In a semi-arid region of Maadher, central Hodna (Algeria), groundwater is the main source for agricultural and domestic purposes. Anthropogenic activities and the presence of climate change’s effects have a significant impact on the region’s groundwater quality. This study’s goals were to use water quality indices to evaluate the groundwater’s quality and its suitability for drinking and irrigation, as well as to identify contaminated wells using a geographic information system (GIS) and the spatial interpolation techniques of ordinary kriging and inverse distance weighting (IDW). The results reveal that all water samples exceeded the World Health Organization’s standards for nitrate ions and had alarming concentrations of calcium, chlorine, and sulfate (WHO). According to Piper’s diagram, the groundwater hydrochemical facies is composed of the elements sulfate-chloride-nitrate-calcium (SO(4)(2-)-Cl(-)NO(3)(-)-Ca(2+) water type). The majority of samples fall into the poor water category, slightly more than 10% fall into the very poor water category, and less than 10% fall into the good to the excellent quality category, per the water quality indices, which classify samples in a similar manner. According to irrigation water indices, every sample is suitable for irrigation. Depending on the direction of groundwater flow, the spatial distributions of Ca(2+), Na(+), Mg(2+), SO(4)(2-), and Cl(-) show that their concentrations are high north of the area and relatively low south of Maadher village (Fig. 3). Nitrate concentrations are high in the majority of samples, particularly those close to the Bousaada wadi. In most samples, particularly those close to the Bousaada wadi, nitrate levels are high. Various water quality models were described, and GIS spatial distribution maps were created using standard kriging and inverse distance weighting (IDW) techniques through selected semi-variograms predicted against measurements. To determine the origin of mineralization and the chemical processes that take place in the aquifer-which include the precipitation and dissolution of dolomite, calcite, aragonite, gypsum, anhydrite, and halite-the groundwater saturation index was calculated.
BACKGROUND: Cutaneous leishmaniasis (CL) is a vector-borne disease prevalent in Algeria since 2000. The disease has significant impacts on affected communities, including morbidity and social stigma. OBJECTIVE: Investigate the association between environmental factors and the incidence of CL in the province of Ghardaïa and assess the predictive capacity of these factors for disease occurrence. DESIGN: Retrospective SETTING: The study area included both urban and rural communities. METHODS: We analyzed a dataset on CL in the province of Ghardaïa, Algeria, spanning from 2000 to 2020. The dataset included climatic variables such as temperature, average humidity, wind speed, rainfall, and the normalized difference vegetation index (NDVI). Using generalized additive models, we examined the relationships and interactions between these variables to predict the emergence of CL in the study area. MAIN OUTCOME MEASURES: The identification of the most significant environmental factors associated with the incidence and the predicted incidence rates of CL in the province of Ghardaïa, Algeria. SAMPLE SIZE AND CHARACTERISTICS: 252 monthly observations of both climatic and epidemiological variables. RESULTS: Relative humidity and wind speed were the primary climatic factors influencing the occurrence of CL epidemics in Ghardaïa, Algeria. Additionally, NDVI was a significant environmental factor associated with CL incidence. Surprisingly, temperature did not show a strong effect on CL occurrence, while rainfall was not statistically significant. The final fitted model predictions were highly correlated with real cases. CONCLUSION: This study provides a better understanding of the long-term trend in how environmental and climatic factors contribute to the emergence of CL. Our results can inform the development of effective early warning systems for preventing the transmission and emergence of vector-borne diseases. LIMITATIONS: Incorporating additional reservoir statistics such as rodent density and a human development index in the region could improve our understanding of disease transmission.
Flood mortality is a serious concern requiring a better understanding of risk factors and their reduction measures. To understand the specificities of flood mortality between developed and developing countries in a Mediterranean framework, we created an accurate database of 242 cases of death recorded in western Algeria and Calabria (southern Italy). This database covers a 33-year period (1990-2022) and includes the time and place of fatal accidents, victim characteristics, circumstances of death, and victim behavior. In order to highlight the people’s vulnerability, we have innovatively developed 13 mortality indices summarized in four complex indices: i) human, ii) physical, iii) environmental, and iv) circumstantial. The results revealed a decrease in high-mortality events and the annual amount of flood fatalities in both regions. The frequency of fatalities and the average number of deaths per year are higher in western Algeria, although the average number of fatalities per flood is practically the same. The flood mortality seasonality is similar oppositely to the spatial distribution. The assessment of mortality indices revealed similarities in vulnerability, except for the flood risk identification, rainfall and event death indices, which highlight the vulnerability of western Algeria, requiring prevention and protection actions suggested in this study. One of the research questions for future studies is to focus on the complex interaction between precipitation and basin-scale conditions, further strengthening the investigation into the role of victim behavior. Moreover, precise fine-tuning of proposed indices and their assessment procedure validation may lead to new practical recommendations for saving lives in future floods.
Drinking water provision has been a constant challenge in the Sahrawi refugee camps, located in the desert near Tindouf (Algeria). The drinking water supply system is itself divided in three zones which pump groundwater from different deep aquifers. It is equipped with reverse osmosis plants and chlorination systems for treating water. The allocation of water supplied to the Saharawi refugees for human consumption in 2016 has been estimated at between 14 and 17 L/person/day on average. This supplied water volume is below recommended standards, and also below the strategic objective of the Sahrawi government (20 L/person/day). Yet the local groundwater resources are huge in comparison with estimated consumption, and hence there is great potential for increasing the supplied volume through effecting improvements in the supply system. The physico-chemical quality of the raw and supplied water between 2006 and 2016 has been assessed according to Algerian standards for human consumption. The raw water of two zones of the supply system presents a very high conductivity and high concentrations of chloride, nitrate, fluoride, sulfate, sodium, calcium, potassium and iodide concentrations of natural origin, which may entail health risks. The treatment of water in a reverse osmosis plant greatly improves its quality and osmosed water met the standards. However, the supply of osmosed and raw water needs to be combined in Zone 1, to avoid an excessive reduction in water volume, and the supplied raw water poses a risk to the health of the refugees. The present study provides an example of a drinking water supply system under extreme drought conditions and in the political and social conditions of a refugee camp. Furthermore, it establishes a reference for supplied water allocation and quality in the Sahrawi refugee camps.
