چكيده لاتين :
1- Introduction
Various factors influence the karstification process in the dissolution of carbonate rocks.
Karst is common influence result of internal morphodynamics (geological structure and
lithology) and external morphodynamics (climate, altitude, vegetation, and time). They affect
the karstification of the demise of carbonate rocks. Karst is the result of numerous methods that
occur in calcareous zones and climatic, geological, and hydrological conditions, and its effects
can be seen in multiple forms, such as pits and caves above and below ground. One of the
climate indices that determines the environmental conditions is the amount of moisture and its
changes. The presence of water is a significant climate factor in karst development. They
reflected in the formation of the environment in several Forming systems: in the high
elevations and latitudes as glacier systems, in the piedmont as ice sheet systems, in the
marginal zone as ice tab and mudflat systems, in the lower zones as runoff and in the smaller
pit as waterfall system (Seif et al., 2015). The solubility of carbonate rocks is sensitive to
temperature changes (Ghobadi, 2009: 142); Limestone dissolution is more rapid at low
temperatures and in colder climates, and the amount of karst erosion in cold and humid regions
is much higher than in hot and humid regions (Zanganeh Asadi et al., 2002). With the impact
of elevation on temperature and precipitation, erosion processes and consequently the face of
the Earth and geomorphological phenomenon change (Alipour et al., 2017). The purpose of
this paper is to investigate the physiographic differences of calcareous Zagros sub-basins
concerning altitude variation and the interpretation of disagreements concerning temperature
and precipitation elements.
2- Methodology
In this paper, considering the karst features and the effect of dissolution on the basin in
terms of physiographic properties (shape parameters), slope, roughness (topographic
parameters) in the Arc Map, the basins of the rivers that were located in the calcareous zones
were determined. The settings of such as environment, basin area, and rivers length, minimum
and maximum height were calculated. The shape and topographic parameters of the basins
were estimated, by using the existing relationships, and then the final rank of the basin's main
waterway was obtained based on the Australian method. The collected data were entered into
Excel software. Finally, linear regression equations between altitude as the independent
variable and other parameters as the dependent variables were estimated to investigate their
variation concerning the altitude factor. They were also studied in elevation classes, different
climatic zones, and distance to the fault.
3- Results
Investigation of the estimated linear regression relation between height as an independent
variable and other parameters as a dependent variable at different ranks indicates that with
increasing elevation, area, roughness coefficient, length, elongation ratio, and basin shape
factor become less and form element lower. Increasing the area of sub-basins at ranks similar
to elevation implies that surface erosion overcomes linear erosion. When corrosion is direct,
the intermediates are usually less extensive, and the basins are consequently getting smaller.
However, the sub-basin area increases due to elevation in single lithology, and as in similar
waterways. Due to the karst-fission effect on basin dimensions and their influence on climatic
elements, the sub-basin area has grown and increased the area of the sub-basin has made the
erosion from the line (water) to surface (dissolution) more inclined. In 297 sub-basins with
rank 2 and 3 northwest Zagros, there was no significant relationship between altitudes with
other parameters except ruggedness. That is, their coefficient of explanation was less than 0.4,
and it could not be analyzed solely by the height factor. Examination of these parameters
indicates that their changes, sometimes with increasing altitude, are minor and occasionally
unanticipated and sometimes have no specific direction. As the river rises, the area of the subbasins
also increases. We identified in the southeastern part of the folded Zagros, 48 basins. In
each rank basin, there is a direct correlation between height and other parameters. It means that
all of them are affected by altitude. They increase with the coefficient of all of them, except the
form factor, it has grown. In low Zagros, 68 catchments in calcareous zones, with ranks two to
four, it was considered that the regression relationships between altitude and parameters except
the form factor had a direct correlation with the difference that this unit had higher correlation
coefficient than the other Zagros units.
4- Discussion & Conclusions
The physiographic coefficients of the basins in the calcareous zones, the change in
temperature and precipitation due to elevation changed. The transformations of karstification
can analyze the change in temperature and precipitation — these changes reflected in different
parts of Zagros (except for the folded northwest Zagros). The increasing of the coefficient of
explanation in low altitude Zagro indicates that due to the physiographic characteristics of the
basins, the role of climate change (temperature and precipitation) in this part of Zagros can be
better traced. The examining factor such as basin physiography due to the increase of altitude
shows that the elongation and length of the sub-basins increase with increasing. and it is
reflected almost like the basin drag coefficient. Erosion at the basin surface may have a
homogeneous or heterogeneous distribution. If the coefficient of roughness is high, it indicates
that the distribution of decay has become seamless. In calcareous regions, as the altitude
increases, the ratio of hardness increases too because the distribution of erosion becomes
heterogeneous. Investigation of the physiographic characteristics of the watersheds concerning
altitude shows that the elongation and length of the basins increase with increasing Zagros with
an explanation coefficient of 0.5. The results show that increasing the coefficient of elongation
and length of the basin in calcareous zones lead to more dissolution, and the form factor, with a
ratio of explanation of 0.53 for the whole Zagros indicate the geometric shape of the basin to
square and rectangle. It almost reflects results similar to the basin drag coefficient. In
calcareous areas, as the altitude increases, the coefficient of roughness increases by an average
of 0.6% due to heterogeneous surface erosion.
Morphometric study of Zagros calcareous sub-basins about climatic factors indicates that
several factors affect these properties, only some of which are related to dissolution conditions;
Crashes, landslides, topography, faults, seams and crevices, and any other factors can affect
these properties that may be addressed in separate studies.
