基于遥感的漳平市杉松林地表可燃物负荷量估测     

陈芸芝  陈崇成  汪小钦  唐丽玉 《地球信息科学学报》2007,9(6):103-135

 杉木林和马尾松是分布于漳平市的两种易燃的可燃物类型。其可燃物负荷量的多少决定着林火行为。在利用ASTER计算杉木林小班平均植被覆盖度的基础上估算其郁闭度,通过与地面调查结果比较分析,校正已发生明显变化的小班郁闭度。根据已有估测方程,结合小班数据中的年龄、胸径和树高等因子对杉木地表可燃物负荷量进行了估测,据此对各杉木小班的燃烧性、燃烧强度及火险等级等因素进行初步评价。最后对漳平市另一易燃的可燃物马尾松类型开展地表可燃物负荷量估测及分析。  相似文献   

Eddy covariance measurements of carbon dioxide,latent and sensible energy fluxes above a meadow on a mountain slope     

Albin Hammerle  Alois Haslwanter  Michael Schmitt  Michael Bahn  Ulrike Tappeiner  Alexander Cernusca  Georg Wohlfahrt 《Boundary-Layer Meteorology》2007,122(2):397-416

Carbon dioxide, latent and sensible heat fluxes were measured by means of the eddy covariance method above a mountain meadow situated on a steep slope in the Stubai Valley in Austria, based on the hypothesis that, due to the low canopy height, measurements can be made in the shallow equilibrium layer where the wind field exhibits characteristics akin to level terrain. In order to test the validity of this hypothesis and to identify effects of complex terrain in the turbulence measurements, data were subjected to a rigorous testing procedure using a series of quality control measures established for surface-layer flows. The resulting high quality dataset comprised 36% of the original observations, the substantial reduction being mainly due to a change in surface roughness and associated fetch limitations in the wind sector dominating during nighttime and transition periods. The validity of the high quality dataset was further assessed by two independent tests: (i) a comparison with the net ecosystem carbon dioxide exchange measured by means of ecosystem chambers, and (ii) the ability of the eddy covariance measurements to close the energy balance. The net ecosystem CO₂ exchange measured by the eddy covariance method agreed reasonably well with ecosystem chamber measurements. The assessment of the energy balance closure showed that there was no significant difference in the correspondence between the meadow on the slope and another one situated on flat ground at the bottom of the Stubai Valley, available energy being underestimated by 28% and 29%, respectively. We thus conclude that, appropriate quality control provided, the eddy covariance measurements made above a mountain meadow on a steep slope are of similar quality as compared to flat terrain.  相似文献   

Assessing the potential for leaf-off LiDAR data to model canopy closure in temperate deciduous forests     

《ISPRS Journal of Photogrammetry and Remote Sensing》2014

Estimates of canopy closure have many important uses in forest management and ecological research. Field measurements, however, are typically not practical to acquire over expansive areas or for large numbers of locations. This problem has been addressed, in recent years, through the use of airborne light detection and ranging (LiDAR) technology which has proven effective in modeling canopy closure remotely. The techniques developed to use LiDAR for this purpose have been designed and evaluated for datasets acquired during leaf-on conditions. However, a large number of LiDAR datasets are acquired during leaf-off conditions since their primary purpose is to generate bare-earth Digital Elevation Models. In this paper, we develop and evaluate techniques for leveraging small-footprint leaf-off LiDAR data to model leaf-on canopy closure in temperate deciduous forests.We evaluate three techniques for modeling canopy closure: (1) the canopy-to-total-return-ratio (CTRR), (2) the canopy-to-total-pixel-ratio (CTPR), and (3) the hemispherical-viewshed (HV). The first technique has been used widely, in various forms, and has been shown to be effective with leaf-on LiDAR datasets. The CTRR technique that we tested uses the first-return LiDAR data only. The latter two techniques are new contributions that we develop and present in this paper. These techniques use Canopy Height Models (CHM) to detect significant gaps in the forest canopy which are of primary importance in estimating closure.The techniques we tested each showed good promise for predicting canopy closure using leaf-off LiDAR data with the CTPR and HV models having particularly high correlations with closure estimates from hemispherical photographs. The CTRR model had performance on par with results from previous studies that used leaf-on LiDAR, although, with leaf-off data the model tended to be negatively biased with respect to species having simple and compound leaf types and positively biased for coniferous species. The CTPR and HV models also showed some slight negative biases for compound-leaf species. The biases for the CTPR and HV models were mitigated when the CHM data were smoothed to fill in small gaps. The CHM-based models were robust to changes in the CHM model resolution which suggests that these methods may be applicable to a variety of small-footprint LiDAR datasets. In this research, the new CTPR and HV methods showed a strong ability to predict canopy closure using leaf-off data, however, future work will be needed to test the applicability of the models to variations in LiDAR datasets, forest types, and topography.  相似文献   

Numerical modeling of hydraulic fracture propagation,closure and reopening using XFEM with application to in‐situ stress estimation          下载免费PDF全文

T. Mohammadnejad  J.E. Andrade 《国际地质力学数值与分析法杂志》2016,40(15):2033-2060

In this paper, a fully coupled model is developed for numerical modeling of hydraulic fracturing in partially saturated weak porous formations using the extended finite element method, which provides an effective means to simulate the coupled hydro‐mechanical processes occurring during hydraulic fracturing. The developed model is for short fractures where plane strain assumptions are valid. The propagation of the hydraulic fracture is governed by the cohesive crack model, which accounts for crack closure and reopening. The developed model allows for fluid flow within the open part of the crack and crack face contact resulting from fracture closure. To prevent the unphysical crack face interpenetration during the closing mode, the crack face contact or self‐contact condition is enforced using the penalty method. Along the open part of the crack, the leakage flux through the crack faces is obtained directly as a part of the solution without introducing any simplifying assumption. If the crack undergoes the closing mode, zero leakage flux condition is imposed along the contact zone. An application of the developed model is shown in numerical modeling of pump‐in/shut‐in test. It is illustrated that the developed model is able to capture the salient features bottomhole pressure/time records exhibit and can extract the confining stress perpendicular to the direction of the hydraulic fracture propagation from the fracture closure pressure. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Characteristics of land surface heat and water exchange under different soil freeze/thaw conditions over the central Tibetan Plateau     

Donglin Guo  Meixue Yang  Huijun Wang 《水文研究》2011,25(16):2531-2541

Freezing and thawing processes at the soil surface play an important role in determining the nature of Tibetan land and atmosphere interactions. In this study, land surface water and heat exchanges under different freezing and thawing conditions over the central Tibetan Plateau were investigated using observations from the Coordinated Enhanced Observing Period/Asia‐Australia Monsoon Project on the Tibetan Plateau, and the Simultaneous Heat and Water Model. During the freezing and thawing stages, significant diurnal variation of soil temperature resulted in a diurnal cycle of unfrozen water content at the surface. Radiation and energy components and evapotranspiration averaged over four freeze/thaw stages also changed diurnally. On average, the surface albedo (0·68) during the completely frozen stage was sharply higher than those during the freezing, thawing, and completely thawed stages due to the snow cover. The Bowen ratios were 3·1 and 2·5 in the freezing and thawing stages, respectively, but the ratio was only 0·5 in the completely thawed stage. Latent heat flux displayed distinctly better correlation with unfrozen soil water content during the freezing and thawing stages than during the completely frozen and thawed stages. This implies that the diurnal cycle of unfrozen soil water, resulting from diurnal freeze/thaw cycles at the surface, has a significant impact on latent heat flux. A surface energy imbalance problem was encountered, and the possible sources of error were analysed. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

荒漠河岸柽柳(Tamarix chinensis)灌丛的能量平衡特征     

马虹  陈亚宁  李卫红 《中国沙漠》2014,34(1):108-117

用涡度相关法对新疆塔里木河下游荒漠河岸柽柳(Tamarix chinensis)灌丛进行了1个生长季的实验观测,利用同步气象资料探讨了干旱胁迫环境下柽柳灌丛的近地面微气象和能量平衡特征,并运用普通最小二乘法线性回归及能量平衡比率法对比分析了不同天气条件下柽柳的日能量平衡变化和分配的差异。结果表明:观测期内柽柳灌丛的能量平衡闭合率为72.3%,地表能量通量和能量分配特征呈明显的单峰型二次曲线,地表净辐射通量和潜热通量是柽柳灌丛生长季的主要能量收入项和支出项;生长季内柽柳灌丛的能量平衡残差出现系统性、正负交替的日循环规律;在不同天气条件下,能量的分配转化和平衡程度均有明显差异,晴天的能量闭合状况好于阴天、降雨及扬沙天气,白天好于夜间;能量平衡比率在日出前与日落后的变化显著,且出现瞬时能量过闭合现象。受光合作用的影响,能量平衡闭合程度及碳通量的变化与不同天气下的温度及水分密切相关。  相似文献   

基于TGO软件的GPS网同步环及异步环提取     

白铁勇  余代俊  付崇江 《测绘科学》2011,36(3):102-103,113

美国Trimble Geomatics Office(TGO)GPS数据处理软件被测绘工作者广泛使用,但因其对环闭合差的检核是用水平分量和垂直分量表达,不能按我国GPS规范,分别对同步环及异步环以三维坐标分量方式检验环闭合差,而给使用带来极大不便。本文提出利用TGO的环闭合差报告和数据交换文件中的有关信息解决此难题,用VB编写成TGO辅助程序加以实现,并与不同的软件进行比较分析,说明该程序可以应用于工程实践中。  相似文献   

⁴⁰Ar/³⁹Ar dating of a Late Proterozoic palaeomagnetic pole for the Armorican Massif (France)     

G. Ruffet  H. Perroud  G. Féraud 《Geophysical Journal International》1990,102(2):397-409

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U–Pb–Hf isotopes and trace elements of metasomatic zircon delimit the evolution of neoproterozoic Capané ophiolite in the southern Brasiliano Orogen     

Karine R. Arena  Léo A. Hartmann  Cristiano Lana 《International Geology Review》2018,60(7):911-928

The Capané ophiolite is a fragment of oceanic lithosphere obducted into the Ediacaran Porongos fold and thrust belt, southern Brasiliano Orogen. A studied rodingite blackwall contained in serpentinite has metasomatic zircon that displays multiple U–Pb ages from Tonian to Cryogenian (793 ± 0.9, 757 ± 2.1, 715 ± 2.2 Ma). The ages are interpreted as corresponding to multiple alteration events in the mantle. Multiple U–Pb–Hf isotopes and trace element analyses on the same crystals by laser ablation were controlled by backscatered electron images. Hf isotopes indicate zircon origin from a depleted mantle (εHf = +15 to +10.7), and trace elements point to an oceanic origin. The Capané ophiolite thus marks the evolution of the Adamastor ocean during the Tonian and Cryogenian, a significant result for the reconstruction of Rodinia and Gondwana supercontinents.  相似文献   

新疆准噶尔古生代洋盆闭合时限——来自卡拉麦里地区石炭纪碎屑锆石U-Pb年代学的约束   总被引：4，自引：0，他引：4  

白建科  陈隽璐  唐卓  张越 《地质通报》2018,37(1):26-38

新疆准噶尔古生代洋盆闭合时限对中亚造山带古生代构造格局及演化研究具有重要意义。东准噶尔卡拉麦里断裂带南缘广泛出露石炭纪陆相粗碎屑岩系,沉积相分析表明其形成于扇三角洲沉积环境。依据区域地层对比、岩石组合特征及地层接触关系,将其重新厘定为山梁砾石组。选择西段滴水泉和东段双井子2个地区的山梁砾石组剖面进行地层对比,并在2个剖面底部采集粗砂岩样品进行LA-ICP-MS锆石U-Pb年龄测定,获得最年轻的碎屑锆石年龄分别为349±4Ma和355±3Ma,代表山梁砾石组沉积时代晚于349Ma,应为早石炭世早期。碎屑锆石年龄分布特征及砾石成分表明,其物源主要来自断裂带北侧的泥盆纪火山岩。在分析前人资料的基础上,认为山梁砾石组碎屑岩系是卡拉麦里造山带强烈隆升造山过程的沉积学响应,形成于前陆盆地,限定了准噶尔古生代洋盆闭合时限在早石炭世早期之前。  相似文献