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41.
ZHANG Hui-min JIANG Hui-ming 《中国地理科学(英文版)》2005,15(3):281-287
With the rapid development of agricultural informalization in the world, the demand of agricultural information has been a focus in the international agriculture and information fields. Based on the investigation, this paper presented the four characteristics of the demand of agricultural information in China, includingregionality, seasonality, great potential demand and variation in kind and level. The factors infuencing the demand of agricultural information were analyzed by the Optimized Less Square (OLS) method. The result shows that, of all factors influcing agricultural information demand, the most important one is economy, the second is facility of information pass, and knowledge and education of user, credit of agricultural information service system and production situation follow. Taking Jilin Province as an example, this article also elaborated the agricultural information demand status, and deduced the regression model of agricultural information demand and verified it by the survey in rural Jilin. 相似文献
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43.
From geometry to dynamics of microstructure: using boundary lengths to quantify boundary misorientations and anisotropy 总被引:1,自引:0,他引:1
John Wheeler Z. Jiang D. J. Prior J. Tullis M. R. Drury P. W. Trimby 《Tectonophysics》2003,376(1-2):19-35
The microstructure of a quartzite experimentally deformed and partially recrystallised at 900 °C, 1.2 GPa confining pressure and strain rate 10−6/s was investigated using orientation contrast and electron backscatter diffraction (EBSD). Boundaries between misoriented domains (grains or subgrains) were determined by image analysis of orientation contrast images. In each domain, EBSD measurements gave the complete quartz lattice orientation and enabled calculation of misorientation angles across every domain boundary. Results are analysed in terms of the boundary density, which for any range of misorientations is the boundary length for that range divided by image area. This allows a more direct comparison of misorientation statistics between different parts of a sample than does a treatment in terms of boundary number.The strain in the quartzite sample is heterogeneous. A 100×150 μm low-strain partially recrystallised subarea C was compared with a high-strain completely recrystallised subarea E. The density of high-angle (>10°) boundaries in E is roughly double that in C, reflecting the greater degree of recrystallisation. Low-angle boundaries in C and E are produced by subgrain rotation. In the low-angle range 0–10° boundary densities in both C and E show an exponential decrease with increasing misorientation. The densities scale with exp(−θ/λ) where λ is approximately 2° in C and 1° in E; in other words, E has a comparative dearth of boundaries in the 8–10° range. We explain this dearth in terms of mobile high-angle boundaries sweeping through and consuming low-angle boundaries as the latter increase misorientation through time. In E, the density of high-angle boundaries is larger than in C, so this sweeping would have been more efficient and could explain the relative paucity of 8–10° boundaries.The boundary density can be generalised to a directional property that gives the degree of anisotropy of the boundary network and its preferred orientation. Despite the imposed strain, the analysed samples show that boundaries are not, on average, strongly aligned. This is a function of the strong sinuosity of high-angle boundaries, caused by grain boundary migration. Low-angle boundaries might be expected, on average, to be aligned in relation to imposed strain but this is not found.Boundary densities and their generalisation in terms of directional properties provide objective measures of microstructure. In this study the patterns they show are interpreted in terms of combined subgrain rotation and migration recrystallisation, but it may be that other microstructural processes give distinctive patterns when analysed in this fashion. 相似文献
44.
This paper presents geochronological, geochemical, and isotopic data relating to Devonian magmatic activity in the Jiefangyingzi area, northern margin of the North China Plate (NCP). LA-ICP-MS zircon U–Pb dating indicates that the Erfendi granites formed in the Middle Devonian and yield a concordant weighted mean age of 384.7 ± 2.5 Ma. The zircons have negative εHf(t) values ranging from −5.8 to −31.3 and two-stage Hf-model ages of TDM2 = 1,735–3,217 Ma. 206Pb/238U ages of zircon grains from a quartz–schist sample in the Shaiwusu Formation vary from 410 to 322 Ma, with a peak at 380 Ma, indicating that magmatic activity peaked during the Late Devonian. The Erfendi granites are silica- and alkali-rich and calcium- and magnesium-poor. The Erfendi granites belong to peraluminous rocks and have clear negative Eu anomalies (δEu = 0.49–0.84); P, Ti, and Nb depletions; Nd, Zr, and U enrichments; and high Ga/Al ratios, similar to aluminous A-type granites. This suggests the Erfendi granites were generated by partial melting of lower crustal rocks. Geochemically, the Erfendi granites are A2-type granites, reflecting a post-collision tectonic setting. The southward subduction of the Palaeo-Asian Oceanic Plate during the Early Palaeozoic formed Bainaimiao volcanic arc at the northern NCP and Deyanqimiao island arc. The collision between the Deyanqimiao island arc and the Bainaimiao volcanic arc was recorded by the Xibiehe molasse deposition and the Badangshan volcanic rocks at the northern margin of the NCP during the Late Silurian to Early Devonian. As a consequence, the Jiefangyingzi area experienced intense post-collision extensional magmatism during the Middle Devonian, which generated massive A2-type granites at the northern margin of the NCP. This collision was also recorded by the back-arc deposition of the Late Carboniferous Shaiwusu Formation. 相似文献
45.
我国测绘成果长期存在坐标系统不统一的现状,使得不同坐标系测绘成果的使用存在一定的局限性,无法充分地利用测绘成果。本文以1∶10 000比例尺成果数据从西安80系到国家2000系转换为例,详细地介绍了基于FME软件零编程实现坐标系转换的方法。 相似文献
46.
47.
拟合推估新用——新逼近模式 总被引:4,自引:0,他引:4
作为拟合推估的新用之一,提出一种带有随机量的新逼近模式,将拟合推估的通行算法,去短取长,藉以推得良好的插值。 相似文献
48.
Zuo Jiahui Niu Fenglin Liu Lu Da Shuai Zhang Houzhu Yang Jidong Zhang Lele Zhao Yang 《Surveys in Geophysics》2022,43(3):673-701
Surveys in Geophysics - In 2D anisotropic media, non-stationary filters and low-rank approximation methods are classical strategies to compute the decomposition operators, but they suffer from... 相似文献
49.
Acta Geotechnica - Reactive magnesia (MgO)-activated ground granulated blast furnace slag (GGBS) is a newly developed binder for soil stabilization/solidification. It can be used as an alternative... 相似文献
50.
Spatial prediction of soil water content in karst area using prime terrain variables as auxiliary cokriging variable 总被引:1,自引:0,他引:1
In karst areas, accurately measuring and managing the spatial variability of soil water content (SWC) is very critical in settling numerous issues such as karst rocky desertification, ecosystem reconstruction, etc. In these areas, SWC exhibits strong spatial dependence, and it is a time and labor consuming procedure to measure its spatial variability. Therefore, estimation of this kind of soil property at an acceptable level of accuracy is of great significance. This study was conducted to evaluate and compare the spatial estimation of SWC by using ordinary kriging (OK) and cokriging (COK) methods with prime terrain variables, tending to predict SWC using limited available sample data for a 2,363.7 km2 study area in Mashan County, Guangxi Zhuang Autonomous Region, Southwest China. The measured SWC ranged from 3.36 to 26.69 %, with a mean of 17.34 %. The correlation analysis between SWC and prime terrain variables indicated that SWC showed significantly positive correlation with elevation (r is 0.46, P < 0.01), and significantly negative correlation with slope (r is ?0.30, P < 0.01); however, SWC was not significantly correlated with aspect in the study area. Therefore, elevation and slope were used as auxiliary data together for SWC prediction using COK method, and mean error (ME) and root mean square error were adopted to validate the prediction of SWC by these methods. Results indicated that COK with prime terrain variables data was superior to OK with relative improvement of 28.52 % in the case of limited available data, and also revealed that such elevation and slope data have the potential to improve the precision and reliability of SWC prediction as useful auxiliary variables. 相似文献