黄土塬区麦田CO2通量季节变化

利用涡度相关法对黄土塬区小麦地CO₂通量季节变化进行了研究。结果表明：（1）小麦CO₂通量日变化与生育期、光合有效辐射、土壤温度密切相关。（2）小麦各生育期CO2的平均日收支由大到小依次为拔节孕穗期＞返青期＞起身期＞抽穗期＞成熟期＞灌浆期＞出苗分蘖期＞越冬期。（3）白昼CO₂通量与光合有效辐射在出苗分蘖期、起身期、成熟期几乎不相关,在灌浆期低度相关,在其他生育期内都达到了显著相关。CO₂通量与夜间2cm土壤温度在越冬、起身、拔节孕穗期显著相关,其他5个生育期内为低度相关。（4）小麦收割后表现为碳源,各天具体状况与前一天是否降雨、当天的天气状况有关。     

华南丘陵区冬闲稻田二氧化碳、甲烷和氧化亚氮的排放特征

采用静态箱 气相色谱法对收获后冬闲稻田CO₂、CH₄和N₂O排放进行了田间原位测定,探讨了越冬稻田3种温室气体的排放规律.结果表明,残茬稻田和裸田的CO₂的排放峰值分别出现在18:00和16:00左右.日间CH₄排放为净值,夜间表现为弱吸收.残茬稻田和裸田N₂O夜间排放分别为日间平均的1.79和1.58倍.残茬稻田的昼夜CO₂平均排放通量显著高于裸田(P＜0.05).在测定期间,残茬稻田CO₂排放随温度升高而增高.相关分析表明,CO₂排放与土温、地表温度和气温均呈显著相关,表明温度是影响收获后稻田CO₂排放的主要因素.在11月10日至翌年1月18日测定期间,残茬稻田的CO₂和CH₄平均排放通量分别为(180.69±21.21) mg·m^-2·h^-1和(-0.04±0.01) mg·m^-2·h^-1,CO₂排放通量较裸田高13.06％,CH₄吸收增高50%.残茬稻田的N₂O排放通量为(21.26±19.31) μg·m^-2·h^-1,较裸田低60.75％.由此说明华南丘陵区冬闲稻田是大气CO₂和N₂O的源,CH₄的汇.     

长白山阔叶红松林二氧化碳浓度特征

采用红外气体分析仪对长白山阔叶红松林2003年度CO₂浓度特征进行了分层连续监测,并结合同步气象资料进行了分析.结果表明,长白山阔叶红松林CO₂浓度存在明显的日变化、季变化与垂直变化,这些变化与植被生理活动、土壤呼吸及林内湍流交换强度有关.生长季林内全天CO₂浓度最高值出现在凌晨5:00左右的近地面层,最低值出现在午后15:00左右的冠层部位;日出前后,随着逆温层的打破,林下CO₂有一明显的释放过程.观测期间林内O₂平均浓度为377 μmol·mol^-1,月平均最高值出现在1月,为388 μmol·mol^-1,最低值出现在8月,为352 μmol·mol^-1.生长季夜间森林表现为CO₂的排放,日间表现为CO₂的吸收汇;非生长季日间与夜间森林都主要表现为CO₂的排放源,但在午间冠层部位仍有数小时表现为CO₂的吸收过程.     

若尔盖高原沼泽湿地与草地二氧化碳通量的比较

采用静止箱/气相色谱法,在2003—2005年的植物生长期对若尔盖高原沼泽湿地和草地的CO₂通量进行了对比观测.结果表明：若尔盖高原沼泽湿地和草地CO₂通量的平均值分别为203.22和323.03 mg·m^-2·h^-1,前者为后者的60%左右.沼泽湿地常年积水的环境条件限制了土壤中的植物残体、根系及有机物质的分解,是沼泽湿地CO₂通量低于草地并形成泥炭积累的重要因素.研究区沼泽湿地与草地CO₂通量的季节变化与气温变化呈正相关,峰值一般出现在7月和8月;其日变化也与气温呈正相关,峰值一般出现在11:00—17:00.5 cm深的土壤温度与CO₂通量的相关性高于10和15 cm深的土壤温度.     

开放式空气二氧化碳浓度增高对小麦物质生产与分配的影响

2001—2003年,利用农田开放式空气CO₂浓度增高 (FACE) 技术平台,以冬小麦宁麦9号为供试材料,研究开放式条件下CO₂浓度增高对小麦整个生育期干物质生产与分配的影响.结果表明：与对照相比,FACE处理使小麦播种-越冬始期的干物质生产量略有增加（10.8%),使越冬始期-拔节期、拔节期-孕穗期、孕穗期-抽穗期显著增加,分别增加了31.6%、40.5%、27.2%,使抽穗期-成熟期略有减少(-5.5%),使成熟期生物产量显著增加(13.6%);FACE处理对小麦播种-越冬始期的平均叶面积系数(LAI)和净同化率(NAR)均无显著影响,但使越冬始期-抽穗期LAI显著增加,NAR稍有增加,使抽穗期-抽穗后20 d NAR显著下降;FACE处理使不同生育时期叶片占全株质量的比例下降,而使茎鞘占全株质量的比例增加;FACE小麦抽穗期和成熟期茎鞘可溶性糖和淀粉含量及总量均明显增加.     

内蒙古克氏针茅草原生态系统-大气通量交换特征

基于内蒙古克氏针茅草原生态系统的涡动相关观测资料和小气候梯度系统观测资料,对研究区碳通量和水热通量的日、季动态进行了研究.结果表明：克氏针茅草原生态系统生长季的碳通量日动态呈U型曲线,即日出前释放CO₂,日出后开始吸收CO₂,正午前后达峰值,午后吸收CO₂减弱,日落后重新转为释放CO₂;9月白天CO₂吸收最为强烈,8月次之,10月最低.克氏针茅草原的感热和潜热通量的日动态均呈倒U型曲线,与碳通量日动态相反,即白天感热和潜热通量多为正值,夜间感热为负值,潜热接近于零;感热通量以5月最高,潜热通量以9月最高.冬季草地为弱碳源,CO₂通量较小,夏季表现为明显的碳汇.     

林冠与大气间二氧化碳交换过程的模拟

以长白山阔叶红松林为研究对象,利用Raupach提出的局地近场理论(localized near field, LNF)耦合垂直风速标准差σ_w（z）和拉格朗日时间尺度T_L （z）,建立林冠内CO₂源汇强度和平均浓度廓线之间的关系.结果表明,拉格朗日模型能准确、稳定地模拟林冠与大气之间CO₂的交换特征.模拟值比涡动相关系统实测值高出约15%,与实测值的相关性为89%,这种差异可能主要来自于输入的浓度廓线的波动以及大气稳定层结造成的涡动相关观测系统误差.在近地面层,由于土壤呼吸作用,整个时间段都为CO₂源.林冠层的CO₂源汇强度变化较为复杂,其日变化经历了源－汇－源的转变过程.林冠与大气间CO₂通量交换明显受大气稳定度影响.     

黄土高原春小麦地上鲜生物量高光谱遥感估算模型

通过田间小区试验,测定了4个春小麦品种(定西24号、陇春8139、高原602和定西38号)在不同生育期和不同种植密度下冠层光谱反射率及其对应的地上鲜生物量,分析了春小麦地上鲜生物量随生育期的变化以及地上鲜生物量与冠层反射光谱和一阶微分光谱之间的相关关系,采用相关系数较大的特征波段及其组合构建光谱特征参数以其作为变量,建立了春小麦地上生物量的高光谱估算模型,并对模型进行检验。结果表明：以参数F₇₈₀和D₇₁₉为变量的对数形式y=3.9498ln F₇₈₀+7.0596和乘幂形式y=512.99D₇₁₉^1.0174估算水平最高,前者均方根误差(RMSE)为0.2173,相对误差(RE)为10.45%,预测值与实测值相关系数为0.854;后者RMSE为0.2188,RE为9.96%,预测值与实测值相关系数为0.853。因此,上述两个模型可作为陇中黄土高原地区春小麦地上鲜生物量的最佳估算模型。     

不同施肥条件下夏玉米光谱特征与叶绿素含量和LAI的相关性

在不同施肥方式下研究了长期试验地夏玉米在4个典型生育期的叶绿素相对含量(SPAD)、叶面积指数(LAI)和冠层光谱特征,系统分析了单波段以及由可见光和近红外波段组成的归一化差异植被指数(NDVI)与叶片叶绿素含量和LAI的相关性.结果表明:在同一个生育期,NK、PK处理和CK的光谱曲线特征相似,NPK、NP、OM、1/2OM1/2NPK处理的光谱特征曲线相似.除460nm外,其它单波段反射率与叶绿素含量和LAI都显著相关,尤其在510~1100nm波段相关性最为密切;不同波段组合的NDVI与这2个指标也显著相关,且相关系数大于单波段.从拔节期到乳熟期,绝大部分NDVI都可以有效地拟合叶绿素含量和LAI的变化,选用NDVI(560,950)和NDVI(660,760)建立拟合模型(R2>0.60),并以NDVI(560,950)拟合效果最佳(R2>0.80).可见,不同施肥方式条件下长期试验地夏玉米冠层光谱特征与叶绿素含量、LAI都具有良好的相关性,可以为夏玉米肥料管理提供科学依据.     

热带季节雨林林冠上方和林内近地层CO2浓度的时空动态及其成因分析

 为探讨西双版纳独特地方气候背景下,热带季节雨林CO₂浓度的时空变化特征和不同时间尺度上环境因素对森林CO₂浓度时间分布的作用,以及 为研究热带季节雨林的碳通量、净生态系统交换量(Net ecosystem exchange, NEE)等提供支持,我们利用热带季节雨林林冠上方和林内近地层 CO₂浓度连续监测资料,结合同步气象资料进行了统计分析。研究结果表明：在植被生理活动、土壤呼吸以及林内湍流的共同作用下,西双版纳 热带季节雨林CO₂浓度表现出明显的日变化、季节变化和林冠上下差异。在日尺度上,林冠上方的CO₂浓度时间变化曲线为“单峰型”,林内近 地层CO₂浓度时间变化曲线为“双峰型”,造成林内近地层傍晚第二个峰值的主要因子是地形因子作用下形成的局地环流。在季节尺度上,林冠 上方CO₂浓度主要受林冠代谢作用的影响,呈现雨季低、干季高的特点,而林内近地层的CO₂浓度则主要受地表呼吸过程所控制,季节变化趋势 与林冠上方相反。林冠上方CO₂浓度低于林内近地层CO₂浓度,且差异较大;在日尺度上,各月（除12月外）CO₂浓度的最大差值皆大于80 mg·m ^－3,且出现在傍晚;在季节尺度上,最大值为-62.9 mg·m^－3,出现在10月,最小值为-8.4 mg·m^－3,出现在12月。     

稻麦叶片氮积累量与冠层反射光谱的定量关系

作物氮素积累动态是评价作物群体长势及估测产量和品质的重要指标,对于作物氮素的实时监测和精确管理具有重要意义。该文以5个小麦(Triticum aestivum)品种和3个水稻(Oryza sativa)品种在不同施氮水平下的3年田间试验为基础,综合研究了稻麦叶片氮积累量与冠层反射光谱的定量关系。结果表明,不同试验中拔节后叶片氮积累量均随施氮水平呈上升趋势;稻麦冠层光谱反射率在不同施氮水平下存在明显差异,可见光区(460~710 nm)反射率一般随施氮水平的增加逐渐降低,近红外波段(760~1 220 nm)反射率却随施氮水平的增加逐渐升高;就单波段而言,810和870 nm处的冠层光谱反射率均与稻麦叶片氮积累量具有相对较高的相关性;在光谱参数中,比值植被指数(Ratio vegetation index, RVI)(870,660)和RVI(810,660)均与稻麦叶片氮积累量具有高度的相关性,且相关系数明显高于单波段反射率,尤其是水稻作物;对于小麦和水稻,均可以利用统一的波段和光谱指数来监测其叶片氮积累量,并可以采用统一的回归方程来描述其叶片氮积累量随单波段反射率和反射光谱参数的变化模式,但若采用单独的回归系数则可以提高稻麦叶片氮积累量估测的准确性。     

农田冬小麦生长和产量对臭氧动态暴露的响应

 评估臭氧(O₃)污染对农田冬小麦生长和产量的影响是污染生态学和生理生态学研究的重要内容之一。该研究运用开顶式气室(OTC),对冬小麦‘ 嘉403’(Triticum aestivum cv. Jia 403)进行了O₃动态暴露的田间原位试验。实验设置过滤空气组(CF)、自然大气组(NF)和两个不同浓度的 O₃动态暴露组(DO100和DO150)。结果表明：1) O₃浓度增加,一方面可以改变灌浆期冬小麦叶片气体交换参数的日变化规律;另一方面引起表观 光量子产额、光饱和点和光补偿点等光响应参数的显著降低。这表明灌浆期叶片光合能力的下降是气孔因素和非气孔因素共同作用的结果。2) O₃暴露可以改变小麦形态特征,如植株变矮、叶片衰老加速、 叶面积变小,并最终导致产量大幅下降。     

Variation in ultraviolet reflectance by carotenoid-bearing feathers of tanagers (Thraupini: Emberizinae: Passeriformes)

Avian visual sensitivity encompasses both the human visible range (400–700 nm) and also near‐ultraviolet (UV) wavelengths (320–400 nm) invisible to normal humans. I used reflectance spectrophotometry to assess variation in UV reflectance for yellow, orange and red plumage in 67 species of tanager (Passeriformes). Previous chemical studies, and my analysis of reflectance minima, suggest that carotenoids are the dominant pigments in yellow, orange and red tanager plumage. Spectra recorded over the range of wavelengths to which birds are sensitive (320–700 nm) were invariably bimodal, with both a plateau of high reflectance at longer (> 500 nm) wavelengths and a distinct secondary peak at UV (< 400 nm) wavelengths. Within this overall framework, variation in UV reflectance was expressed within well‐defined quantitative limits: (1) peak reflectance was always lower than the corresponding plateau of reflectance at longer visible wavelengths; (2) the intensity of peak reflectance declined steadily below 350 nm; (3) wavelengths of peak reflectance clustered between 350 and 370 nm. Significant correlations were detected between various measures of total reflectance in the UV and visible wavebands, but not between various measures of spectral location of UV and visible reflectance. I propose that the strong absorption band at short visible wavelengths (～ 380–550 nm) responsible for bimodal spectra of carotenoids in vitro is also responsible for bimodal reflectance by carotenoid‐based plumage colours. The construction of the UV and visible reflectance bands from different sides of this same absorbance band provides a mechanism for the observed covariation between UV and visible wavelengths. Lack of an association between the spectral locations of the UV and visible reflectance bands may result from the limited variation in spectral location of the UV band. These patterns suggest that plumage colours are subject to constraints, just as are more traditional morphological characters. © 2005 The Linnean Society of London, Biological Journal of the Linnean Society, 2005, 84 , 243–257.     

Effects of CO2 Enrichment at Different Irradiances on Growth and Yield of Wheat: I. EFFECTS OF CULTIVAR AND OF DURATION OF CO2 ENRICHMENT

Wheat, Triticwn aestivum L., the winter cultivars Hobbit andCappelle-Desprez, and the spring cultivars Sicco and KJeiber,were grown in normal air or air enriched with CO₂ either outdoorsin a glass-roofed cage or in controlled environment rooms. Inneither the winter nor the spring wheat was growth increaseddue to enrichment with CO₂ before anthesis. Enrichment of thetwo winter wheat cultivars increased shoot dry weight significantlyat 15 d after anthesis but produced no significant increasein grain yield. With the spring cultivars there was a significantincrease in shoot dry weight by 18 d after anthesis and thegrain yield was also larger due to an increase in grain size.Shoot weight increased because the stems were larger, and therewas a diversion of assimilate from grain growth to late tillerproduction. Root tissue comprised less than 20% of the totaldry matter at anthesis (for all cultivars); effects of CO₂ enrichmenton root growth appeared to be less important than effects onshoot and ear growth. Growth and yield responses to CO₂ enrichmentwere observed (for the spring cultivars) at irradiances of both250 and 635 µE m^–2 s^–1, but the effects weregreater at the lower irradiance. Key words: CO₂ enrichment, Wheat, Cultivar     

Estimation of leaf nitrogen content from spectral characteristics of rice canopy

Ground-based remotely sensed reflectance spectra of hyperspectral resolution were monitored during the growing period of rice under various nitrogen application rates. It was found that reflectance spectrum of rice canopy changed in both wavelength and reflectance as the plants developed. Fifteen characteristic wavebands were identified from the apparent peaks and valleys of spectral reflectance curves, in accordance with the results of the first-order differentiation, measured over the growing season of rice. The bandwidths and center wavelengths of these characteristic wavebands were different among nitrogen treatments. The simplified features by connecting these 15 characteristic wavelengths may be considered as spectral signatures of rice canopy, but spectral signatures varied with developmental age and nitrogen application rates. Among these characteristic wavebands, the changes of the wavelength in band 11 showed a positive linear relationship with application rates of nitrogen fertilizer, while it was a negative linear relationship in band 5. Mean reflectance of wavelengths in bands 1, 2, 3, 5, 11, and 15 was significantly correlated with application rates. Reflectance of these six wavelengths changed nonlinearly after transplanting and could be used in combination to distinguish rice plants subjected to different nitrogen application rates. From the correlation analyses, there are a variety of correlation coefficients for spectral reflectance to leaf nitrogen content in the range of 350-2400 nm. Reflectance of most wavelengths exhibited an inverse correlation with leaf nitrogen content, with the largest negative value (r = -0.581) located at about 1376 nm. Changes in reflectance at 1376 nm to leaf nitrogen content during the growing period were closely related and were best fitted to a nonlinear function. This relationship may be used to estimate and to monitor nitrogen content of rice leaves during rice growth. Reflectance of red light minimum and near-infrared peak and leaf nitrogen content were correlated nonlinearly.     

小麦叶面积指数与冠层反射光谱的定量关系

在分析不同氮素水平下小麦叶面积指数（LAI）和冠层光谱反射率随生育期变化模式的基础上,确立了LAI与冠层光谱反射率及光谱参数的相关关系,提出了小麦LAI的敏感光谱参数及预测方程.结果表明,小麦LAI和近红外短波段（760～1 220 nm）反射率都随施氮量的增加呈上升趋势,可见光波段反射率则相反;从拔节期到成熟期,LAI和近红外短波段反射率均表现为先上升后下降的趋势,而可见光波段（460～710 nm）反射率随生育期的推进先降低后升高,以孕穗期反射率最低,近红外长波段区域（1 480～1 650 nm）反射率的变化与可见光部分相同.LAI与可见光波段反射率呈负相关,与近红外短波段反射率呈极显著正相关,其中以810 nm相关性最好.可以选择RVI(810,510)和DVI(810,560)作为反演小麦LAI的光谱参数.另外,在证明垂直植被指数PVI和转换型土壤调整指数TSAVI对LAI预测能力的同时,发现利用RVI(810,510)、DVI(810,560)和PVI 3个植被指数共同推算小麦LAI的准确度更高.     

平稳小波变换在冬小麦SPAD高光谱监测中的应用

在2010与2011年度冬小麦生长季通过大田小区试验,利用ASD便携式野外光谱仪和SPAD 502叶绿素计实测冬小麦冠层的高光谱反射率与SPAD值.分析不同SPAD值下的冬小麦冠层光谱特征,建立了基于归一化植被指数（NDVI）与比值植被指数（RVI）、小波能量系数的不同生育期冬小麦SPAD估算模型.结果表明： 随着SPAD值的增大,“绿峰”与“红谷”特征愈加明显.在冬小麦返青期、拔节期、抽穗期、灌浆期NDVI估算SPAD的效果较好,估算模型的R²分别为0.7957、0.8096、0.7557、0.5033.小波能量系数回归模型可以提高冬小麦SPAD的估算精度,在返青期、拔节期、抽穗期、灌浆期以高频、低频小波能量系数为自变量的冬小麦SPAD估算模型的R²分别达到0.9168、0.9154、0.8802、0.9087.     

小麦叶片氮素状况与光谱特性的相关性研究

 系统分析了不同时相下两个小麦(Triticum aestivium)品种叶片含氮量及叶片氮积累量与冠层光谱反射特征的关系。结果表明,随施氮水平的增加,小麦冠层在可见光区的反射率逐渐降低,而近红外波段的反射率逐渐升高。小麦叶片氮素状况与比值指数或归一化指数显著相关,两个品种表现极为一致,可以用一个指数方程来拟合。分阶段建模并没有提高模型的精度,因此可以建立一个适用于整个生育时期的通用氮素诊断方程。叶片含氮量同光谱指数在整个生育期内的关系要优于叶片氮积累量的,其中,与叶片含氮量关系最佳的指数为红波段(660 nm)和蓝波段(460 nm)的组合(R2>0.80);与叶片氮积累量关系最佳的光谱指数为中红外波段(1 220 nm)与红波段(660 nm)的组合(R2>0.62)。     

Effects of climate change on productivity of cereals and legumes; model evaluation of observed year-to-year variability of the CO2 response

The effect of elevated [CO₂] on the productivity of spring wheat, winter wheat and faba bean was studied in experiments in climatized crop enclosures in the Wageningen Rhizolab in 1991–93. Simulation models for crop growth were used to explore possible causes for the observed differences in the CO₂ response. Measurements of the canopy gas exchange (CO₂ and water vapour) were made continuously from emergence until harvest. At an external [CO₂] of 700 μmol mol^?1 Maximum Canopy CO₂ Exchange Rate (CCERmax) at canopy closure was stimulated by 51% for spring wheat and by 71% for faba bean. At the end of the growing season, above ground biomass increase at 700 μmol mol^?1 was 58% (faba bean), 35% (spring wheat) and 19% (winter wheat) and the harvest index did not change. For model exploration, weather data sets for the period 1975-88 and 1991–93 were used, assuming adequate water supply and [CO₂] at 350 and 700 μmol mol^?1. For spring wheat the simulated responses (35–50%) were at the upper end of the experimental results. In agreement with experiments, simulations showed smaller responses for winter wheat and larger responses for faba bean. Further model explorations showed that this differential effect in the CO₂ response may not be primarily due to fundamental physiological differences between the crops, but may be at least partly due to differences in the daily air temperatures during comparable stages of growth of these crops. Simulations also showed that variations between years in CO₂ response can be largely explained by differences in weather conditions (especially temperature) between growing seasons.