·a-1),低氮(LN,50 kg N·hm-2·a-1),中氮(MN,100 kg N·hm-2·a-1)和高氮(HN,150 kg N·hm-2·a-1),于2010—2012年生长季测定土壤呼吸速率的动态变化,并分析土壤呼吸速率与土壤温度、土壤湿度、土壤微生物生物量C、N的关系。结果表明:随着观测年限的推移,模拟氮沉降对对照处理的土壤呼吸速率、去凋处理的土壤呼吸速率、凋落物层呼吸速率的促进作用逐渐减弱。去除凋落物使土壤呼吸速率降低了29.0%,施氮减小了去除凋落物后土壤呼吸速率的变化幅度。土壤呼吸速率与土壤温度均呈显著指数相关(P0.05),土壤温度解释了土壤呼吸速率变异的37.3%~62.2%,去除凋落物降低了模型决定系数R2;以土壤温度和土壤水分构建的复合关系方程拟合效果均好于单因子模型,土壤温度和水分共同解释了土壤呼吸季节变化的67.6%~85.6%,并且施氮降低了去凋处理的复合模型决定系数R2,而对对照处理没有显著影响。施氮提高了土壤微生物生物量C、N,并且土壤微生物生物量C、N与土壤呼吸速率呈显著正相关(P0.05)。说明氮沉降、凋落物是影响油松林土壤CO2通量的两个重要因子。     

Symbiotic nitrogen fixation in eight Acacia senegal provenances in dryland clays of the Blue Nile Sudan estimated by the 15N natural abundance method

The symbiotic biological N₂fixation by Acacia senegal was estimated using the ¹⁵N natural abundance (δ ¹⁵N) procedure on eight provenances collected from different environments and soil types grown in a clay soil in the Blue Nile region, Sudan. Balanites aegyptiaca (a non-legume) was used as a non-N₂-fixing reference plant to allow ¹⁵N-based estimates of the proportion of the Acacia N derived from atmospheric N₂ (N_dfa) to be calculated. Results show variation in leaf δ ¹⁵N between A. senegal and the reference plant and among years. The relative δ ¹⁵N values (‰) were higher in B. aegyptiaca than in the N₂-fixing acacia provenances. Provenances originally collected from clay soils fixed little N in the first year, but the amount fixed increased as the trees aged. All provenances showed a decrease in δ ¹⁵N with age. The N_dfa varied between 24% (Mazmoom provenance) and 61% (Rahad provenance) 4 years after planting. There was no significant difference in δ ¹⁵N between provenance groups based on soil type or rainfall at original growing site. The amount of N_dfa increased significantly with age in all provenances. The above-ground contribution of fixed N to foliage growth in a 4-year-old A. senegal was highest in the Rahad sand–soil provenance (46.7 kg N ha⁻¹) and lowest in the Mazmoom clay-soil provenance (28.7 kg N ha⁻¹). Our study represents the first use of the δ ¹⁵N method for estimating the N input by A. senegal to the clay plain soils of the gum belt in the Sudan.     

不同种源五角枫幼苗叶片N、P化学计量学特征对氮添加的响应

不同土壤氮环境下植物对氮沉降的响应趋势不同,因此研究不同种源地的五角枫(Acer mono)对氮沉降的响应机理具有重要的意义。为了深入了解不同种源五角枫对氮沉降的适应和响应机制,主要通过3个种源的五角枫幼苗氮添加控制实验,分析不同种源的五角枫幼苗比叶面积(SLA)和叶片干物质含量(LMDC)以及叶片N、P含量和N∶P对氮添加的响应规律。结果表明:(1)不同氮添加处理下,内蒙古种源五角枫幼苗(NW)和山西种源五角枫幼苗(SW)的LDMC均显著低于对照,NW和SW在N4条件下表现为显著的促进作用。随着氮添加浓度的增加,NW与北京种源的五角枫幼苗(BW)的SLA在N4条件下显著增加;SW的SLA在N2的水平下显著增加。(2)氮添加下,只有SW的P_(mass)在N1水平下显著增加,N_(mass)在N1和N3水平下表现为显著增加。说明在低氮水平下,能够促进SW对P的吸收,从而增加植物体内对P的积累。同时在低氮和中高氮条件下,能够促进SW对N的吸收,说明SW能较好的适应低氮和高氮环境,使其生存能力更强。(3)分析变异来源及各指标的相关性得出,氮添加条件下,五角枫的SLA、LDMC、P_(area)及N∶P与氮添加处理呈显著的相关关系,而SLA、LDMC、N_(mass)、P_(mass)、Narea、P_(area)和N∶P对氮添加处理和种源的交互作用均未表现出相关关系,说明引起五角枫各性状主要受氮添加处理影响。(4)综合各指标的变化,氮添加条件下,NW的LDMC显著降低,SLA显著增大,同时叶N含量、叶P含量以及N∶P比较高;SW的LDMC显著降低,SLA增大,同时叶N含量、叶P含量表现为显著增大,结合叶经济谱理论分析得出,SW和NW属于"快速投资-收益"型,而BW倾向于"缓慢投资-收益"型。因此,不同种源的五角枫对于氮沉降的响应存在差异,并且持续的氮添加已经改变了五角枫的适应性。     

Influences of nitrogen load on the growth and photosynthetic responses of <Emphasis Type="Italic">Quercus serrata</Emphasis> seedlings to O<Subscript>3</Subscript>

The objectives of this study were to clarify the influences of nitrogen (N) load on the growth and photosynthetic responses of Quercus serrata seedlings to O₃ and to obtain basic data for evaluating the critical levels of O₃ for protecting Q. serrata forests in Japan. The effects of O₃ and/or N load on growth and photosynthetic activity of Q. serrata seedlings were investigated during the two growing seasons. Two-year-old seedlings were assigned to 12 experimental treatments, which were comprised of the combination of four gas treatments (charcoal-filtered air and three levels of O₃ at 1.0, 1.5 and 2.0 times ambient concentration) and three N treatments (0, 20 and 50 kg ha⁻¹ year⁻¹). During the second growing season, no significant interactive effects of O₃ and N load on the growth and net photosynthetic rate of the seedlings were detected. Threrfore, we concluded that N supply to the soil at ≤50 kg ha⁻¹ year⁻¹ does not significantly influence the growth and photosynthetic responses of Q. serrata seedlings to O₃. Based on the O₃ exposure-response relationships for the whole-plant growth of the seedlings, the critical level of O₃ for Q. serrata was estimated to be approximately 36 nmol mol⁻¹ as the average 15-h O₃ concentration during the one growing season.     

Photosynthetic temperature responses of four neem (Azadirachta indica A. Juss) provenances in the dry-hot valley area of China

The temperature dependences of net photosynthetic rate (P _N), stomatal conductance (g _s), transpiration rate (E) and dark respiration (R _D) of four neem (Azadirachta indica A. Juss) provenances of 11 years old were measured in three seasons of 2006 in the dry-hot valley area of southwest China under field conditions. The results indicated that P _N of four neem provenances showed clear parabolic responses with the increase of temperature. The optimum temperature of P _N was around 25°C in initiation stage and 30°C in prosperous stage except for neem originating from Jodhpur (MA) provenance which was very close to the mean daily temperature of the preceding week while it was around 27°C (MA provenance excepted) in last stage which was rather close to the mean daily maximum temperature of the preceding week. The optimum temperature for P _N of MA provenance was about 2–4°C higher than that of the other three neem provenances in prosperous stage and last stage. According to the fitted parameters of photosynthetic temperature response curves, the photosynthetic performance in prosperous stage was more sensitive to temperature changes than that in initiation stage and last stage while the photosynthetic performance of neem originating from MA provenance was less sensitive to temperatures than that of neem originating from Kalyani, New Delhi and Kulapachta provenances in each growing stage. Furthermore, the temperature ranges for P _N of MA provenance were much wider than those of the remaining provenances in each growing stage. These differences in photosynthetic temperature acclimation between neem provenances not only reflected temperature regime of native habitats of these provenances but suggested that MA provenance could be more tolerant to extreme temperatures compared with the remaining provenances. The temperature response curves of g _s and E were generally similar in form in the same growing stage for all neem provenances; however, shape of the response curves in initiation stage and last stage was similar to parabolic curve while that in prosperous stage was similar to linear relation. The temperature for maximum g _s and E in initiation stage was close to the optimum temperature of P _N, but the maximum g _s reached at much lower temperature than P _N and E in last stage. The response of R _D to temperature increased exponentially with temperature; however, there were obvious differences in different growing stages. R _D in initiation stage was markedly higher than that in prosperous stage and last stage at a given temperature for four neem provenances. These results suggested that four neem provenances can acclimate to their growing environment through changed photosynthetic ecophysiological responses in course of subjecting to seasonal variation of temperature.     

不同种源花榈木苗期生长及生理特性比较

为了解不同种源花榈木在贵阳的生长特性和差异,该文通过对10个种源地花榈木进行育苗试验,测定其两年生实生苗的苗高、地径、生物量、叶片光合参数、光合色素、硝酸还原酶活性、硝态氮含量和根系活力,并进行差异性分析。结果表明:(1)10个种源花榈木净光合速率、气孔导度、胞间CO₂浓度、蒸腾速率和水分利用效率差异显著(P<0.05),表明不同种源花榈木光合特性及光能利用效率具有较大差异,浙江杭州和浙江永康花榈木是具有较高光合生长潜力的种源。(2)种源间的叶绿素含量、硝酸还原酶、硝态氮、根系活力存在显著差异,福建建瓯种源的叶绿素a、叶绿素b含量和叶绿素总量最高,能够将光合原初反应过程中积蓄的光能进行高效地传递,促进碳的同化; 贵州花溪种源硝酸还原酶活性最大,硝态氮含量最高,对氮元素的利用能力较强,能够促进植物蛋白质、氨基酸和叶绿素等的合成; 贵州望谟种源根系活力最大,吸收养分的能力强。(3)各种源间苗高、地径和生物量的分配存在显著差异,浙江杭州种源的植株枝叶繁茂、根系发达,生长表现好,安徽黄山种源的植株矮小,生长表现较差; 浙江杭州种源将生物量更多分配在根和叶,提高其根系吸收养分和叶片获取光能的能力,安徽黄山种源总体生物量积累最少,长势最差。(4)通过主成分分析法对各种源的花榈木适应性进行综合评价,结果显示浙江杭州种源>贵州黎平种源>浙江永康种源>贵州望谟种源>福建建瓯种源>贵州凯里种源>贵州石阡种源>贵州花溪种源>贵州平塘种源>安徽黄山种源。综上结果表明,浙江杭州、贵州黎平和浙江永康种源花榈木对贵阳地区立地环境具有较强的适应能力和生长潜力。     

Growth and photosynthetic responses of <Emphasis Type="Italic">Fagus crenata</Emphasis> seedlings to O<Subscript>3 </Subscript>under different nitrogen loads

To obtain the basic data for evaluating the critical level of ozone (O₃) to protect Japanese deciduous broad-leaved forest tree species, the growth and photosynthetic responses of Fagus crenata seedlings to O₃ under different nitrogen (N) loads were investigated. The seedlings were grown in potted andisol supplied with N as NH₄NO₃ solution at 0, 20 or 50 kg ha⁻¹ year⁻¹ and were exposed to charcoal-filtered air or O₃ at 1.0, 1.5 and 2.0 times the ambient concentration for two growing seasons. The interactive effect of O₃ and N load on the whole-plant dry mass of the seedlings at the end of the second growing season was significant. The O₃-induced reduction in the whole-plant dry mass of the seedlings was greater in the relatively high N treatment than that in the low N treatment. This interactive effect was mainly due to the difference in the degree of O₃-induced reduction in net photosynthesis among the N treatments. The degree of O₃-induced reduction in N availability to photosynthesis was greater in the relatively high N treatment than that in the low N treatment. In conclusion, the sensitivity of growth and photosynthetic parameters of F. crenata seedlings to O₃ become high with increasing amounts of N added to the soil. Therefore, N deposition from the atmosphere should be taken into account to evaluate the critical level of O₃ to protect Japanese deciduous broad-leaved forest tree species.     

桂西南不同种源蚬木光合和生长特征的研究

为选择喀斯特特有树种蚬木(Excentrodendron hsienmu)优良种源,采用完全随机区组试验设计,研究了不同种源蚬木光合生理和生长特征的月动态变化。结果表明,蚬木光合生理特性在不同月份、不同种源间差异显著,净光合速率、气孔导度、蒸腾速率和水分利用效率表现出对气候变化的适应,均随月份发生变化。各种源蚬木净光合速率、气孔导度和蒸腾速率均在8月份最高,4月份和12月份较低。水分利用效率则在8月份最低,4月份和12月份较高。相关分析表明,蚬木各种源苗高与地径、净光合速率均显著正相关,而净光合速率与地径也表现一定的正相关关系,说明净光合速率可作为蚬木生长过程中的指示性监测指标。蚬木大新、武鸣、隆安种源在整个生长季节均表现较高的净光合速率和生长量,以及较低的蒸腾速率,因此,这3个蚬木种源更适合在南宁地区引种种植。     

CO<Subscript>2</Subscript> enrichment,nitrogen fertilization and development of freezing tolerance in Norway spruce

Plant growth and adaptation to cold and freezing temperatures in a CO₂-enriched atmosphere have received little attention despite the predicted effects of elevated CO₂ on plant distribution and productivity. Norway spruce [Picea abies (L.) Karst.] seedlings from latitudinally distinct seed sources (66°N and 60°N) were grown for one simulated growth season under controlled conditions in an atmosphere enriched in CO₂ (70 Pa) and at ambient CO₂ (40 Pa), combined factorially with low (3.6 mM) or high (15.7 mM) concentrations of nitrogen fertilization. There was a clear difference between the two provenances in height growth, in the timing of bud set, and in freezing tolerance. Nitrogen fertilization increased height growth in both provenances, while CO₂ enrichment stimulated height growth only in the southern provenance. We found no significant effects of elevated CO₂ or nitrogen fertilization on the timing of bud set. During cold acclimation, freezing tolerance increased from –10°C to –35°C, and there was a marked increase in all soluble sugars except inositol. Elevated CO₂ in combination with high nitrogen led to a slight increased freezing tolerance in both provenances during the early stages of cold acclimation. However, towards the end of cold acclimation, elevated CO₂ and high nitrogen led to reduced freezing tolerance in the southern provenance, while elevated CO₂ and low nitrogen reduced freezing tolerance in the northern provenance. These results suggest that CO₂ enrichment influences the development of freezing tolerance, and that these responses differ with available nitrogen and between provenances.     

Effects of water stress on photosynthetic activity,dry mass partitioning and some associated metabolic changes in four provenances of neem (<Emphasis Type="Italic">Azadirachta indica</Emphasis> A. Juss)

Chlorophyll (Chl) content, dry mass, relative water content (RWC), leaf mass per area (LMA), proline (Pro) content, malondialdehyde (MDA) content, superoxide dismutase (SOD) and peroxidase (POD) activity, P _N-PAR response curves and gas exchange were studied to determine the effects of water stress on photosynthetic activity, dry mass partitioning and metabolic changes in four provenances of neem (Azadirachta indica A. Juss). The results indicated that provenance differences existed in the adaptation response to water stress that included changes to growth strategies coupled with ecophysiological and metabolic adjustments. As water stress increased, stomatal conductance (g _s), net photosynthetic rate (P _N), transpiration rate (E), and leaf RWC decreased while LMA increased in all provenances. Dry mass was reduced in droughted plants and the percentage increased in dry mass allocated to roots, and enzyme activities of SOD and POD were highest in neem originating from Kalyani (KA) provenance and lowest in neem originating from New Dehli (ND) provenance. In contrast, water stress increased MDA content least in KA and most in ND. Furthermore, neem originating from ND also had the greatest decrease in Chl a/b ratio while the ratio was least affected in neem originating from KA. These findings suggest neem originating from KA may have more drought resistance than neem originating from ND. The data from P _N-PAR response curves are less clear. While these curves showed that drought stress increased compensation irradiance (I _c) and dark respiration (R _D) and decreased saturation irradiance (I _s) and maximum net photosynthetic rate (P _max), the extent of decline in P _max was provenance dependent. P _max under non-waterlimiting conditions was higher in neem originating from Jodhpur (MA) (about 14 μmol m⁻² s⁻¹) than in the other three provenances (all about 10 μmol m⁻² s⁻¹), but mild water stress had minimal effect on P _max of these three provenances whereas P _max of MA provenance declined to 10 μmol m⁻² s⁻¹, i.e. a similar value. However, under severe water stress P _max of MA and KA provenances had declined to 40% of non-stressed values (about 6 and 4 μmol m⁻² s⁻¹, respectively) whereas the decline in P _max of neem originating from Kulapachta (KU) and ND provenances was about 50% of nonstressed values (about 5 μmol m⁻² s⁻¹). These data suggest the P _N responses of KU and ND provenances are most tolerant, and KA and MA least tolerant to increasing water stress, but also suggest MA provenance could be the most desired under both non-water-limiting and water-limiting conditions due to highest P _max in all conditions.     

黄河上游灌区稻田N2O排放特征

黄河上游灌区稻田高产区过量施肥现象十分突出,氮肥过量施用引起土壤氮素盈余,导致N₂O排放量增大,由此引起的温室效应引起广泛关注。采用静态箱-气相色谱法研究黄河上游灌区稻田不同施肥处理下N₂O排放特征。试验设置5个施肥处理,包括常规氮肥300 kg/hm²下单施尿素和有机肥配施2个处理,分别用N300和N300-OM代表;优化氮肥240 kg/hm²下单施尿素和有机肥配施2个处理,分别用N240和N240-OM代表;对照不施氮肥用N0代表。试验结果得出,灌区水稻生长季稻田土壤N₂O排放主要集中在水稻分蘖前及水稻生长的中后期,稻田氮肥施用、灌水及土壤温度的变化对N₂O排放通量影响较大,不同处理水稻各生育阶段N₂O累积排放量与稻田土壤耕层NO^-₃-N含量动态变化显著相关。稻田N₂O排放不是黄河上游灌区稻田氮素损失的主要途径,但灌区稻田N₂O排放的增温潜势较大;稻田氮肥过量施用会显著增加N₂O排放量,在相同氮素水平下,有机肥配施会显著增加稻田土壤N₂O的排放量(P＜0.01)。优化施氮能有效减少灌区稻田水稻生长季N₂O排放量。稻田不同处理的水稻整个生长季土壤N₂O排放总量为2.69-3.87 kg/hm²,肥料氮通过N₂O排放损失的百分率仅为0.43%-0.64%。在灌区习惯灌水和高氮肥300 kg/hm²时,N300-OM处理的稻田N₂O排放量达3.87 kg/hm²,在100 a时间尺度上的全球增温潜势(GWPs)为20.76×10⁷ kg CO₂/hm²;优化施氮240 kg/hm²水平下,N240和N240-OM处理的N₂O累计排放量较N300-OM处理,分别降低了1.18 kg/hm²和0.57 kg/hm²,在100 a尺度上每年由稻田N₂O排放引起的GWPs分别降低了6.33×10⁷ kg CO₂/hm²和3.06×10⁷ kg CO₂/hm²。