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1.
Spatial representation in the social interaction potential metric: an analysis of scale and parameter sensitivity 总被引：1，自引：1，他引：0
The social interaction potential (SIP) metric measures urban structural constraints on social interaction opportunities of a metropolitan region based on the time geographic concept of joint accessibility. Previous implementations of the metric used an interaction surface based on census tracts and the locations of their centroids. This has been shown to be a shortcoming, as the metric strongly depends on the scale of the zoning system in the region, making it difficult to compare the SIP metric between metropolitan regions. This research explores the role of spatial representation in the SIP metric and identifies a suitable grid-based representation that allows for comparison between regions while retaining cost-effectiveness with respect to computational burden. We also report on findings from an extensive sensitivity analysis investigating the SIP metric’s input parameters such as a travel flow congestion factor and the length of the allowable time budget for social activities. The results provide new insights on the role of the modifiable areal unit problem in the computation of time geographic measures of accessibility. 相似文献
2.
Yair Rinat Ari Matmon Maurice Arnold Georges Aumaître Didier Bourlès Karim Keddadouche Naomi Porat Efrat Morin Robert C. Finkel 《Quaternary Research》2014
Rockfall ages in tectonically active regions provide information regarding frequency and magnitude of earthquakes. In the hyper-arid environment of the Dead Sea fault (DSF), southern Israel, rockfalls are most probably triggered by earthquakes. We dated rockfalls along the western margin of the DSF using terrestrial cosmogenic nuclides (TCN). At each rockfall site, samples were collected from simultaneously exposed conjugate boulders and cliff surfaces. Such conjugate samples initially had identical pre-fall (“inherited”) TCN concentrations. After boulder detachment, these surfaces were dosed by different production rates due to differences in post-fall shielding and geometry. However, in our study area, pre-rockfall inheritance and post-rockfall production rates of TCN cannot be evaluated. Therefore, we developed a numerical approach and demonstrated a way to overcome the above-mentioned problems. This approach can be applied in other settings where rockfalls cannot be dated by simple exposure dating. Results suggest rockfall ages between 3.6 ± 0.8 and 4.7 ± 0.7 ka. OSL ages of sediment accumulated behind the boulders range between 0.6 ± 0.1 and 3.4 ± 1.4 ka and support the TCN results. Our ages agree with dated earthquakes determined in paleoseismic studies along the entire length of the DSF and support the observation of intensive earthquake activity around 4–5 ka. 相似文献
3.
Efrat Farber Ittai Gavrieli Thomas D. Bullen Ran Holtzman Uri Shavit 《Geochimica et cosmochimica acta》2004,68(9):1989-2006
The chemical and isotopic (87Sr/86Sr, δ11B, δ34Ssulfate, δ18Owater, δ15Nnitrate) compositions of water from the Lower Jordan River and its major tributaries between the Sea of Galilee and the Dead Sea were determined in order to reveal the origin of the salinity of the Jordan River. We identified three separate hydrological zones along the flow of the river:
- (1)
- A northern section (20 km downstream of its source) where the base flow composed of diverted saline and wastewaters is modified due to discharge of shallow sulfate-rich groundwater, characterized by low 87Sr/86Sr (0.7072), δ34Ssulfate (−2‰), high δ11B (∼36‰), δ15Nnitrate (∼15‰) and high δ18Owater (−2 to-3‰) values. The shallow groundwater is derived from agricultural drainage water mixed with natural saline groundwater and discharges to both the Jordan and Yarmouk rivers. The contribution of the groundwater component in the Jordan River flow, deduced from mixing relationships of solutes and strontium isotopes, varies from 20 to 50% of the total flow.
- (2)
- A central zone (20-50 km downstream from its source) where salt variations are minimal and the rise of 87Sr/86Sr and SO4/Cl ratios reflects predominance of eastern surface water flows.
- (3)
- A southern section (50-100 km downstream of its source) where the total dissolved solids of the Jordan River increase, particularly during the spring (70-80 km) and summer (80-100 km) to values as high as 11.1 g/L. Variations in the chemical and isotopic compositions of river water along the southern section suggest that the Zarqa River (87Sr/86Sr∼0.70865; δ11B∼25‰) has a negligible affect on the Jordan River. Instead, the river quality is influenced primarily by groundwater discharge composed of sulfate-rich saline groundwater (Cl-=31-180 mM; SO4/Cl∼0.2-0.5; Br/Cl∼2-3×10-3; 87Sr/86Sr∼0.70805; δ11B∼30‰; δ15Nnitrate ∼17‰, δ34Ssulfate=4-10‰), and Ca-chloride Rift valley brines (Cl-=846-1500 mM; Br/Cl∼6-8×10-3; 87Sr/86Sr∼0.7080; δ11B>40‰; δ34Ssulfate=4-10‰). Mixing calculations indicate that the groundwater discharged to the river is composed of varying proportions of brines and sulfate-rich saline groundwater. Solute mass balance calculations point to a ∼10% contribution of saline groundwater (Cl−=282 to 564 mM) to the river. A high nitrate level (up to 2.5 mM) in the groundwater suggests that drainage of wastewater derived irrigation water is an important source for the groundwater. This irrigation water appears to leach Pleistocene sediments of the Jordan Valley resulting in elevated sulfate contents and altered strontium and boron isotopic compositions of the groundwater that in turn impacts the water quality of the lower Jordan River.
4.
The spatial structure of a region is known to affect the degree of face-to-face interaction opportunities for a city’s residents. These interaction opportunities are important building blocks in aspects of economic production. To date, though, there is scant empirical evidence linking interaction opportunities to worker locations. In this article, using a spatial measure of social interaction potential (SIP), we seek to discover whether, and by how much, opportunities for interaction differ at home and work locations for workers within different industry and occupation groups in U.S. metropolitan areas. Based on the time-geographic concept of joint accessibility, SIP is sensitive to population and employment densities, as well as travel times associated with worker commutes in a region. We compare SIP at the census tract level of geography both within and between Metropolitan Statistical Areas (MSAs) nationally and test SIP distributions by occupation and industrial categories using nonparametric Kruskal–Wallis and Dunn tests. The study finds that several categories of higher skill and creative workers live and work in higher SIP areas. These findings provide evidence in support of theories of knowledge creation that rely on spontaneous face-to-face interaction and also indicate the effect of lifestyle preferences in location choices for highly skilled and arts workers. 相似文献
5.
Efrat E 《GeoJournal》1991,24(4):355-363
The State of Israel is facing now one of the most difficult absorption challenges it has ever had. About 250.000 Soviet-Jewish immigrants have arrived to the country since 1989 and another million are waiting in the Soviet Union for immigration. A direct absorption plan around an absorption basket of a few thousand dollar per family of three for the first year enables the immigrants to choose their place of habitation. They concentrate in big cities and veteran settlements along the coastal plain where employment possibilities are better. This trend is against the government's plans to direct them to peripheral regions. The current mass-immigration creates an unexpected change in the population and settlement pattern of Israel. 相似文献
6.
Elisha Efrat 《GeoJournal》1993,31(2):163-168
During the Gulf War Israel was divided into six alarm zones to enable the people to be released gradually from their shelters according to the rate of damage and danger which has been in the different regions. These zones were outlined superficially, neither according to basic geographical elements, nor to the ballistic behaviour of the Iraqi missiles. A modified division into ten alarm zones was announced in September 1992 following the blockade which the USA had laid on military aviation in southern Iraq. A different division of alarm zones, based on ballistic and geographical parameters is proposed should there be missile attacks on the country in the future. 相似文献
7.
Prof. Dr. Elisha Efrat 《GeoJournal》1977,1(4):41-46
Conclusions The industrialization of the development towns is one of the main factors in the creation of a modern productive economy in a new social environment. The proportion of Israel's large industrial plants that have been located in the developments town is much larger than the corresponding proportion of all the country's industries. The tendency to establish relatively large industries in the development towns will probably continue for a considerable time, and it will necessitate the chanelling of large government resources to the development regions.A more serious obstacle is the shortage of labour, and particularly of skilled labour. In contrast to the supply of capital, this difficulty cannot be solved by administrative decisions taken in accordance with an agreed economic policy. What is needed here is a revolution in vocational training, and a diversification in plant sizes, the smaller plants supplying services to the larger industries.Vocational education is one of the most important conditions for the success of the industrialization process in the development towns. Jews have no technological and industrial tradition, and when they established their state, they did not attach sufficient importance to the rapid training of a labour force that would be able to take its place in the new factories. In making up for this omission, it is important to avoid concentrating on the conservative and traditional trades, and attention should be paid to the needs of the newer and more sophisticated industries. 相似文献
8.
9.
Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response 总被引：1，自引：0，他引：1
Efrat Morin David C. Goodrich Robert A. Maddox Xiaogang Gao Hoshin V. Gupta Soroosh Sorooshian 《Advances in water resources》2006
Weather radar systems provide detailed information on spatial rainfall patterns known to play a significant role in runoff generation processes. In the current study, we present an innovative approach to exploit spatial rainfall information of air mass thunderstorms and link it with a watershed hydrological model. Observed radar data are decomposed into sets of rain cells conceptualized as circular Gaussian elements and the associated rain cell parameters, namely, location, maximal intensity and decay factor, are input into a hydrological model. Rain cells were retrieved from radar data for several thunderstorms over southern Arizona. Spatial characteristics of the resulting rain fields were evaluated using data from a dense rain gauge network. For an extreme case study in a semi-arid watershed, rain cells were derived and fed as input into a hydrological model to compute runoff response. A major factor in this event was found to be a single intense rain cell (out of the five cells decomposed from the storm). The path of this cell near watershed tributaries and toward the outlet enhanced generation of high flow. Furthermore, sensitivity analysis to cell characteristics indicated that peak discharge could be a factor of two higher if the cell was initiated just a few kilometers aside. 相似文献
10.
Elisha Efrat 《GeoJournal》1986,13(4):401-411
The objectives of the paper are to indicate, on a national and regional level, the areas of geographical inequality in Israel, which create economic and social gaps in the development of the country. Geographical inequality in this study has been analyzed through eleven different criteria, relevant to economic and social welfare situations, as: distance from the nearest big city, road accessibility, rate of population density, natural economic potential, spatial security, distance from the central plain and centers of economic activity, climatic index of discomfort, topography, oldness of the settlements in the surroundings, etc. Each element of inequality has been plotted on a map indicating its quantitative values,on the basis of square units, comprising 25 km2 each. A weighting of all the squares according to qualitative criteria enabled to prepare a comprehensive and compilative map with isolines showing the different spatial and inequality degrees.The map which has been elaborated from the data shows districts and localities in a range of different spatial degrees of deprivation. The history of settlement in Israel since the end of the 19th century, the planning guidelines since the establishment of the State in 1948, and the main geographic features of the country are the reasons of regional disparities. 相似文献