利用热扩式边材液流探针（TDP）测定树木整株蒸腾耗水量的研究

 介绍了热扩散式液流探针的工作原理及利用液流探针测定树木边材液流速率的方法。利用边材液流探针和多种气象因子传感器及数据采集系统组成的微型气象站,通过对北京西山地区油松(Pinus tabulaeformis)、栓皮栎(Quercus variabilis)混交林林分平均木树干边材液流速率及风速、有效辐射和空气温度、空气相对湿度的日变化和连日变化的测定和分析,揭示了5月干旱季节两树种蒸腾耗水的日变化和连日变化规律,以及栓皮栎树干基部和树冠大枝边材液流的差异,并进行了理论推导,同时分析了液流速率的波动规律与主要气象因素波动的相关性。     

春季麻栎树干边材木质部液流垂直变化及其滞后效应

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,对泰山林科院林场麻栎(Quercus acutissima)人工林树干不同高度边材液流及其相关环境因子进行了连续观测,对影响边材液流的主要环境因子进行了相关性和滞后效应分析。结果表明:同一立木,树干上位边材液流流速上升快,高峰期持续时间短,但高峰流速较高,最大流速在0.002 cm·s^-1以上;树干下位边材液流流速上升、下降慢,液流高峰期持续时间较长,最大流速不超过0.001 cm·s^-1。太阳净辐射是麻栎边材液流最主要的影响因子,且成正相关,空气温度、空气相对湿度对边材液流的影响较小,空气温度与麻栎边材液流的影响成正相关,相对湿度与边材液流速率成负相关。边材液流与主要环境因子日周期波动在时间上存在延迟效应,延迟效应因树干高度和环境因子而变。树干上、中和下部边材液流与太阳净辐射变化的滞后时间分为80、20和30 min,与空气温度的滞后时间分别为60、130和110 min,与空气相对湿度的滞后时间分别为170、160和90 min。     

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。     

元宝枫生长旺季树干液流动态及影响因素

利用热扩散式边材液流探针和多种气象、土壤因子传感器组成的全自动数据采集系统和美国产Licor-6400光合测定系统,于夏秋季节对北京西山地区低山成林元宝枫单株边材液流动态和叶片蒸腾作用进行了系统观测。元宝枫树干边材液流变化受天气的影响,环境胁迫或环境的改善都能改变边材液流的波动特征。在正常情况下,边材液流的日变化呈单峰曲线:日出后树干液流迅速上升,峰值在中午前后出现,然后下降,在次日早晨前达到坡谷。最热月7月液流启动和进入坡谷的时间比其他各月早1~4 h。6月树干上位液流速率大于中位和下位,其他各月树干下位液流速率大于上位和中位,这种差距在7月达2~3倍。多元回归分析表明,在整个生长旺季,元宝枫边材液流变化深受气温、太阳辐射、空气相对湿度、土壤温度和风速等环境因子的影响,但在不同的观测时段和观测部位其影响的主导因子不完全相同,只有空气温度在任何情况下都是影响液流的主导因子;元宝枫边材液流的变异规律较好地说明了其耐旱的生态策略。     

黄土高原半干旱区刺槐生长盛期树干液流动态

通过研究树干液流速率与气象因子的关系,可以定量地分析树木生长与群落蒸腾耗水的相互关系,揭示黄土高原半干旱区刺槐水分利用动态及其适应环境因子的内在机理,为当地生态环境建设提供理论依据。应用热扩散式树干茎流计(TDP)于2008年7月1日至7月26日,在黄土高原半干旱区安塞县对刺槐(Robinia pseudoacacia)人工林生长盛期树干液流速率进行了连续测定,并对周围气象、土壤水分等指标进行了同步测定。刺槐生长盛期树干液流速率晴天日变化呈宽峰形曲线,在测量时期液流速率日平均值为0.00133cm·s–1;刺槐树干单位边材面积的液流速率与光合有效辐射、大气温度、水汽压差呈极显著正相关关系,与相对湿度呈负相关关系。其相关程度绝对值顺序为光合有效辐射大气温度水汽压差相对湿度风速;刺槐边材面积与胸径之间存在着显著的线性相关关系,相关系数为0.878,单位边材面积的液流速率随树干胸径的增大而减小。     

干旱荒漠区银白杨树干液流动态

应用热扩散式树干茎流计(TDP)于2012年7月1日至7月25日,在克拉玛依地区农业开发区对银白杨(Populus alba L.×P.talassica)人工林树干液流速率进行了连续测定,并对气象、土壤水分等指标进行了同步测定。结果表明:7月份的晴天银白杨树干液流速率日变化呈单峰型,阴天呈多峰型,在测量时期液流速率日平均值为0.6059 L/h;银白杨树干单位边材面积的液流速率与太阳总辐射、大气温度、水汽压差呈极显著正相关关系,与相对湿度呈负相关关系。其相关系数绝对值顺序为太阳总辐射>大气温度>水汽压差>相对湿度>风速;银白杨边材面积与胸径之间存在着显著的线性相关关系,相关系数为0.834,单位边材面积的液流速率随树干胸径的增大而减小。     

毛红椿人工林树干液流动态变化对坡位的响应

2012年7-10月,采用液流测定系统监测了位于浙江省开化县的毛红椿人工林上下坡位的树干液流,并同步监测生态环境因子,分析了毛红椿人工林树干液流与土壤含水量、温度和水势等环境因子的关系.结果表明: 研究区上、下坡位树干液流日变化均呈典型的“昼高夜低”单峰曲线;下坡位毛红椿树干液流速率平均值显著高于上坡位;上坡位土壤温度显著高于下坡位,而下坡位土壤含水量和土壤水势显著高于上坡位;下坡位土壤含水量和土壤水势是影响毛红椿树干液流速率的主要因子,而上坡位土壤温度和土壤水势对毛红椿树干液流速率有较大影响.     

油松、栓皮栎树干液流速率比较

应用TDP(ThermalDissipationProbe)技术对油松和栓皮栎树干液流进行了初步研究,经过野外近1a的实地定位观测,研究结果显示:栓皮栎月平均树干液流速率在整个生长期都较油松的月平均树干液流速率要高。前者大约是后者的5~10倍。栓皮栎在土壤干旱时期能够在白天产生明显的树干液流。在土壤干旱时期油松白天不产生树干液流而在晚上产生明显树干液流。在土壤相对湿润时期,油松和栓皮栎树干液流速率的波形与太阳总辐射的波形变化一致,但不同的是油松的树干液流速率波形呈明显的单峰状,而栓皮栎树干液流速率波形呈明显的多峰状。在土壤相对湿润时期太阳总辐射很低时能对油松树干液流速率产生明显的降低作用,而对栓皮栎树干液流则没有明显影响。在土壤干旱时期,油松和栓皮栎树干液流速率的峰值分别大约为0.0001cm/s和0.0006cm/s左右;在土壤水分充足时期,油松和栓皮栎树干液流速率的峰值分别大约相等约为0.0015cm/s左右,分别是油松和栓皮栎在干旱日期的液流速率峰值的10倍和2.5倍。     

侧柏树干边材液流空间变化规律

利用热扩散探针配合自动气象站,于2005年在北京林业大学妙峰山试验林场对侧柏树干边材液流指标空间变化规律进行了研究.结果表明:侧柏树干不同高度边材液流速率随树干高度的升高而增加,而且高层液流峰值的出现时间要比低层早,高层液流曲线尖窄,曲线斜率大,低层液流曲线变化缓慢,曲线斜率小.不同高度的平均液流速率峰值:6.6m处为0.015cm·s-1,4.6m处为0.009cm·s-1,2.6m处为0.006cm·s-1,0.6m处为0.003cm·s-1;无论是液流速率还是连日耗水量,不同直径的单株均表现出沿直径的增加而增加,但液流速率随直径的变化并不是线性的;土壤的含水量限制了树木的耗水能力,日平均液流通量与土壤含水量呈现良好的S型关系,其中与土层20～40cm层关系更为密切;不同气象因子对树干的液流影响方式不同,太阳辐射强度、大气温度和风速与液流指标呈正相关,并且属于第一主分量,对液流的影响较为直接,空气相对湿度和土壤温度与液流指标呈负相关,属于第二主分量,对液流的影响较为缓慢.通过多元线性回归,得出各气象因子和液流相关性均比较高,说明通过气象因子对树干液流进行预测是切实可行的.     

辽西北沙地樟子松树干液流的变化特征及其影响因素

树干液流是量化植物蒸腾耗水的基本指标。本研究于2015年5—10月采用FLGS-TDP热扩散式树干液流计对辽西北半干旱区的沙地樟子松树干液流进行连续观测,同时结合林内小气候观测系统,探讨樟子松树干液流的动态变化特征及其影响因素。结果表明:树干液流速率和日累积量均为晴天阴天雨天,树干液流速率变化均呈"倒U"型,晴天时出现"光合午休"现象;不同月际间(5—10月),树干液流速率与月累积量为7月6月8月5月9月10月;不同季节间,树干液流启动时间夏季比秋季早1 h左右,且树干液流速率夏季秋季。树干液流受气象因子的影响较大,其中光合有效辐射、空气温度、饱和水汽压差(VPD)和风速与树干液流呈显著正相关,空气相对湿度则相反;土壤温度和含水量对树干液流的影响较为复杂,随时间(月际)、天气状况(阴天、晴天和雨天)和土层深度(5、10、20、40和100 cm)的变化而变化,其中,生长季期间和不同月际间(5—10月)、表层土壤温度(0~10 cm)与树干液流均呈显著正相关,深层土壤(20~100 cm)则相反;生长季前(5月)和生长季末期(10月),树干液流随土壤水分的增多而增加,生长季期间(6—9月)则相反,树干液流随土壤含水量的增加而减弱。     

Comparative study of circadian variation in oral,tympanic, forehead,axillary and elbow pit temperatures measured in a cohort of young university students living their normal routines

The primary objective of the present research work is to study and compare the circadian variability in body temperature recorded from different locations of the body during subjects’ normal routines. Temperatures of oral cavity (sublingually), tympanum, forehead, axilla and the elbow pit were measured simultaneously at approximate 1-h intervals for five consecutive days during subjects’ waking span in their routine living condition. The observations were made in eight young, apparently healthy, university students. Data were analysed using cosinor rhythmometry for evaluation of circadian rhythms and two-way ANOVA with repeated measures to assess the effect of time of day and measuring site on body temperatures and their interaction. Significant circadian rhythms in body temperature, irrespective of site, were found. Based on autocorrelation analysis, it was observed that the day-to-day variability in body temperature was consistent. The acrophases of all the studied temperature rhythms were located in the afternoon, except axillary temperature, which occurred in the early evening. The mean daytime temperature was found to be the highest when recorded sublingually and it was the lowest on the forehead or elbow pit. On the basis of the results of this study, we recommend that the methods used could be introduced into laboratory courses in a curriculum of chronobiology courses for both UG and PG classes for the demonstration/study of circadian rhythms in body temperature under normal routines. The methods used are valuable as they are non-invasive, easily accepted and assessable in a student setting.     

灰飞虱发育起点温度及有效积温的探讨

利用培养箱在恒温条件下饲养灰飞虱Laodelphax striatellus Fallén,测定了卵、若虫、成虫繁殖前和全世代发育历期,用直线回归法计算了灰飞虱各虫态和全世代的发育起点温度和有效积温分别为10.06、6.43、10.29、8.08℃和102.3、365.2、87.5、552.1日·度。并根据有效积温法则预测了该虫在济宁市1年完成的代数为4～5代。     

桑树(Morus alba)朱砂叶螨（Tetranychus cinnabarinus）实验种群的温度效应

采用生命表分析、生存分析、"王-兰-丁"模型及线性模型等分析方法,对15～28℃温区的5个恒温处理朱砂叶螨(Tetranychus cinnabarinus)实验种群进行了系统研究.结果表明,此温区内,种群在生殖、发育和生存3方面,有明显的温度效应:内禀增长力、周限增长力、净增殖力和平均日产卵量、世代平均周期、及种群倍增时间的倒数呈线性增长;而平均寿命、最大死亡年龄,随温度升高而递减;性比和实际产卵天数对温度不敏感.种群在生殖、发育和生存三者之间,采取了较为"折衷"的策略:8℃为发育临界点;13℃左右为生殖和种群增长临界温度;22℃左右为生殖和种群增长最适温度;30℃左右为发育最适温度.     

核桃扁叶甲的发育起点温度和有效积温

室内观察测定5个恒温条件下,核桃扁叶甲Gastrolina depressa Baly各虫态的发育历期及起点温度和有效积温。结果表明:在16～32℃温度范围内,核桃扁叶甲均能完成发育,其发育历期随温度的升高而缩短,卵期、幼虫期、蛹期、产卵前期的发育起点温度分别为9.4,12.2,14.3和11.1℃,有效积温分别为43.2,77.2,36.0和104.7日.度;整个世代的发育起点温度为12.0℃,有效积温为260.5日.度。持续过高温度不适合核桃扁叶甲的生长发育。     

竹织叶野螟发育起点温度和有效积温

采用19,22,25,28和31℃5个温度对竹织叶野螟Algedonia coclesalis Walker各虫态(龄)发育起点温度和有效积温进行测定。结果表明,竹织叶野螟的在19～31℃范围内均能正常生长发育,尤其是28～31℃范围最适宜于竹织叶野螟的生长发育。卵、1龄幼虫、2龄幼虫、3龄幼虫、4龄幼虫、5龄幼虫、6龄幼虫、7龄幼虫、蛹、成虫及世代的发育起点温度分别为6.63,12.51,11.18,10.93,10.05,8.01,6.80,5.78,6.20,7.81和8.33℃,有效积温分别为124.19,64.54,72.59,82.08,93.46,136.84,155.42,201.06,211.55,111.49和1235.50日.度。     

变温和恒温对沙葱萤叶甲发育速率的影响

沙葱萤叶甲为近年来在内蒙古草原猖獗成灾的新害虫,为明确温度对其发育速率的影响,分别设置5个变温组合(8/20℃,11/23℃,14/26℃,17/29℃和20/32℃)和6个恒温(13℃,17℃,21℃,25℃,29℃和33℃),比较了变温和恒温对沙葱萤叶甲幼虫和蛹发育速率的影响。结果表明,不同变温组合和恒温对沙葱萤叶甲幼虫和蛹的发育速率有显著的影响。发育历期随温度的升高而缩短,在变温条件下,1龄幼虫期、2龄幼虫期、3龄幼虫期、总幼虫期和蛹期分别从最低温度组合(8/20℃,平均15℃)的11.00,13.44,23.18,46.42和16.89 d,缩短至最高温度组合(20/32℃,平均27℃)的4.92,4.63,9.17,17.83和5.83 d;在恒温条件下,13℃下幼虫不能发育和存活,1龄幼虫期、2龄幼虫期、3龄幼虫期、总幼虫期和蛹期分别从17℃的14.50,10.75,20.63,45.50和11.00 d,缩短至33℃的6.10,5.47,10.60,22.17和5.33 d。在变温条件下,幼虫和蛹的发育起点温度分别为7.44℃和8.48℃,有效积温分别为344.82日度和113.52日度;在恒温条件下,幼虫和蛹的发育起点温度分别为0.64℃和5.11℃,有效积温分别为714.28日度和147.06日度。变温促进了沙葱萤叶甲幼虫和蛹的发育,本研究结果为沙葱萤叶甲的预测预报及综合防控提供了科学依据。     

Considerations for the measurement of core,skin and mean body temperatures

Despite previous reviews and commentaries, significant misconceptions remain concerning deep-body (core) and skin temperature measurement in humans. Therefore, the authors have assembled the pertinent Laws of Thermodynamics and other first principles that govern physical and physiological heat exchanges. The resulting review is aimed at providing theoretical and empirical justifications for collecting and interpreting these data. The primary emphasis is upon deep-body temperatures, with discussions of intramuscular, subcutaneous, transcutaneous and skin temperatures included. These are all turnover indices resulting from variations in local metabolism, tissue conduction and blood flow. Consequently, inter-site differences and similarities may have no mechanistic relationship unless those sites have similar metabolic rates, are in close proximity and are perfused by the same blood vessels. Therefore, it is proposed that a gold standard deep-body temperature does not exist. Instead, the validity of each measurement must be evaluated relative to one's research objectives, whilst satisfying equilibration and positioning requirements. When using thermometric computations of heat storage, the establishment of steady-state conditions is essential, but for clinically relevant states, targeted temperature monitoring becomes paramount. However, when investigating temperature regulation, the response characteristics of each temperature measurement must match the forcing function applied during experimentation. Thus, during dynamic phases, deep-body temperatures must be measured from sites that track temperature changes in the central blood volume.     

恒温下大戟长管蚜的发育起点温度和有效积温

在16,19,22,25,28和31℃恒温条件下以花卉一串红(Salvia splendens)饲养大戟长管蚜Macrosiphum euphorbiae(Thomas),测得该蚜虫的各龄历期和产仔前期,得出全若虫期的历期。依据有效积温法则计算的1～4龄若蚜和全若虫期的发育起点分别是12.5,7.8,10.3,4.1和9.3℃,有效积温分别是14.6,43.9,29.9,31.9和117.2日.度。大戟长管蚜适合生长发育的温度是19～28℃,最适合温度为25℃。     

Evaluation of the cold strain index (CSI) for peripheral cold environmental stress

The purpose of this study was to evaluate the cold strain index (CSI) for peripheral environmental stress using data from a previous footwear study. Eight men (20±2 yr) dressed in protective cold weather clothing with varying footwear underwent 5 days of cold air (−23.4 °C) testing while attempting to sit for 240 min. Rectal, skin, and toe temperatures (T_toe) were continuously measured. All test exposures were ended after 50–165 min due to cold foot discomfort or T_toe<5 °C. However, CSI values indicated little cold strain. Therefore, we revised CSI to include peripheral cold assessment, which was found to be consistent with subject behavior and measured low T_toe.     

A study of human skin and surface temperatures in stable and unstable thermal environments

Skin temperature is a common physiological parameter that reflects human thermal responses. The purpose of this research was to investigate the effects of radiant temperature on human skin temperature and surface temperature in stable and unstable thermal environments. For a clothed human body, the skin temperature is the surface temperature of the skin, while the surface temperature is the outer surface temperature of the clothes. For this aim, the radiant temperature from 26 to 38 °C and then from 38 to 26 °C was controlled in three different ways; in stable condition keeping stable above 40 min, in unstable condition at a rate of 2 °C/5 min, and in another unstable condition at a rate of 2 °C/10 min. Experimental data showed that at the same radiant temperature, the local skin/surface temperatures during the radiant temperature decrease were higher compared to those during the radiant temperature increase. During the radiant temperature increase/decrease, the increments/decrements of the mean skin temperature and the mean surface temperature decreased gradually from the stable condition, 2 °C/10 min to 2 °C/5 min. Compared to surface temperature, the faster the radiant temperature changed, the more obviously the change in skin temperature was delayed. These data demonstrated that the human body has physiological adaptability to unstable thermal environments.