H. Beigi Harchegani, S. S. Heshmati,
Volume 18, Issue 67 (6-2014)
Abstract
Shahrekord groundwater is the main source of water for drinking, and the agricultural and industrial activities of its
inhabitants. Water quality measures of scaling and corrosion can deteriorate steel-based systems used for storage or
supplying water for drinking and to industry and irrigation. The main aim of this study was to assess the spatial
variability and mapping of scaling and corrosion using Langelier index (LI) and Ryznar index (RI) and that of the
related parameters of pH, total dissolved solids (TDS), total hardness (TH), and total alkalinity (TA) in Shahrekord
groundwater. For this purpose, water samples from 97 wells were analyzed for pH, TDS, TH, and TA and LI and RI
indices were calculated. The Gaussian model best described the spatial variability of TDS while the Spherical model
was best for all other parameters. Based on LI and RI averages of, -0.13 and 7.9 respectively, Shahrekord groundwater
has a slight potential for corrosion. The values of all parameters, except RI, were lowest in the northwest and highest in
the southeast of the aquifer. In most parts and in the center of the aquifer, the values of LI ranged from -0.5 to zero
indicating negligible scaling potential. Spatial distribution of the RI index was almost inversely symmetrical to that of
LI index. LI showed strong positive correlations with its components (varying from 0.61 to 0.90) while RI had strong
negative correlations with its components (ranging from -0.66 to -0.98). LI and RI had the strongest correlations,
respectively, with pH (r=0.90) and total alkalinity (r=-0.90).
B. Khalili Moghadam, Z. Ghorbani, E. Shahbazi,
Volume 18, Issue 69 (12-2014)
Abstract
Salt with various kinds and contents is one of the most important factors affecting soil splash erosion rate. The aim of the present study was to evaluate various salinity and alkalinity levels on splash erosion rate and its components (upslope, down slope and total splash) in different slopes. A factorial experiment with three factors was conducted in a completely randomized design with three replications by a Multiple Splash Set (MSS). The treatments included splash erosion rate at 4 levels of salinity and alkalinity (EC: 2 dSm-1, SAR: 2، EC: 15, SAR: 24 ،EC: 56, SAR: 42، EC: 113, SAR: 47), two levels of rainfall intensity (2.5 and 3.5 mm.min-1) and 5% and 15% slope levels. The results showed that the organic carbon and mean weight diameter (MWD) decreased at higher levels of salinity and alkalinity. The effect of saline and sodic, slope and rainfall intensity levels on the splash erosion rate and its components was significant. Also, slope×saline and sodic, rainfall intensity×saline and sodic, slope×saline and sodic×rainfall intensity interaction treatment caused a significant increase in splash erosion rate and its components. It seems that splash erosion is increased in saline and sodic soils due to the reduction in OC and MWD
