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251.
运用归一化光谱混合模型分析城市地表组成 总被引:7,自引:1,他引:7
运用归一化光谱混合分析(NSMA)方法,用ETM 数据调查广州市海珠区城市地表组成,采用亮度标准化方法减小亮度变化。通过标准化,使亮度差异在每个植被-非渗透性表面-土壤-水体(V-I-S-W)组成中减小或者消除,这样使得一个单一的端元能够代表一种地表组分。在此基础上,通过归一化影像,选择了植被、非渗透性表面、土壤和水体4种端元,运用一种约束光谱混合分析(SMA)模型,分解了不同种类的城市地表组成。通过与已有模型计算结果比较,认为本文所构建的模型较优,其对研究区非渗透性表面估计的均方根误差为12.6%。 相似文献
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253.
The characteristic of seismic coda wave attenuation in Yunnan area in 7 frequency-bands range from 1 Hz to 20 Hz was estimated by using the local earthquake's waveform data recorded from 22 Yunnan digital seismic stations.Coda attenuation Q-c1 of each station was firstly calculated by single scattering method. Then, mean free path Le and seismic albedo Bo of each station were calculated, and scattering attenuation Q-1s and intrinsic attenuation Q-1i were separated from total attenuation Q-1t by multiple lapse time window analysis based on the multiple scattering model in uniform random isotropic scattering medium. The attenuating characteristics in Yunnan show that most value of Le are in 10~30 km, with maximal within 2~6 Hz;Bo are about 0.5 at 1~2 Hz, but less than 0.5at other frequency-bands, which means Q-1i is comparable with Q-1s at 1~2 Hz, and after 1~2 Hz, Q-1i is greater than Q-1s and dominates the attenuation process. Q-1c is close to Q-1i at other frequency bands except 1~2 Hz.Results show that Q-1 especially Qs-1 varies spatially, Q-1 in eastern Yunnan zone is a bit higher than in northwestern Yunnan zone;northwestern Yunnan zone higher than southwestern Yunnan zone. Comparing with other results in global, Qs-1 in Yunnan is lower than the global average value among these results, Q-1i is higher than the global average value, and Q-1t lies the middle among these results. 相似文献
254.
Temporal-spatial variations of euphotic depth of typical lake regions in Lake Taihu and its ecological environmental significance 总被引:5,自引:0,他引:5
ZHANG Yunlin QIN Boqiang HU Weiping WANG Sumin CHEN Yuwei CHEN Weimin 《中国科学D辑(英文版)》2006,49(4):431-442
Euphotic depth can be defined as the portion of wa- ter column that supports the net primary productivity. Its lower end is the critical depth, namely, the depth measured when the daily net primary productivity is zero[1]. In the ecosystems of oceans, lakes and rivers, phytoplankton live in the euphotic depth and euphotic depth is usually taken as the lower boundary, when studying the primary productivity and biomass of phytoplankton; therefore the corresponding depth is sometimes called the t… 相似文献
255.
Extensive computer simulations aimed at testing a hypothesis that impact craters may explain the scaling behaviour of surface
spectra are presented. The simulations show that indeed crater effects alone may explain the spectral scaling of Mars’ topography
revealed from MOLA data. The range of the scaling exponents obtained for a wide range of simulation parameters does not exceed
the limits observed for Mars. The simulations suggest that the shape of large craters is the key factor leading to the two
scaling ranges in the surface spectra. Particular values of the scaling exponents may additionally depend on the depth-diameter
relationship and the crater size distribution. 相似文献
256.
Seismic Moment Tensor Resolution on a Local Scale: Simulated Rockburst and Mine-induced Seismic Events in the Kopanang Gold Mine, South Africa 总被引:2,自引:0,他引:2
Seismic records contain information about the effect of the source as well as the effect of wave propagation through the rock
mass. The effect of wave propagation is usually not well known as only simplified models of geological structures are available.
Therefore, the information about the source retrieved by inverting seismograms may include errors due to incomplete knowledge
of the rock mass along the propagation path, which in turn cause a distortion in the calculated moment tensor (MT). The distortion
of the MT on a local scale was observed by inverting records of a simulated rockburst conducted at the Kopanang gold mine
in South Africa. A dominant isotropic component of the explosive characteristics was found from the inversion. The deviatoric
components retrieved from the blast are spurious. A test of their stability indicated that they are not significant, assuming
an uncertainty above 5% for velocities and 10% for attenuation within the homogeneous model available for the mine. Thus,
the retrieval of the MT from records of local networks in mines using a homogeneous model of the rock mass seems to be feasible.
However, the homogeneous model of the rock mass can only be applied to close stations, within a few kilometers of the source.
The seismic records from distant stations were too complex to be modelled by a homogeneous rock mass. Records of six mine-induced
seismic events recorded at the Kopanang gold mine were also inverted. A vertical linear dipole along the pressure (P) axis
was found for three of the events, suggesting a pillar burst. The mechanism of two events contains an isotropic implosion
together with a nearly vertical dip-slip, and seems to indicate a combination of a cavity collapse with a down dip-slip along
a nearly vertical fault. One event corresponds to a dipole along the tensional (T) axis. However, it is vertical, thus its
association with tensile faulting of the hangingwall is uncertain. 相似文献
257.
258.
微物理过程分档处理的三维对流云模式研究 总被引:2,自引:0,他引:2
在三维完全弹性冰雹云参数化模式动力框架和二维面对称分档模式(微物理过程分档处理)的基础上,建立粒子全分档的三维对流云分档模式.利用建立的分档模式对2000年6月29日美国堪萨斯州的一次超级单体风暴进行了模拟,并将模拟结果与三维冰雹云参数化模式的模拟结果作了对比.结果表明:分档模式可以较好地模拟出强对流云中两支上升气流,模拟得到的最大上升气流速度大于参数化模式;分档模式模拟得到的雷达回波强度、顶高和回波宽度更接近实测. 相似文献
259.
260.
储集层孔隙度和电阻率曲线间微差形态波形的复杂程度隐含着储集层含油气性的信息,可以用混沌动力学系统加以刻划。油层相空间庞加莱截面明显具有自相似结构,呈现混沌特性;而水淹层和水层的相空间庞加莱截面显示,其混沌性呈显著减弱之势,系统趋于简单有序。其功率谱密度不论水淹程度如何,整体为一随频率增大其能量按指数递减连续频谱;随水淹程度逐渐减弱,递减幅度减小,整体能量逐渐降低,某些频率成分被吸收削弱,由光滑状逐渐演变成锯齿起伏状,其功率谱熵逐渐增大。基于测井信息的混沌特征和功率谱熵特征识别水淹层的方法,对利用传统测井解释理论判别比较困难的低阻油层有较强的识别能力。 相似文献