浑善达克沙地榆树树干液流动态研究

本文应用Granier热扩散技术对内蒙古浑善达克沙地榆树疏林林分进行树干液流通量研究，分别选择胸径大小占林分80%以上林木的三种胸径级（15-25cm，25-35cm，35-45cm）榆树样树各三株，应用Granier探针进行每隔15min的树干液流测定，同步测定林分环境因子，包括空气温度、相对湿度、土壤温度、土壤湿度、光合有效辐射、风速等10余个环境因子，在生长季节进行了5个月的测定，详细研究和分析了榆树树杆液流特征，其中包括昼夜变化趋势和规律、不同天气状况下的液流密度变化特点以及在生长季不同时期的液流密度变化规律，阐述了不同胸径级榆树树干液流变化特征。同时利用连续获得的树干液流通量与环境因子数据，分析了树干液流通量与环境因子的关系，阐明不同时期影响树干液流通量变化的主导因素，以及树干液流密度对环境因子的响应规律。并通过钻取样地内的树木生长年轮芯测定了榆树不同径级的边材面积，建立边材和胸径的关系方程，估算了不同胸径林分的边材面积以及冠层蒸腾的季节动态。 在晴朗的白天，不同胸径级榆树的树干液流密度变化曲线均呈单峰曲线，只是峰值持续的时间不同。不同胸径级榆树树干液流密度变化具有明显的昼夜节律性。在生长季结束后液流并不是马上停止，而是有微弱的波动。阴雨天液流密度变化曲线均不规则且液流密度值较小，甚至出现多峰曲线，而且峰值明显;液流密度的变化出现较大的波动性，夜间却有液流发生，而且值较晴天的夜间液流密度稍大。 林分不同胸径级榆树树干大径级木、中径级木和小径级木液流通量特征表现为: 榆树大径级木液流密度的峰值大于中等木，中等木峰值大于小径级木，差异明显;大径级木由于年龄较大，液流密度曲线变化平缓，没有明显的峰值，呈弧形曲线; 而且不同年龄的树木反映差别比较大，但是总体趋势还是受胸径的影响。 随季节推移生长季各月份液流密度均值基本逐渐减小，进入生长季末期(10月)基本处于微弱波动状态。液流通量月平均值最大值一般都出现在6-8月，大径级木、中径级木和小径级木各月液流通量变化差异较大。日液流通量比较分析得出，大径级木日液流通量最大值分别为394.53，中径级木为66.04，小径级木为63.56 kg∙ d-1。综合分析对不同胸径树木影响较大的环境因子为VPD，PAR，Ta; 但是在不同生长季节，对不同类型树木起主要作用的环境因子也不尽相同，但是PAR与VPD是其中基本主要起作用的两个因子。 通过建立边材与胸径的关系方程，得出边材和胸径关系(R2=0.99)。通过经验公式计算得出，林分生长期的蒸腾耗水量相当于2.24mm/day, 低于当地同期降雨量2.78mm/day.

北京山区落叶阔叶林优势种水分生理生态研究

本文研究了北京山区落叶阀叶林优势种一辽东栎、大叶白蜡、北京丁香、核桃楸、山杏和荆条等乔灌木的稳定碳同位素比率，长期水分利用效率、植物蒸腾特性和土壤植物体的水分运动特点，并从植物解剖学的角度研究了这些植物叶片特点和其水分生理生态特性的关系。 对北京山区落叶阔叶林生态系统这几种乔、灌木植物叶片中的碳稳定性同位素比率(δ¹³C值)测定结果显示，这些植物叶片的δ¹³C值受多种因子的影响，具有较大的种间差异及时空异质性。主要表现在不同植物种叶片δ¹³C值不同，其排列顺序为山杏(- 24.75±0.85%。>大叶白蜡(- 25,94±1.52%。)=荆条(- 26.01±1.63%。)=辽东栎(一26.07±1.17%。)=北京丁香(-26.46±0.80c70。)>核桃楸(-28.11±1.52%。);生长初期叶片δ¹³C值较生长末期高，尤以核桃楸和辽东栎表现明显其生长初期和末期的叶片δ¹³C值皆相差达3‰;生境条件，特别是土壤水分含量和土层厚度，对植物叶片的813C值的高低有较大的影响，生长在于旱生境中的植物具有较高的δ¹³C值。另外，即使是同一株植物，叶片δ¹³C值也因其在冠层中所处的位置不同而异，冠层项部叶片的δ¹³C值高于林冠内部的叶片。北京山区落叶阔叶林优势种的长期水分利用效率与种的特点有关，山杏最高(4.950±0．l71mmolC0_2•mol-1H_2O)，核桃楸最低(3.760±0.203mmolC0_2•mol-1H_2O)，大叶白蜡、荆条、辽东栎和北京丁香居中(4.346- 4.530 mmolCO_2•mol-1H_2O)，大部分植物长期水分利用效率在春季（5月）较高，秋季较低，荆条由于物候期的特殊性在其生长季初期较低，而后逐渐增高。核桃楸在不存在水分亏缺情况下，树干液流速率受微气候因子的影响，液流速率的最大值达1600g•hour 左右。树干液流速率的日进程和大气相对湿度、温度的日进程具有相当好的生态学同步性。通过对核桃楸夜晚树干液流的分析可以得出其有根压存在的结论。 植物叶片和枝条中自由水和束缚水含量主要决定于植物种的特性，枝条的年龄、生境特点，特别是土壤水分特点。在落叶阔叶林I(样地2)中植物叶片自由水含量的排列顺序是：北京丁香>核桃楸>大叶白蜡>辽东栎;而杂灌丛（样地1）中植物叶片自由水含量的排列顺序是：核桃楸>大叶白蜡>山杏>荆条>北京丁香>辽东栎，可见群落类型对植物自由水含量影响是很大的，植物束缚水含量与其自由水含量的格局完全相反，荆条、山杏等植物含量高，核桃揪含量低。枝条水分含量有与叶片水分含量相类似的特点。 北京山区落叶阔叶林优势种的水分生理生态学特性和其叶片的特点有很大的关系，首先是植物叶片的特点总是和其种的特性相联系，主要表现在叶的类型、叶片上毛、气孔密度、着生方式等，如荆条叶片上下表面都密被披针形毛，气孔小，核桃楸气孔较大且凸出，大叶白蜡叶片上的气孔凹陷，辽东栎的气孔呈椭圆状，保卫细胞上有许多白色蜡质结晶。有一些种有环状的气孔外缘。生境的变化对叶片的形态特征有影响，在全光照条件下叶片小而犀，而在庇荫条件下叶片大而薄，在扫描电镜下可见全光照条件下北京丁香叶片基本无毛，庇荫条件下则有短微毛，全光条件下荆条叶片上毛有小乳头状凸起，庇荫条件下没有。本文所研究的植物种气孔都着生在叶片的下表面，气孔密度的大小排列顺序是：辽东栎>山杏>北京丁香>核桃楸>大叶白蜡。经方差分析显示种闷气孔密度存在极显著性差异。对所研究植物的气孔导度和环境因子、叶片解剖特点进行线性回归分析，得到了总体的和各个种的回归模型，结果表明光照强度、气孔密度等对气孔导度影响显著，但因种的不同相互之间存在差别。 植物的蒸腾速率受多因子的影响，主要有种的特点、微气候因子（光照强度、大气相对湿度、叶面温度、叶室温度等）和土壤水分特点。植物的蒸腾速率日进程和微气候因子日进程有相当好的生态学同步性。对辽东栎的蒸腾速率和光照强度的研究发现二者有很好的线性关系。这些植物蒸腾速率都表现出一定规律的日进程和季节进程，大多数植物蒸腾速率在一天中有数次波动，最高峰一般出现在中午12时之前;在整个生长季中，6月底至8月初的蒸腾速率高于其他月份。

黄土高原半干旱区人工林刺槐展叶期树干液流动态分析

应用热扩散式树干茎流计(TDP)于2008年4月26日至5月31日,在黄土高原半干旱区安塞县对人工林刺槐展叶期树干液流及其气象、土壤水分等6个指标进行连续测定。结果表明:刺槐展叶期可分为芽期、展叶初期、中期和全叶期。在芽期,刺槐树干液流速率日变化无明显昼夜波动;在展叶初期至全叶期日变化呈现出从微弱波动逐渐增大到趋于平稳的剧烈波动;在展叶中期以后液流速率表现为上升快、下降缓慢的单峰曲线;在全叶期平均峰值约为0.0027cm.s-1;树干液流速率与光合有效辐射强度、大气温度、水蒸气压亏缺和风速呈极显著正相关,与相对湿度呈负相关,其相关程度依次为光合有效辐射强度>大气温度>水蒸气压亏缺>相对湿度>风速,且可用光合有效辐射强度和大气温度线性表达式来估测;土壤水分在展叶期呈逐渐减少趋势,但对树干液流的胁迫不显著;在展叶期刺槐单株日蒸腾耗水量随直径的增大而增大并与胸径呈良好的线性关系,可用来估算展叶期刺槐人工林蒸腾耗水量。

树干直径变化与其水分传输和贮存关系研究进展

生长、含水量变化和水分张力变化都能引起树木直径的变化,树木直径变化表现为长期的不可逆生长和短期的昼夜变化。因为木质部、韧皮部和树皮的不同功能,它们膨胀和收缩的速度也不相同。木质部直径的变化与木质部液流相关,而韧皮部和树皮直径的变化不仅和木质部液流相关,还与韧皮部储存水以及木质部与韧皮部间的水分交换有关。

Effective thermal conductivity of graded nonlinear composites with heat contact resistance

The perturbation expansion method is used to find the effective thermal conductivity of graded nonlinear composites having thermal contact resistance on the inclusion surface. As an example, we have studied the graded composites with cylindrical inclusions immersed in a homogeneous matrix. The thermal conductivity of the cylindrical inclusion is assumed to have a power-law profile of the radial distance r measured from its origin. For weakly nonlinear constitutive relations between the heat flow density q and the temperature field T, namely, q = -mu del T - chi vertical bar del T vertical bar(2) del T, in both the inclusion and the matrix regions, we have derived the temperature distributions using the perturbation expansion method. A nonlinear effective medium approximation of graded composites is proposed to estimate the effective linear and nonlinear thermal conductivities. by considering the temperature singularity on the inclusion surface due to the heat contact resistance. (c) 2006 Elsevier B.V. All rights reserved.

辽河盆地东部凹陷热历史及其与油气关系

This dissertation focuses on the basin geothermal history, tectonothermal evolution and the relationship between geothermal field evolution and hydrocarbon generation. Based on the research of present-day geothermal field, geothermal history of Eastern Subdepression of Liaohe Basin was reconstructed with available data from drillings, loggings, seismic cross-sections, BHTs and thermal indicators. 12 heat flow density values were calculated. Ranging from 45.7 mW/m~2 to 70.0 mW/m~2, the mean value of these determinations exhibits 58.0(±5.83mW/m~22). The heat flow density in the uplift and ramp is greater than that in the sag. The main factors affecting the heat flow density are the morphostructure of basement and thickness of sedimentary cover. The Subdepression experienced a much higher heat flow period from 43 Ma to about 25 Ma. The heat flow increased gradually from Sha3 stage to Dongying stage, and reached the peak at the late of Dongying stage, then cooled down. Structural subsidence analysis shows that the subsidence of Eastern Subdepression can be divided into two phases: earlier (25-43Ma) initial (rift) and late (since 25Ma) thermal subsidence. The lower present-day heat flow and the higher palaeo-heat flow corresponding to structural subsidence stage as well as the typical rift subsidence style in Eastern Subdepression provide with some insights to the tectonic-thermal evolution of the basin. The source rocks of Sha3 member began to generate oil in the Shal stage, and entered oil-window at the late of Dongying stage. The source rocks of Shal began to generate oil at the late of Dongying stage, and being at the stage of lower maturation-maturation now. Most of Dongying source rocks are not mature now. The late of Dongying stage is the critical time for the oil system.

Interferometric Measurement of Density in Nonstationary Shock Wave Reflection Flow and Comparison with CFD

We present density measurements from the application of interferometry and Fourier transform fringe analysis to the problem of nonstationary shock wave reflection over a semicircular cylinder and compare our experimental measurements to theoretical results from a CFD simulation of the same problem. The experimental results demonstrate our ability to resolve detailed structure in this complex shock wave reflection problem, allowing visualization of multiple shocks in the vicinity of the triple point, plus visualization of the shear layer and an associated vortical structure. Comparison between CFD and experiment show significant discrepancies with experiment producing a double Mach Reflection when CFD predicts a transitional Mach reflection.

Probing the high density behavior of the symmetry energy by using proton elliptic flow

Based on the isospin- and momentum-dependent transport model IBUU04, we calculated the reaction of the Sn-132+Sn-124 systems in semi-central collisions at beam energies of 400/A MeV, 600/A MeV and 800/A MeV by adopting two different density dependent symmetry energies. It was found that the proton differential elliptic flow as a function of transverse momentum is quite sensitive to the density dependence of symmetry energy, especially for the considered beam energy range. Therefore the proton differential elliptic flow may be considered as a robust probe for investigating the high density behavior of symmetry energy in intermediate energy heavy ion collisions.

Double neutron-proton differential transverse flow as a probe for the high density behavior of the nuclear symmetry energy

The double neutron-proton differential transverse flow taken from two reaction systems using different isotopes of the same element is studied at incident beam energies of 400 and 800 MeV/nucleon within the framework of an isospin- and momentum-dependent hadronic transport model IBUU04. The double differential flow is found to retain about the same sensitivity to the density dependence of the nuclear symmetry energy as the single differential flow in the more neutron-rich reaction. Because the double differential flow reduces significantly both the systematic errors and the influence of the Coulomb force, it is thus more effective probe for the high-density behavior of the nuclear symmetry energy.

Probing the high density behavior of the symmetry energy by using the neutron-proton differential flow

Based on the isospin- and momentum-dependent transport model IBUU04, we investigated the neutron-proton differential flow in the (132) Sn + (124) Sn mid-central collisions at beam energies of 400MeV/A, 600MeV/A and 800MeV/A by adopting two different symmetry energies. It was found that the neutron-proton differential flow as a function of rapidity is very sensitive to the density dependence of symmetry energy, especially at incident energies around 400MeV/A