氮肥对旱作小麦光合作用与环境关系的调节

土壤水分胁迫下,测定不同供氮小麦生理指标与环境因子的结果表明,25％的空气湿度是氮对作物调控的下限。在此值以上,增施氮肥可以提高光合速率适应高温和高湿的能力,扩大气孔导度受空气温度和湿度抑制的范围,提高叶片保水能力,从而增强小麦抗旱能力。     

西藏林芝地区农田土壤蒸发对大气温湿度的响应

蒸发是土-气界面上水分损失和水循环的重要组成因子,受到环境温湿度条件的强烈影响。为阐明高原背景条件下土壤蒸发速率对大气温湿度因子的响应,以西藏林芝农田裸地为研究对象,采用土壤H₂O/CO₂通量仪自动测定土壤表面水分蒸发速率、近地层气温、大气湿度等因子,并通过相关性分析研究变量间的相关关系。结果表明,土壤水分蒸发速率表现为单峰型日变化特征,最大值出现在午后14:00-15:00时,最小值出现在夜间,气温和大气湿度也表现相似的变化特征。土壤蒸发速率与气温之间呈极显著正相关关系(R>0.9, P<0.001),近地层大气湿度对土壤蒸发速率有极显著的正响应关系(R>0.7, P<0.001)。     

Spatial variability of summer microclimates and plant species response along transects within clearcuts in a beech forest

In a 4383 ha beech forest in central Belgium, we investigated whether, within clearcuts, microclimate gradients are detectable, and we tested for correlations between plant species composition and microclimatic heterogeneity. The results highlight a strong correlation between microclimatic parameters and distance from the forest edge. Of the 47 taxa found, 38 (81%) showed a significant change in expected occurrence in response to at least one of the investigated microclimatic parameters (air and soil temperature, air humidity, light intensity). The results suggest that a substantial number of forest herbaceous species with broad European distributions show particular microclimatic requirements. Furthermore, many species show a different response to combined factors, such as for instance soil temperature with increasing air humidity, which indicates that combinations of microclimatic parameters stronger determine the actual temperature, humidity or light levels at which species are expected to be present or not.     

油松人工林SPAC水势梯度时空变化规律及其对边材液流传输的影响

 利用热扩散式边材液流茎流探针（TDP）和微型自动气象站组成的测定系统于2001年4月在北京林业大学妙峰山教学实验林场（39°54′N,116°28′E）对低山油松（Pinus tabulaeformis）人工林土壤-植物-大气体（SPAC）界面水势梯度及油松木质部边材液流传输速率的时空变化规律及其相关因子进行了连续测定。土壤水势随深度下降逐渐升高,日周期波动幅度减小,灌水后上层土壤水势迅速提高,但随着水分扩散和林地持续蒸散,土壤湿度迅速下降并逐渐与对照趋同;叶片水势连日逐渐降低,灌水后水势较对照有一定程度提高;林冠不同层次叶片水势在日周期内不同时间差异显著,但同一层次之间差异不明显;油松人工林土壤、叶片、大气水势梯度比约为1∶5∶30,灌水后SPAC相临界面水势差增大,水势梯度提高至1∶15∶90。大气水分饱和亏缺与土壤水势和叶片水势、以及土壤水势与叶片水势之间均有极显著相关性。干旱春季灌溉对油松木质部边材液流时空波动产生很大影响,灌水后连日树干上位边材液流峰值出现时间推迟1 h,连日平均液流速率提高48.59%,连日平均最大液流速率提高25.12%。木质部边材液流速率日变化和连日变化与SPAC水势和气象因子如空气相对湿度、空气温度、太阳辐射强度密切相关。与对照相比,灌水后边材液流速率与SPAC各介质水势和界面水势差的相关性下降。     

The Effect of Climatic Factors on the Activity of Ants (Hymenoptera,Formicidae) in Broadleaf Forests of Kiev. Communication 2

Studies of seasonal dynamics of the activity of ants were carried out in July–August of 2013–2015 in broadleaf forests (Kyiv, Ukraine. Transects were located within foraging areas of three dominant species Formica rufa L., Lasius fuliginosus (Latreille), and L. emarginatus (Olivier). Thirteen species of ants were encountered on the soil surface. Factors that influence the activity of ants in forests may be ranked by importance as follows. (1) Climatic factors: (a) air temperature and soil humidity; (b) mean monthly rainfall; (c) air humidity. (2) Phytogenic factor (tree species composition). 3. Interspecific hierarchy of ants (primarily, territoriality of the dominant species).     

Air humidity,soil moisture and soil chemistry as determinants of the herb layer composition in European beech forests

Question: What role does air humidity play as an environmental factor for the abundance and distribution of temperate woodland herbs? Location: Beech forests on calcareous soils in southern lower Saxony, central Germany. Methods: The abundance of woodland herb species and total herb cover were investigated in 60 plots with contrasting exposure, slope angle and relief type. On all plots, air humidity, air temperature, soil moisture, photosynthetically active radiation, pH (H₂O) and concentration of salt‐exchangeable Ca, Mg and K were measured. Species‐environment relationships were analysed with multiple regression analysis and CCA. Results: Air humidity (RH), soil moisture and the concentration of exchangeable Ca and K, but not light, C/N ratio and the concentration of exchangeable Mg were identified as the most important abiotic factors influencing the cover of the most abundant plant species and total herb cover. RH varied substantially across the different forest floor site types and influenced species abundance independent of soil moisture. In several species (including Mercurialis perennis and Impatiens noli‐tangere), RH was found to be a key environmental factor. Other species such as Aegopodium podagraria and Lamiastrum galeobdolon depended more on elevated soil moisture, while RH was less important. Conclusions: This study showed that the distribution of widespread temperate woodland herb species depends on high air humidity, and that certain sensitive species do not occur at sites with reduced air humidity even though soil moisture is high. Thus, high air humidity and ample soil moisture are key abiotic factors in beech forests on calcareous soils. Shade level (PAR) was found to be of secondary importance.     

Badger Meles meles setts–architecture, internal environment and function

Badger setts vary considerably in size, ranging from simple single-entrance burrows to complex tunnel systems hundreds of metres long with multiple entrances and underground chambers. Data from 19 excavated setts show that main setts are larger than other setts in terms of area and volume, and contain more chambers, nests and latrines; but setts of different sizes and types are built according to the same basic architectural principles. Little is known about the environmental conditions within setts, other than that temperature and humidity are constant in parts of a sett that are at least 7 m from the nearest entrance. Setts are used for breeding and as sleeping places and refuges, but a question remains as to the functional value of large setts. It is suggested that large main setts allow members of a social group to avoid one another underground, especially when breeding. Little is known about the use of other types of sett.     

南方红豆杉生长发育及其紫杉醇含量与环境因子的关系

研究了人工种植的3年生南方红豆杉的生长发育特征及其枝叶中紫杉醇的含量,并观测了其生长环境因子的动态特征。通过对南方红豆杉的生长发育特征以及其枝叶中紫杉醇含量与生长环境因子进行相关分析发现,南方红豆杉生长发育与空气和土壤湿度呈极显著的正相关,与空气和土壤温度、土壤N和K含量、土壤有机质和土壤紧实度呈正相关,与净辐射和土壤P含量呈负相关,但相关关系不显著,说明高温、高湿以及遮荫有利于南方红豆杉的生长,且对土壤P含量有较高需求;南方红豆杉枝叶中紫杉醇含量与空气和土壤湿度、土壤N、P和K含量呈负相关,与净辐射、空气和土壤温度、土壤有机质和土壤紧实度呈正相关,但相关关系均不显著,说明高温、高光强和干旱促进南方红豆杉枝叶中紫杉醇含量的增加,且紫杉醇含量的增加对土壤中N、P和K含量有一定的需求,尤其是N和K,对P需求不大;南方红豆杉生长发育与其枝叶中紫杉醇含量呈负相关,相关关系也不显著,推测紫杉醇可能是南方红豆杉的防御物质,以促使南方红豆杉抵御高温、干旱和高光强等不良环境。     

土地利用方式对喀斯特地区环境小气候日动态的影响

2007年6月,通过典型样地观测,研究了广西凌云县典型喀斯特地区5种不同土地利用方式下光照强度、气温、空气相对湿度、土壤温度、表层（0～5 cm土层）土壤含水量的日动态.结果表明：不同土地利用方式改变了地上植被的组成、覆盖度和高度,进而改变了环境小气候,研究区不同土地利用方式的小气候质量依次为林地＞灌林＞草地＞农耕地＞石漠化裸地; 石漠化裸地光照强度较强、气温和土壤温度较高、空气相对湿度和土壤含水量较低,且各因子的变幅均较大,样地环境趋于干热化;与石漠化裸地相比,林地、灌林地、草地和农耕地内的光照强度分别下降96.4%、52.0%、17.0%和44.2%,气温分别下降30.1%、20.2%、12.7%和17.8%,空气相对湿度分别提高129.2%、57.2%、18.0%和41.2%,土壤温度分别下降11.5%、8%、2.5%和5.5%,表层土壤含水量分别提高42.6%、33.2%、15.7%和14.0%,林地与灌林地各因子的变幅相对趋缓,样地环境趋于凉湿化.各样地光照强度、气温和土壤温度之间呈正相关,三者均与空气相对湿度、土壤含水量呈负相关,空气相对湿度与表层土壤含水量呈正相关.     

鲁东沿海丘陵茶园防护林的小气候特征

近年来山东乳山茶业逐渐兴起, 但由于北方冬春季温度低和倒春寒频繁发生, 茶叶种植面积逐年减小。如何在低成本管理的基础上提高茶叶产量和品质, 成为乳山茶园管理的一大难题。以2007年春季采用水平梯田整地种植的茶园为试验区, 以梯田周围营造的4种网格(8 m × 80 m, 12 m × 80 m, 20 m × 80 m, 40 m × 80 m)茶园防护林为研究对象, 分别在2013年4月、8月和12月, 测定风速、空气温度、土壤温度、空气相对湿度及土壤相对湿度, 以纯茶园作为对照, 进行了小气候因子测定和分析。结果表明: (1) 4种防护林均能有效地降低茶园内风速, 调节气温、土壤温度和土壤相对湿度, 增加空气相对湿度, 为茶树生长提供适宜的生态环境; (2)由于区域水分通量和太阳辐射的季节变化, 4种防护林的小气候调节效应也表现出一定的季节性差异; (3)主成分分析结果表明, 4种茶园防护林中, 影响小气候因子的主要因素是气温和土壤温度, 其因子负荷量分别为-0.978和0.986, 但风速与气温呈极显著相关关系, 与土壤温度之间无显著线性关系, 因此, 风速也能间接地影响林内小气候; (4) 8 m × 80 m的防护林对小气候的总体调节效应优于其他3种防护林。     

Effect of Acacia plantations on net photosynthesis, tree species composition, soil enzyme activities, and microclimate on Mt. Makiling

To determine the effectiveness of rehabilitation on improving ecosystem functions, we examined net photosynthetic rate (P _N), tree species composition, soil enzyme activities, and the microclimate (air and soil temperature, relative humidity) of an area on Mt. Makiling that has been rehabilitated and protected from fire for over 12 years. After it was last burned extensively in 1991, restoration was initiated by planting Acacia mangium and Acacia auriculiformis. We selected three areas to study in 2003. Two areas were rehabilitated with A. mangium and A. auriculiformis, and one was still dominated by Imperata cylindrica and Saccharum spontaneum. P _N of A. mangium and A. auriculiformis showed significantly lower values than those of I. cylindrica and S. spontaneum. The Acacia plantations had more naturally regenerated tree species than the grassland. Additionally, more tree species appeared in the A. mangium plantation than in the A. auriculiformis plantation. Ficus spetica was present in all of the study sites. Dehydrogenase and phosphatase activities were significantly higher in soil under the Acacia plantations than under grassland. Grassland showed higher air temperature, relative humidity, and soil temperature as well as a larger variation per hour in these parameters compared to the Acacia plantations. The highest air temperature, relative humidity, and soil temperature were measured in April during the dry season. From the regression analysis, soil temperature was significantly correlated with air temperature. Hence plantations, as a rehabilitation activity for grassland, promote natural regeneration and stabilize the microclimate. This stabilization of the microclimate affects establishment and growth of naturally occurring tree species.     

1980—2005年松嫩平原土壤湿度对气候变化的响应

基于松嫩平原16个农业气象站1980—2005年作物生长季的旬土壤湿度、月气温和月降水量观测资料,采用统计分析方法,分析了研究区表层（0～30 cm）土壤湿度的时空变化特征及其对气温、降水量等气候变化的响应.结果表明：1980—2005年间,松嫩平原不同区域作物生长季表层土壤湿度均呈减小趋势,松嫩平原表层土壤存在干旱化趋向,其中,西部和南部地区尤为明显;20世纪90年代以前,研究区表层土壤处于比较湿润阶段,之后土壤湿度持续降低,并发生了偏干现象;研究期间,松嫩平原作物生长季平均气温呈周期性波动上升,每6 a一个周期,期间小幅波动,1992年开始明显上升;生长季降水量的年际变幅较大,存在一个4～5 a的波动周期;研究区作物生长季表层土壤湿度与气温呈极显著负相关关系,与降水量呈极显著正相关关系（P<0.01）.气温和降水量是影响松嫩平原作物生长季表层土壤湿度变化的主要气候因素.     

长白山温带阔叶红松林对温湿环境的调节效应

森林具有改善气候、调节微环境的作用,森林小气候的研究对于揭示森林生态系统功能、评估森林生态环境效益具有重要意义.本研究以长白山阔叶红松林为例,基于2003—2014年林内通量塔气象资料及其附近气象站空旷地的同时段气象资料,对其最高、最低和平均气温、相对湿度和表层土壤温度的日变化和季节变化进行对比分析.结果表明: 林内气温和相对湿度分别呈现单峰型和U型日变化规律,日较差较林外低2.31 ℃和8.3%,表层土壤温度日变化趋于恒定,阔叶红松林减缓了温湿度的日变化.夏季主要为降温效应,冬季表现出显著的增温效应.夏季林内气温和土温比林外低1.30和3.91 ℃;冬季林内气温和土温比林外高2.06和5.44 ℃.森林对最高温和最低温的调节效应显著.在季节尺度上,夏季森林降低最高气温和土温1.80和5.45 ℃,冬季提高最低气温和土温3.69和7.92 ℃.在年尺度上,林内年最高气温和土温分别较林外低1.60和4.99 ℃,年最低气温和土温分别较林外高1.12和8.82 ℃.森林对土温的调节效应强于对气温的调节效应.气温和土温均以对低温的保温作用为主.     

洪水漫溢对林窗微环境时空差异的影响——以塔里木河中游荒漠河岸林为例

林窗是森林生态系统中普遍存在的干扰形式。探究洪水漫溢对林窗内部微环境时空异质性的影响,对揭示荒漠河岸林物种多样性变化及其更新特征具有重要意义。在塔里木河中游非洪水和洪水漫溢区各选取一个大小相似的林窗样地,并使用便携式气象监测仪对林窗内不同方位的空气温湿度进行监测,对比分析不同水淹条件下林窗内微环境的时空分布差异,为深入探索荒漠河岸林植被更新机制奠定基础。结果表明：（1）非洪水漫溢区和洪水漫溢区林窗内空气温度均呈现先上升后下降的变化趋势,空气湿度均呈现先下降后上升的变化趋势,且同一个样地中温度与湿度之间存在明显的负相关关系,而洪水漫溢改变了森林微环境,使林窗内湿度升高,温度下降。（2）非洪水漫溢区和洪水漫溢区林窗内不同方位温度分布差异较小,洪水漫溢对温度变化影响不大;两个样地林窗内湿度变化过程较为复杂,差异明显,洪水漫溢区湿度变化梯度更为密集。（3）非洪水漫溢区和洪水漫溢区林窗内温度差界限明显,西南方向温度差较小,中心位置温度差最大,洪水漫溢并未改变不同方位温度变化趋势;湿度差以中心偏北方向较大,其中非洪水漫溢区湿度差在西北方向较小,而洪水漫溢区湿度差最小值出现在西南方向。研究结果表示荒漠河岸林林窗微环境时空差异具有干旱区独特性,同时阐明了林窗微环境对洪水漫溢的响应,为深入研究林窗干扰对荒漠河岸林更新与演替提供了科学依据。     

MicroclimOz – A microclimate data set for Australia,with example applications

Many problems in pure and applied ecology require the quantification of above‐ and below‐ground microclimates. Here I describe a data set of hourly microclimates for the Australian continent, simulated from the years 1990 to 2017 across a grid of 1893 locations approx. 60 km apart. The data were generated with the NicheMapR microclimate model, driven by 0.05° gridded daily meteorological forcing data (air temperature, wind speed, humidity, cloud cover, rainfall), 0.025° elevation and 0.008° soil texture data. The above‐ground microclimate variables include horizontal plane solar radiation, solar zenith angle, sky temperature (from which down‐welling longwave radiation can be computed), air temperature, relative humidity and wind speed at 1 and 120 cm height, and snow depth. The below‐ground variables include soil temperature, pore humidity, soil moisture and soil water potential for 0, 2.5, 5, 10, 15, 20, 30, 50, 100 and 200 cm below‐ground. The computations are for four shade levels (0%, 50%, 70% and 90%). The data set can be used for a wide variety of applications, including the computation of heat and water budgets of organisms, the potential for vegetation growth, and the computation of stress and growth indices. The use of daily forcing data also allows assessments of the consequences of extreme events including heat waves. Example applications are provided for computing plant growth potential, grasshopper egg development, lizard body temperature and mammalian energy and water requirements.     

Adult diapause in the Colorado potato beetle, Leptinotarsa decemlineata: effects of external factors on maintenance, termination and post-diapause development

ABSTRACT. This study tests the effects of temperature, water, food and photoperiod on breaking diapause and resumption of activity (emergence from the soil) in Leptinotarsa decemlineata (Say) (Coleoptera: Chrysomelidae) diapausing under natural winter conditions or at constant temperatures in the laboratory. Behavioural and physiological criteria were used to characterize the various phases of diapause. Three successive phases are distinguished during hibernation: 'diapause development' or true diapause, a facultative 'post-diapause quiescence' and, finally, a transient phase of post-diapause development leading to emergence from the soil. Diapause development is completed within 3 months in the field and its duration depends on temperature. Although they are buried in the soil during this phase, beetles remain sensitive to photoperiod when artificially exposed to it. They do not emerge from the soil when exposed to higher temperatures. Thereafter, they stay in a quiescent state maintained by low temperature, low humidity or lack of food. The response to temperature changes during hibernation. In the soil, activity begins when soil temperature reaches 4–5C, but this temperature is too low to permit postdiapause development. The transient phase has a temperature threshold between 8 and 10C, whereas emergence from the soil occurs only when the temperature exceeds 11C. Post-diapause development is influenced strongly by temperature and humidity. After emergence, post-diapause development leads eventually to reproduction. Food is essential for reproduction after diapause whereas photoperiod plays no further role.     

Air humidity as key determinant of morphogenesis and productivity of the rare temperate woodland fern Polystichum braunii

(1) Most ferns are restricted to moist and shady habitats, but it is not known whether soil moisture or atmospheric water status are decisive limiting factors, or if both are equally important. (2) Using the rare temperate woodland fern Polystichum braunii, we conducted a three‐factorial climate chamber experiment (soil moisture (SM) × air humidity (RH) × air temperature (T)) to test the hypotheses that: (i) atmospheric water status (RH) exerts a similarly large influence on the fern's biology as soil moisture, and (ii) both a reduction in RH and an increase in air temperature reduce vigour and growth. (3) Nine of 11 morphological, physiological and growth‐related traits were significantly influenced by an increase in RH from 65% to 95%, leading to higher leaf conductance, increased above‐ and belowground productivity, higher fertility, more epidermal trichomes and fewer leaf deformities under high air humidity. In contrast, soil moisture variation (from 66% to 70% in the moist to ca. 42% in the dry treatment) influenced only one trait (specific leaf area), and temperature variation (15 °C versus 19 °C during daytime) only three traits (leaf conductance, root/shoot ratio, specific leaf area); RH was the only factor affecting productivity. (4) This study is the first experimental proof for a soil moisture‐independent air humidity effect on the growth of terrestrial woodland ferns. P. braunii appears to be an air humidity hygrophyte that, whithin the range of realistic environmental conditions set in this study, suffers more from a reduction in RH than in soil moisture. A climate warming‐related increase in summer temperatures, however, seems not to directly threaten this endangered species.     

土壤和气象条件对宁夏枸杞灰分含量的影响

根据 2 0 0 0～ 2 0 0 1年我国北方 6省区枸杞取样和田间试验资料 ,分析了影响枸杞灰分含量的土壤和气象因子 ,并建立了相应的关系模式。结果表明 ,枸杞灰分含量的变异系数为15 %左右 ,枸杞灰分含量主要由品种因素决定 ,环境因子对灰分含量有重要作用。影响枸杞灰分含量的环境因子主要有果实形成期平均相对湿度、日较差和开花到成熟期降水日数、土壤全钾含量等。果实形成期相对湿度是影响枸杞灰份含量的最主要的因子 ,枸杞灰分含量随这一时期平均相对湿度的增大呈指数型增加。降水日数是影响CMA的关键因子 ,随着枸杞开花到成熟期降水日数的增加 ,CMA呈对数型增加     

Diurnal changes in gas exchange and chlorophyll fluorescence parameters of <Emphasis Type="Italic">Fritillaria cirrhosa</Emphasis> and <Emphasis Type="Italic">F. delavayi</Emphasis> under field conditions

To determine what factors limit the growth of wild Fritillaria cirrhosa and Fritillaria delavayi in field conditions, we investigated diurnal changes of the net photosynthetic rate (P _N) and the correlation between P _N and various environmental factors. Parameters of chlorophyll (Chl) fluorescence were evaluated to test whether ecological fragility caused the extinction of wild F. cirrhosa and F. delavayi. Our study reveals for the first time that F. cirrhosa and F. delavayi did not encounter significant stress under field conditions. A small reduction in maximum photochemical efficiency was observed under high irradiance. The maximum P _N of F. cirrhosa was 30 % higher than F. delavayi (p<0.05), and a similar difference was observed for apparent quantum yield (27.3 %, p<0.01). F. delavayi was better adapted to a wide range of irradiances and high environmental temperature. Correlation between P _N and environmental factors (without considering the effects of interactions among environmental factors on P _N) using leaves of F. cirrhosa revealed that the three primary influencing factors were air pressure (p<0.01), relative humidity (p<0.01), and soil temperature (p<0.05). In F. delavayi, the influencing factors were relative humidity (p<0.01), soil temperature (p<0.05), CO₂ concentration (p<0.05), and air pressure (p<0.05). Path analysis (considering effects among environmental factors on P _N) showed that air temperature (negative correlation), photosynthetic photon flux density (PPFD) and relative humidity were the three primary limiting factors influencing the growth of F. cirrhosa. For this species, relative humidity reacted indirectly with air pressure, which was reported singularly in other species. Limiting growth factors for F. delavayi were PPFD, air pressure (negative correlation), soil temperature (negative correlation) and air temperature (negative correlation).