盘锦湿地芦苇叶片气孔导度的模拟   总被引：8，自引：0，他引：8       下载免费PDF全文

周莉  周广胜  贾庆宇  吕国红  谢艳兵  赵先丽 《气象与环境学报》2006,22(4):42-46

基于2005年5～9月盘锦湿地芦苇叶片气体交换观测数据,针对芦苇叶片气孔导度与光合速率以及光合速率与光合有效辐射之间的关系进行分析。结果表明:芦苇叶片气孔导度与光合速率的关系可应用Ball-Berry模型描述,光合速率与光合有效辐射的关系可应用非直角双曲线光合模型描述,联合Ball-Berry模型与非直角双曲线光合模型可通过环境变量求解叶片气孔导度。模型考虑了气孔导度与光合之间的相互作用。利用实验数据对气孔导度模型验证表明,叶片气孔导度模拟值和观测值回归方程的斜率为0.95,方程决定系数R=0.82(P<0.05)。  相似文献   

Electrical Struture of the Crust in Manas Earthquake Area,Xinjiang,China     

Zhao Guoze  Zhan Yan  Tang Ji  Zhao Junmeng  Jin Guangwen  Deng Qianhui  and Wang Jijun 《中国地震研究》2000,14(1):75-85

Magnetotelluric sounding data obtalned recently in Manas earthquake area were processed. Inthe result, curves of apparent resistivity, impedance Phase, skewness and optimum rotationangle versus period and the real magnetic induction vectors were obtained. Then the data ofall measuring points were interpreted by 2D automatic inversion. The result indicates thatalong the sounding profile the shallow crust can be divided into 5 segments and the deep crustcan be divided into 3 segments, with faults or deep-seated fault zones as the contactboundaries between them. The sedimentary cover along the profile extents down to depthabout 12 km in maximum and a low-resistivity body exists in the crust in southern section ofthe profile. The interpretation results are well consistent with geological and othergeophysical data. The Manas M7. 7 earthquake occurred near a contact zone where theelectrical structure of the crust sharply changes.  相似文献   

Electrical resistivity and 57Fe Mössbauer spectra of Fe-bearing calcic amphiboles     

E. Schmidbauer  Th. Kunzmann  Th. Fehr  R. Hochleitner 《Physics and Chemistry of Minerals》2000,27(5):347-356

Electrical resistivity and ⁵⁷Fe Mössbauer spectra are reported for three calcic amphiboles with different Fe concentrations. AC measurements (20?Hz–1?MHz) were performed, applying impedance spectroscopy between 100 and 785?°C in an N₂ gas atmosphere. It was found that up to three semiconducting charge transport processes can be distinguished, which in part changed slightly when several runs were carried out to higher temperatures. The extrapolated DC resistivity is much smaller for an amphibole with high Fe content than for the two with lower Fe concentrations. The derived activation energies are between ～0.48 and ～1.06?eV. For temperatures ≤600?°C the results are compatible with a charge transport mechanism due to electron hopping between Fe²⁺ and Fe³⁺. Above 600?°C, dehydrogenation and/or beginning amphibole decomposition obviously alter the conduction mechanism. From Mössbauer spectra it was established that in all amphibole samples Fe²⁺ and Fe³⁺ are simultaneously present. Mössbauer parameters were derived by fitting the observed spectra to models taking the occupation of various M sites into account.  相似文献   

Buried paleo-channels on the New Jersey continental margin: channel porosity structures from electromagnetic surveying     

Rob L. Evans  L. K. Law  B. St. Louis  S. Cheesman 《Marine Geology》2000,170(3-4):381-394

We report on a marine electromagnetic (EM) survey across two portions of the New Jersey continental margin that have been previously shown to contain buried paleo-channels. The EM method used provides bulk porosity estimates to depths of around 20 m below the seafloor and is thus able to place porosity constraints on the nature of the channel infill and the contrast in physical properties across the channel boundaries. Our data show that a key condition for the channels to have an electrical signature is that they incise an underlying regional unconformity, R, thought to represent a subaerially eroded surface, exposed during the late Wisconsinan glaciation. Channels that cut R are seen through increases in apparent porosity. Another seismically imaged channel sequence, which lies within the outer-shelf sediment wedge sequence above R, does not have an electrical signature, indicating that the sediments above and below the channel boundaries have similar physical properties.  相似文献   

视纵向电导成像方法在矿井地质灾害调查中的应用     

王文忠  刘继东 《中国煤炭地质》2008,20(2):57-60

在对甘肃省2005年度科研项目“电磁成像系统存煤矿地质探测中的应用研究”的研究过程中,提出一种提高电法勘探分辨率及解释精度的方法-视纵向电导成像方法。该方法在计算纵向电导微分的基础上．进行视纵向电导微分成像。为验证其微分成像的应用效果,设计了低阻薄层（H2=3m）与低阻厚层（H2=30m）2个3层地电模型（参数为：ρ1=ρ3=100Ω·m,ρ2=10Ω·m,H1=100m）。通过计算分析,可以看出：无论是低阻薄层还是低阻厚层,与其地电模型界面对应位置,视纵向电导曲线存在明显转折点,视纵向电导微分成像图则可看出明显电性差异,而常规视电阻率曲线却难以解释低阻薄层。利用该方法与常规解释结合,对陕西某矿区进行采空区探测,共圈出东、西两块采空区．后经钻探验证,采空区边界范同和展布形态基本和解释结果相吻合,但比较两种解释方法,常规解释的范围较视纵向电导微分成像解释的范围要大,可见新方法的解释结果更加可靠。  相似文献   

Investigation of a shallow alluvial aquifer using geoelectrical methods: a case from Turkey     

Gökhan Göktürkler  Çağlayan Balkaya  Zülfikar Erhan  Ayça Yurdakul 《Environmental Geology》2008,54(6):1283-1290

Near-surface geophysical methods are commonly used to solve a wide class of geological, engineering and environmental problems. In this study, a geoelectrical survey was performed to investigate an alluvial aquifer. The study area is located in the southwest of the Çubukluda? graben, situated in the south of ?zmir, Turkey. The geophysical studies included the electrical resistivity imaging and self-potential (SP) methods. The resistivity data were acquired along eight profiles in the northern part of the study area by a Wenner-Schlumberger electrode configuration and the data processing was achieved by a tomographic inversion technique. The SP data were collected by gradient technique along 16 profiles. Total field values were calculated for each profile by addition of the successive gradient values, then a total field SP map was obtained. The water-saturated zone in the northern part of the study area was clearly revealed by the electrical resistivity imaging and the SP survey yielded useful information on the subsurface fluid movement.  相似文献   

Evaluation of landfill disposal boundary by means of electrical resistivity imaging     

Vladimir Frid  Gady Liskevich  Dmitriy Doudkinski  Nikolay Korostishevsky 《Environmental Geology》2008,53(7):1503-1508

This paper deals with an employment of electrical resistivity imaging (ERI) for survey of leachate content on the waste disposal site in Northern Israel. The research consisted of conducting ten ERI lines and drilling investigation wells. Data simulation used a 2D EarthImager inversion program. Analysis of 2D ERI interpretation results shows that determination of the boundary between the landfill body bottom intensively saturated with leachates and underlying layers of highly water saturated fat nonconsolidated clays presents a challenge. However, statistical analysis of ERI data indicates that standard deviation and confidence interval of a set of resistivity data measured in the landfill body are significantly larger than those in underlying clays. Moreover, maximum changes of these parameters are found on the boundary between landfill body and underlying soil, thus reflecting natural differences in scattering of resistivity data measured in these two objects.  相似文献   

Combined analysis of electrical resistivity and geotechnical SPT blow counts for the safety assessment of fill dam   总被引：1，自引：0，他引：1  

Seokhoon Oh  Chang-Guk Sun 《Environmental Geology》2008,54(1):31-42

Electrical resistivity survey and the geotechnical SPT blow counts (N value) method were simultaneously analyzed to investigate the stability of a center-core type earth-fill dam against the seepage phenomenon. The coupling of these heterogeneous field methods provided a chance to understand the status of underground material by comparing the geophysical and geotechnical view. The analysis shows that the zones with low resistivity value generally have low N value, which means low stiffness. However, some zones with a high resistivity pattern are not accompanied by an increase of its N value, and are even showing a lower N value. These results imply that one should be careful to directly correlate resistivity value with the real status of the core material of a fill dam. And a highly resistive zone may be in poor status due to the effect of increase of resistivity value as a result of the piping condition. Additional laboratory tests show that there is a deficiency of fine soil particles believed as the clay at the troubled region, which means an increase in resistivity value. Therefore, multiple explorations should be planned to reduce the uncertainty in application of geophysical methods to dam safety evaluation in order to compensate the resistivity information of core material.  相似文献   

冬小麦冬季灌水适应性温度指标研究     

杨光仙  胡程达  彭记永 《气象与环境科学》2017,40(2):39-43

通过2011-2013年2个越冬期的盆栽试验,利用高低温(交变)湿热试验箱研究了不同最低温度下(-9℃、-6℃、-3℃和0℃)冬灌对冬小麦叶片理化性质、产量构成要素及产量的影响。结果表明,与最低温度为0℃的处理相比,在最低温度为-9℃和-6℃的处理造成了冬小麦叶绿素含量和气孔导度的大幅下降,可溶性糖含量大幅升高,差异均达显著(p0.01),灌水处理并没有带来明显的改善;而最低温度为-3℃时,叶绿素和可溶性糖含量总体上无明显差别,气孔导度则有一定程度的降低,差异显著(p0.05),冬灌导致其叶片叶绿素和可溶性糖含量分别有不同程度的升高和降低,具有明显的正效应。最低温度为0℃的处理,冬灌对冬小麦叶片叶绿素含量、可溶性糖含量及气孔导度等影响均有明显的正效应。从产量及其构成要素上看,-6℃与-9℃条件下,冬灌致使单株小穗数、穗粒数和穗粒重下降;-3℃和0℃条件下,冬灌提高了单株穗粒数和穗粒重。综上所述,最低温度在-6℃及以下不适合进行冬灌,而最低温度在-3℃及以上则适合。  相似文献   

油气电法勘探综述     

郑秀芬  李金铭 《地球物理学进展》1997,12(2):89-96

在直接找油气的物探方法中，电法作为一类重要的非地震地球物理方法，越来越受到人们的重视与关注。本文对其中几种主要的方法，如激发极化法、电场差分法和自然电场法等，从原理、发展概况和应用效果方面进行了简要论述。另外，对用来解决地质构造问题的非直接找油气的建场测探法、大地电磁法和可控源音频大地电磁法等，本文也作了扼要介绍。  相似文献