Identifying the determinants of access to agricultural credit in Southern Punjab of Pakistan

Based on the survey data of 250 farmers from the Multan district of Southern region of Punjab, Pakistan this study aims to empirically examine the determinants of access to agricultural credit. This study used the probit model to analyze the data. The results revealed that formal education, farm size, level of farm mechanization, farm revenue and landholding size positively and significantly influenced access to agricultural credit while the age of the farmer’s, distance, and off- farm income negatively and insignificantly influenced farmer’s accessibility to agricultural credit. The findings of the current study offer a policy guideline to streamline national policy on agricultural finance. This study also recommends that ZaraiTaraqiati Bank (ZTBL) and other Commercial Banks should improve their agricultural credit schemes to fulfil the diversified needs of small farm holders.

     

Extraction and analysis of geological lineaments by combining ASTER-GDEM and Landsat 8 image data in the central high atlas of Morocco

Natural Hazards - The present work focuses on using remote sensing techniques and geographical information system (GIS) to automatically extract lineaments in the southeast of Morocco, which is one...     

A geostatistical approach for assessing population exposure to NO2 in a complex urban area (Beirut,Lebanon)

Few studies in the Middle East region estimated the spatial distribution of air pollutants for exposure studies. This paper presents a geostatistical approach to assess background NO₂ spatial distribution and the associated exposed population in a Mediterranean city with a complex topography, Beirut. Such modeling gave an accurate mapping of the 2010 yearly background average value of NO₂: it varies between 35 and 67 μg m^?3 with a mean of 53 μg m^?3. The mean SD of the estimated error was about 3 μg m^?3. The results showed that the spatial distribution of NO₂ follows a nested structuring, with a major structure related to topoclimatic characteristics (interaction topography/atmospheric flow at large scale) and a minor one linked to micro-environment and micro-climatic characteristics (interactions urban morphology/atmospheric flows at fine scale). The probability for the city’s inhabitants to be exposed to NO₂ levels exceeding 40 μg m^?3 threshold limit set by the World Health Organization (WHO) showed that Beirut city has a real sanitary risk to the NO₂ pollution. 93 % of the population (around 358,459 people) is 100 % sure to be exposed to a yearly average exceeding 40 μg m^?3. This knowledge will be certainly useful for developing a tool for decision support in order to implement policies of reducing air pollution in Beirut, which is, given the results, very urgent.     

Spatio-temporal characteristics of aftershocks and seismogenic structure of the 2011 MW9.0 Tohoku earthquake,Japan

The Tohoku megathrust earthquake, which occurred on March 11, 2011 and had an epicenter that was 70 km east of Tohoku, Japan, resulted in an estimated ten's of billions of dollars in damage and a death toll of more than 15 thousand lives, yet few studies have documented key spatio-temporal seismogenic characteristics. Specifically, the temporal decay of aftershock activity, the number of strong aftershocks (with magnitudes greater than or equal to 7.0), the magnitude of the greatest aftershock, and area of possible aftershocks. Forecasted results from this study are based on Gutenberg-Richter's relation, Bath's law, Omori's law, and Well's relation of rupture scale utilizing the magnitude and statistical parameters of earthquakes in USA and China (Landers, Northridge, Hector Mine, San Simeon and Wenchuan earthquakes). The number of strong aftershocks, the parameters of Gutenberg-Richter's relation, and the modified form of Omori's law are confirmed based on the aftershock sequence data from the M_W9.0 Tohoku earthquake. Moreover, for a large earthquake, the seismogenic structure could be a fault, a fault system, or an intersection of several faults. The seismogenic structure of the earthquake suggests that the event occurred on a thrust fault near the Japan trench within the overriding plate that subsequently triggered three or more active faults producing large aftershocks.     

Role of women as risk communicators to enhance disaster resilience of Bandung,Indonesia

This study addresses the need for women risk communication and highlights the potential role of Women Welfare Associations (WWAs) of Bandung, Indonesia, as risk communicators. A risk communication framework is modeled for women’s risk communication process. A set of indicators in social, institutional, and economic resilience activities (SIERAs), with a scope of 45 activities covering three different disaster periods, were developed to characterize the delivery process of risk information by women in WWAs through their activities at sub-district and ward levels. The data were collected through a questionnaire survey method using the risk communication SIERA approach. Women’s leaders at wards were surveyed concerning their perceptions on these 45 scopes of SIERA, ongoing activities, and their risk information source and dissemination process. Correlation analysis was applied to determine the relationship between the variables such as periods of disaster, types of activities (social, institutional, economic), and attributing factors (location, population, and education institution) in finding variations in risk communication activity that functions for women and communities. Five risk communication processes of WWAs are identified and implemented that work for women in Bandung. When their perceptions and ongoing activities are compared, activities such as dissemination of disaster risk information, conveying early warnings to their peers, and involvement of the local government have been confirmed to match the risk communication plans and implementation of WWAs. These indicate that WWAs’ activities in Bandung implement a certain degree of risk communication that is embedded in their activities. The results confirm that women through their social networks can become active agents of change and thus act beyond their usual domestic roles and responsibilities in order to contribute to the overall enhancement of community resilience.

     

Sources of groundwater recharge at the confluence of the Niles, Sudan

 Due to the rapid expansion of the Sudanese capital city far away from its three Niles, it has become a necessity to estimate the sustainability of the groundwater resources in this arid area. The purpose of this study – based on the stable-isotopic composition of groundwater – is to identify the sources of recharge and their relative contribution. The results show that groundwater infiltrated from the Niles under the present prevailing arid climate, with greater contribution from the White Nile compared to the Blue Nile, occupies an extension of 12 km from the Niles within the two main aquifers. Paleogroundwater of meteoric origin, infiltrated in the cooler pluvial earlier Holocene, occupies the outer zones beyond the Niles' effect. A rational utilization policy is recommended to preserve the finite groundwater resources. Received: 27 August 1998 · Accepted: 2 March 1999     

GeoVisuals: a visual analytics approach to leverage the potential of spatial videos and associated geonarratives

ABSTRACT

Videos embedded with spatial coordinates, especially when combined with additional expert insights, offer the potential to acquire fine-scale multi-time period contextualized data for a variety of different environments. However, while these geospatial multimedia (GSMM) data include abundant spatiotemporal, semantic and visual information, the means to fully leverage their potential using a suite of visual and interactive analysis techniques and tools has thus far been lacking. In this paper, we address this gap by first identifying the types of tasks required of GSMM data, and then presenting a solution platform. This GeoVisuals system utilizes a visual analysis approach built on semantic data points that can be integrated spatially, which in turn enables management in a unified database with combined spatio-temporal and text querying. A set of visualization functions are integrated in two investigation modes: geo-video analysis and geo-location analysis.     

Geochemical mass balance and weathering rates of ultramafic schists in Amazonia

The hydrochemical balance of the Yaou catchment in French Guiana was determined over a period of 1 year, combined with a detailed characterization of the primary minerals and their weathering products, in order to estimate ultramafic rock weathering rates in a rainforest environment. The time required to develop the main horizons of the laterite profile was obtained from estimations of the weathering rates and dissolution kinetics of some major parent minerals (chlorite, serpentine, biotite, calcite).

The specific transport of solute matter in the catchment is 205 kg/ha/a. The Cl and NO₃ net outputs shows that the system is in dynamic equilibrium, notably with respect to the biomass reservoir. The output flux of Mg in solution is mainly supplied from the weathering of primary minerals, whereas that of Ca comes both from atmospheric contributions and from the dissolution of carbonates. The fluxes of K and, more particularly, Na derive essentially from the atmosphere. Knowing the weathering rate of primary minerals, the total CO₂ consumption rate by silicate weathering is estimated at 1430 mol/ha/a.

The weathering rates of chlorite, serpentine and biotite range from 18 to 65 mol/ha/a, and those of talc and calcite are, respectively 51 and 153 mol/ha/a. Weathering rates normalized to mineral modal proportions give a decreasing order of stability resistance to weathering (calcitebiotitechlorite>serpentine>talc) that agrees with their vertical distribution in the weathering profile. The dissolution kinetics of chlorite, biotite and serpentine, expressed in relation to the Si release rate, were calculated using estimations of the mineral exchange surface by (a) optical microscope image processing of crystal outlines, and (b) BET specific surface measurements. The release rate of Si, computed for biotite, chlorite and serpentine, ranges around 10⁻¹³ and 10⁻¹⁴ mol/m²/s using microscope images on particle sizes. The estimated dissolution kinetics is two orders of magnitude lower when using the BET measured exchange surface, which is 100 times larger.

The saprolitization rate, calculated from the weathering rates of calcite, chlorite and biotite, is on average 7.5 m/Ma. The rate of latosol development, calculated from the weathering rate of serpentine at the saprolite–latosol interface, is estimated at 4.5 m/Ma. That means that the profile is chemically thickening at a rate of 3 m/Ma.