归一化植被指数与降水量、土壤湿度的关系   总被引：2，自引：0，他引：2  

普布次仁 《气象》1995,21(12):8-12

归一化植被指数是描述植被绿度及生长状况的指数，由于植被生长依赖于环境条件因此ＮＤＶＩ与环境参量的关系是应用ＮＤＶＩ监测环境状况的基础。分别应用位于中国北部的干旱及半干旱地区的降水量资料对ＮＤＶＩ与降水量之间的关系地分析，结果表明仅在干旱半干旱地区生长季末的累积降水量与累积ＮＤＶＩ存在着显著的非线性关系，相关系数为０．７８。  相似文献   

台湾费丛峡谷对强地面运动的影响研究──利用单台资料及2．5维SH混合方法     

温联星  姚振兴 《地球物理学报》1995,38(1):64-70

本文通过格林函数反褶积方法，由台湾峡谷附近的记录资料预测峡谷区的强地面运动的时程曲线．峡谷区的理论格林函数应用２．５维ＳＨ混合方法求解．通过格林函数反褶积方法得到的峡谷区费丛１及费丛２台的位移、速度、加速度和实际资料对比，取得了满意结果．计算结果表明，峡谷底部的峰值加速度相对峡谷边缘为最小；在靠近震中的一侧，峡谷的加速度的最大振幅相对比另一侧大．还给出了其余３个台的预测结果，研究了它们的加速度傅里叶谱和反应谱．  相似文献   

岩浆不混溶的物理化学条件—以河北阳原杂岩体为例     

侯增谦 《岩石矿物学杂志》1987,6(3):212-220

本文主要讨论了岩浆不混溶的内在因素和物化条件。研究提出阳原杂岩大于零的过剩自由能是出现不混溶的内在原因。岩浆中高P_2O_5、TiO_2、Zr、Hf、Ta、REE是岩浆不混溶的诱导因素。化学位计算揭示了球状黑云辉石正长岩之球体、基质两相及正长质和辉石质岩浆单元在液态时曾处于平衡状态。岩浆不混溶可能是在温度约1200℃、上地壳深度范围内发生的。阳原母岩浆不混溶的两液相可以分离聚集成两大岩浆单元,岩浆分溶不充分,便产生中间成分的黑云辉石正长岩。  相似文献   

动态聚类-模糊模式识别及其应用     

殷棣  贺国信 《铀矿地质》1987,(6)

本文以模糊子集论为指导,在迪戴的DCM法的基础上提出了动态聚类-模糊模式识别方法。实际上,它是一种新的模糊聚类的方法。该方法以DCM法的动态聚类部分做为原始数据变换的手段,而将迪戴的强模式概念推广为模糊模式,将强模式识别推广为模糊模式识别。此外,还提出了模糊模式间联系度的概念,从而解决了类间联系、类内典型个体、类间过渡个体、个体对各类的隶属程度以及内部有某种演化趋势的类别的划分等问题。文章还给出了该方法的数学模型和算法概要。最后,通过一个在地质学中的应用实例,说明了该方法的应用效果。  相似文献   

A comment on the continuity equation model of slope profile development and its boundary conditions     

Adrian C. Armstrong 《地球表面变化过程与地形》1982,7(3):283-284

The constant base boundary condition used by Kirkby to derive characteristic form solutions to the continuity equation are unlikely in practice. Constant form solutions relying on constant basal erosion are however more probable.  相似文献   

发展方程的非线性计算不稳定问题     

Ji Zhongzhen  Lin Wantao  Yang Xiaozhong 《大气科学进展》2001,18(3):397-403

进一步讨论了有关非线性不稳定的一些问题,其主要内容有： １．考察了有代表性的三类发展方程,指出其对应的差分格式是否出现非线性计算不稳定,与原微分方程解的性质密切相关。 ２．进一步讨论了带周期边条件的守恒型差分格式的非线性计算稳定性问题,总结了克服非线性不稳定的有效措施。 ３．以非线性平流方程为例,着重分析了带非周期边条件的非守恒差分格式的非线性计算稳定性问题,给出了判别其计算稳定性的“综合分析判别法”。  相似文献   

高表面活性矿物对Zn~(2+)的吸附机理及其环境意义     

吴平霄  廖宗文  毛小云 《矿物学报》2001,(3)

本文利用高表面活性矿物蒙脱石、蛭石、沸石在一定的介质条件下对Zn2 +进行吸附实验研究。蒙脱石和蛭石对Zn2 +的等温吸附线呈双“S”型 ,而沸石对Zn2 +的等温吸附线则呈“Langmuir”型。三种矿物对Zn2 +的吸附容量大小顺序为 :蒙脱石 >蛭石 >沸石。运用粉晶X射线衍射、红外光谱、差热及热重分析等技术对矿物及矿物吸附Zn2 +后的结构特征进行了研究。结果表明 ,蒙脱石吸附锌后其层间域中吸附锌大量水解形成新的物相 ,而蛭石与沸石吸附锌后水解很少。这为利用高表面活性矿物控制和治理环境污染及其可循环利用提供了理论依据。  相似文献   

Type Ia supernovae: An explosion in the regime of a convergent delayed detonation wave     

N. V. Dunina-Barkovskaya  V. S. Imshennik  S. I. Blinnikov 《Astronomy Letters》2001,27(6):353-362

The model of a presupernova’s carbon-oxygen (C-O) core with an initial mass of 1.33 M _⊙, an initial carbon abundance X _C ⁽⁰⁾ =0.27, and a mean rate of increase in mass of 5 × 10^?7 M _⊙ yr^?1 through accretion in a binary system evolved from the central density and temperature ρ_c=10⁹ g cm^?3 and T _c=2.05 × 10⁸K, respectively, by forming a convective core and its subsequent expansion to an explosive fuel ignition at the center. The evolution and explosion equations included only the carbon burning reaction ¹²C+¹²C with energy release corresponding to the complete conversion of carbon and oxygen (at the same rate as that of carbon) into ⁵⁶Ni. The ratio of mixing length to convection-zone size α_c was chosen as the parameter. Although the model assumptions were crude, we obtained an acceptable (for the theory of supernovae) pattern of explosion with a strong dependence of its duration on α_c. In our calculations with sufficiently large values of this parameter, α_c=4.0 × 10^?3 and 3.0×10^?3, fuel burned in the regime of prompt detonation. In the range 2.0×10^?3≥α_c≥3.0×10^?4, there was initially a deflagration with the generation of model pulsations whose amplitude gradually increased. Eventually, the detonation regime of burning arose, which was triggered from the model surface layers (with m ? 1.33 M _⊙) and propagated deep into the model up to the deflagration front. The generation of model pulsations and the formation of a detonation front are described in detail for α_c=1.0 × 10^?3.  相似文献   

On determining the noon polar cap boundary from SuperDARN HF radar backscatter characteristics     

M. Pinnock  A. S. Rodger 《Annales Geophysicae》2001,18(12):1523-1530

Previous work has shown that ionospheric HF radar backscatter in the noon sector can be used to locate the footprint of the magnetospheric cusp particle precipitation. This has enabled the radar data to be used as a proxy for the location of the polar cap boundary, and hence measure the flow of plasma across it to derive the reconnection electric field in the ionosphere. This work used only single radar data sets with a field of view limited to 2 h of local time. In this case study using four of the SuperDARN radars, we examine the boundary determined over 6 h of magnetic local time around the noon sector and its relationship to the convection pattern. The variation with longitude of the latitude of the radar scatter with cusp characteristics shows a bay-like feature. It is shown that this feature is shaped by the variation with longitude of the poleward flow component of the ionospheric plasma and may be understood in terms of cusp ion time-of-flight effects. Using this interpretation, we derive the time-of-flight of the cusp ions and find that it is consistent with approximately 1 keV ions injected from a subsolar reconnection site. A method for deriving a more accurate estimate of the location of the open-closed field line boundary from HF radar data is described.  相似文献   

90年代中国省级区域经济与环境协调度分析   总被引：131，自引：8，他引：123  

张晓东  池天河 《地理研究》2001,20(4):506-515

在阐述经济环境协调度理论的基础上,建立了环境承载力与经济发展水平之间的协调度模型。并通过对90年代我国省级区域的实证分析,发现我国空间区域经济环境协调度基本符合“U”型曲线,区域经济发展模式大多以牺牲环境为代价,特别是中西部地区的问题比较严重。  相似文献