Evaluation of the relationship between soil erosion and landscape metrics across Gorgan Watershed in northern Iran

Author(s):  
Fazlolah Ahmadi Mirghaed ◽  
Bubak Souri ◽  
Marjan Mohammadzadeh ◽  
Abdolrassoul Salmanmahiny ◽  
Seyed Hamed Mirkarimi
2020 ◽  
Vol 13 (1) ◽  
pp. 51
Author(s):  
Alexandra Pagáč Mokrá ◽  
Jakub Pagáč ◽  
Zlatica Muchová ◽  
František Petrovič

Water erosion is a phenomenon that significantly damages agricultural land. The current land fragmentation in Slovakia and the complete ambiguity of who owns it leads to a lack of responsibility to care for the land in its current condition, which could affect its sustainability in the future. The reason so much soil has eroded is obvious when looking at current land management, with large fields, a lack of windbreaks between them, and no barriers to prevent soil runoff. Land consolidation might be the solution. This paper seeks to evaluate redistributed land and, based on modeling by the Universal Soil Loss Equation (USLE) method, to assess the degree of soil erosion risk. Ownership data provided information on how many owners and what amount of area to consider, while taking into account new conditions regarding water erosion. The results indicate that 2488 plots of 1607 owners which represent 12% of the model area are still endangered by water erosion, even after the completion of the land consolidation project. The results also presented a way of evaluating the territory and aims to trigger a discussion regarding an unambiguous definition of responsibility in the relationship between owner and user.


Solid Earth ◽  
2017 ◽  
Vol 8 (3) ◽  
pp. 661-669 ◽  
Author(s):  
Yue Li ◽  
Xiao Yong Bai ◽  
Shi Jie Wang ◽  
Luo Yi Qin ◽  
Yi Chao Tian ◽  
...  

Abstract. Soil loss tolerance (T value) is one of the criteria in determining the necessity of erosion control measures and ecological restoration strategy. However, the validity of this criterion in subtropical karst regions is strongly disputed. In this study, T value is calculated based on soil formation rate by using a digital distribution map of carbonate rock assemblage types. Results indicated a spatial heterogeneity and diversity in soil loss tolerance. Instead of only one criterion, a minimum of three criteria should be considered when investigating the carbonate areas of southern China because the one region, one T value concept may not be applicable to this region. T value is proportionate to the amount of argillaceous material, which determines the surface soil thickness of the formations in homogenous carbonate rock areas. Homogenous carbonate rock, carbonate rock intercalated with clastic rock areas and carbonate/clastic rock alternation areas have T values of 20, 50 and 100 t/(km2 a), and they are extremely, severely and moderately sensitive to soil erosion. Karst rocky desertification (KRD) is defined as extreme soil erosion and reflects the risks of erosion. Thus, the relationship between T value and erosion risk is determined using KRD as a parameter. The existence of KRD land is unrelated to the T value, although this parameter indicates erosion sensitivity. Erosion risk is strongly dependent on the relationship between real soil loss (RL) and T value rather than on either erosion intensity or the T value itself. If RL > > T, then the erosion risk is high despite of a low RL. Conversely, if T > > RL, then the soil is safe although RL is high. Overall, these findings may clarify the heterogeneity of T value and its effect on erosion risk in a karst environment.


Iraq ◽  
2018 ◽  
Vol 80 ◽  
pp. 233-250
Author(s):  
Melissa Sharp ◽  
Kyra Kaercher

The Chalcolithic period in Mesopotamia and Iran (c.6000–4000 b.c.e.) is characterised by larger cities replacing small farming settlements, technological developments including wheel thrown pottery and copper metal working, and people establishing long distance trade networks. The Halaf horizon (5900–5100 b.c.e.) developed out of the local late pottery Neolithic tradition and is found throughout western Syria, southern Turkey, and northern and central Iraq. This archaeological culture is defined by a finely painted pottery, dryland farming, round and rectangular houses, and the use of stamp seals. A comparable ceramic horizon, the J-ware horizon (5200–4700 b.c.e.) arose in the Mahidasht and Kermanshah valleys of Iran. The J-ware ceramics are finely painted, possibly deriving from the Halaf tradition, but also slipped and burnished. The Rowanduz Archaeological Program's (RAP) excavations elucidate links between northern Iraq and northern Iran from the Chalcolithic to the modern period. This paper explores the relationship between the Halaf and J-ware traditions at Banahilk, recently re-excavated by RAP, and the larger contacts during the Chalcolithic.


2018 ◽  
Vol 2018 ◽  
pp. 1-6 ◽  
Author(s):  
O. Zargari ◽  
E. Kazemnezhad Leyli ◽  
S. Z. Azimi

Background. Psoriatic arthritis (PsA) results in an increased burden of psoriasis and impairs both quality of life and an individual’s functional capacity. The relationship between nail involvement and PsA in psoriasis is not fully characterized. Aim. To evaluate the frequency and characteristics of nail involvement in psoriatic patients and to assess the relationship with joint involvement. Methods. A total of 197 patients with moderate-to-severe psoriasis were consecutively invited to participate in this cross-sectional study. The patients are divided into two groups: those with and those without psoriatic arthritis. Results. 69.5% of psoriatic (137 out of 197) patients had nail involvement. The most common nail abnormality was onycholysis, followed by pitting and oil droplet changes. Nail involvement was more common in patients with psoriatic arthritis (82.1% versus 57.8%, p=0.001). Conclusion. Nail involvement is commonly associated with PsA. Onycholysis, splinter hemorrhage, and oil drop were significantly more common in the PsA group as opposed to patients with just skin findings. In general, psoriatic patients with arthritis had more severe disease.


2018 ◽  
Vol 46 (2) ◽  
pp. 553-562 ◽  
Author(s):  
Ataollah KAVIAN ◽  
Leila GHOLAMI ◽  
Maziar MOHAMMADI ◽  
Velibor SPALEVIC ◽  
Moghadeseh FALAH SORAKI

Soil erosion is one of the key challenges in soil and water conservation. Vegetation that covers soil and organic and inorganic mulch is very useful for the control of erosion processes. This study examined treatment with wheat residual (as agriculture mulch) on infiltration, time to runoff, runoff coefficient, sediment concentration and soil erosion processes. The study has been conducted for sandy-loam soil taken from summer rangeland (Northern Iran) with simulated rainfall intensities of 50 and 100 mm h-1. The experiment was conducted in slopes of 30% in three replications with two amounts of wheat residual of 50 and 90 %. The results showed that conservation percent of soil erosion for wheat residual 50 and 90% was 61.68 and 73.25%, respectively (in rainfall intensity of 50 mm h-1). Also, the conservation percent of soil erosion for wheat residual of 50 and 90% cover was 70.68 and 90.55, respectively (in rainfall intensity of 100 mm h-1). It was concluded that the conservation treatments could reduce runoff coefficient, sediment concentration and soil erosion and increase the time to runoff and infiltration coefficient. This effect was significant on time for infiltration, sediment concentration and soil erosion variables (R2=0.99), time to runoff and runoff coefficient variables (R2=0.95). The interaction effects of rainfall intensity and soil conservation was significant for sediment concentration and soil erosion variables (R2=0.99).


Land ◽  
2021 ◽  
Vol 10 (9) ◽  
pp. 990
Author(s):  
Yongfen Zhang ◽  
Nong Wang ◽  
Chongjun Tang ◽  
Shiqiang Zhang ◽  
Yuejun Song ◽  
...  

Landscape patterns are a result of the combined action of natural and social factors. Quantifying the relationships between landscape pattern changes, soil erosion, and sediment yield in river basins can provide regulators with a foundation for decision-making. Many studies have investigated how land-use changes and the resulting landscape patterns affect soil erosion in river basins. However, studies examining the effects of terrain, rainfall, soil erodibility, and vegetation cover factors on soil erosion and sediment yield from a landscape pattern perspective remain limited. In this paper, the upper Ganjiang Basin was used as the study area, and the amount of soil erosion and the amount of sediment yield in this basin were first simulated using a hydrological model. The simulated values were then validated. On this basis, new landscape metrics were established through the addition of factors from the revised universal soil loss equation to the land-use pattern. Five combinations of landscape metrics were chosen, and the interactions between the landscape metrics in each combination and their effects on soil erosion and sediment yield in the river basin were examined. The results showed that there were highly similar correlations between the area metrics, between the fragmentation metrics, between the spatial structure metrics, and between the evenness metrics across all the combinations, while the correlations between the shape metrics in Combination 1 (only land use in each year) differed notably from those in the other combinations. The new landscape indicator established based on Combination 4, which integrated the land-use pattern and the terrain, soil erodibility, and rainfall erosivity factors, were the most significantly correlated with the soil erosion and sediment yield of the river basin. Finally, partial least-squares regression models for the soil erosion and sediment yield of the river basin were established based on the five landscape metrics with the highest variable importance in projection scores selected from Combination 4. The results of this study provide a simple approach for quantitatively assessing soil erosion in other river basins for which detailed observation data are lacking.


2020 ◽  
Vol 21 (7) ◽  
pp. 271-282
Author(s):  
Seyed Akbar Javadi ◽  
Nosratollah layeghi ◽  
Mohamad Jafari ◽  
Hossein Arzani
Keyword(s):  
Land Use ◽  

F1000Research ◽  
2019 ◽  
Vol 7 ◽  
pp. 1523 ◽  
Author(s):  
Masato Oda ◽  
Burhanuddin Rasyid ◽  
Hide Omae

Crop residue incorporation increases stable soil pores and soil water infiltration and reduces surface water runoff and soil erosion. However, few studies have examined the relationship between crop residue incorporation and water infiltration. A previous study showed that water infiltration increases depending on the quantity of applied wheat straw. In this study, we examined whether the relationship is applicable to different crop residues in a crop rotation. We grew corn, rose grass, and okra in crop rotation under plastic film houses and measured the water infiltration rate at the time of ridge making. A strong correlation was found between the quantity of applied residue and the soil water infiltration rate (r = 0.953), although there are outliers in the case of no prior crop. However, aboveground biomass of the prior crop showed a stronger correlation with water infiltration rate (r = 0.965), without outliers. Previous studies have revealed the exponential relation between plant root mass and soil erosion. Our data also show a positive relationship between resistance to erosion and root mass when assuming that aboveground biomass is proportional to the underground biomass. The result also showed that the effect of the prior crop root mass disappears within the next crop period. Our results indicate that maintaining a large root biomass is crucial for reducing soil erosion.


Water ◽  
2021 ◽  
Vol 13 (16) ◽  
pp. 2190
Author(s):  
Fangfang Zhu ◽  
Yuchen Li ◽  
Jinhua Cheng

The particle size distribution characteristics of runoff sediments are vital for understanding the effect of the mechanism of soil erosion on slopes. The objective of this study was to investigate the particle-size distribution of sediments eroded from slopes covered by different litter coverage masses under artificial rainfall simulation. Litter was spread on the surface of a soil tank according to different biomasses (0 g·m−2, 100 g·m−2, 200 g·m−2 and 400 g·m−2). The mean weight diameter (MWD), fractal dimension (D) and enrichment ratio (ER) are characteristic parameters of sediment particle size. The MWD and D were more sensitive to soil erosion and had a significant negative correlation with the slope angle and rainfall intensity. The performance of the MWD on the slope (5°) was less than the MWD on the slope (10°). The relationship between eroded sediment distribution characteristic parameters and the litter coverage mass had a significant influence on the content of coarse particles. The content of fine particles accelerated, decreased and then stabilized, whereas coarse particles increased first and then stabilized. The litter diameter and surface area were the main parameters that affected the MWD and D. Under different rain intensities and slopes, the ER varied inconsistently with litter coverage mass. Coarse particles were eroded easily and selectively, and soil erosion had no sorting effect on fine particles. These findings support the quantitative study of the relationship between the amount of litter coverage mass and the particle size of soil sediments.


Author(s):  
Vance T. Holliday

Literally since they first set foot on the Earth’s surface, humans and their hominid ancestors have affected soils. The degree of effect humans have on soils varies from the most subtle, which could include simply walking across the soil, to the most dramatic, such as wholesale removal, mixing, or burial associated with urbanization. Butzer (1982, pp. 123–156) and Davidson (1982) present very useful summaries of the history and nature of such influence in a geoarchaeological context. Geoarchaeologists can be confronted with soils subjected to a wide degree of anthropogenic alteration. The detection of these alterations and their differential distribution can, in theory, be used to determine site boundaries, define stratigraphic relationships, delimit intrasite activity areas and features, and aid in their functional interpretation (Woods, 1984, p. 67). The primary challenge is detecting the human-induced alteration and then, of course, interpreting it. In a very broad sense, the detectability of human impact is roughly proportional to the degree of impact; that is, very subtle alterations are difficult or impossible to detect, but more substantial changes are more obvious. As in most other aspects of archaeology, interpreting the meaning of anthropogenic effects on soils is much more problematic. The study of human impacts on soils is one of the oldest applications of soil studies in archaeology, particularly in regions with a long history of significant human modification of the environment. The topic is also an important part of soil science and agriculture. As a result, there is a very large literature on the topic, especially for the Old World. There well may be more writing on this aspect of soils research in archaeology than on all others combined. The topic is of such interest because human impacts on soils can be so obvious and pervasive in archaeological contexts; recognizing human impacts is critical in sorting out artificial versus natural pedogenic and other geogenic processes; it provides another avenue of research into understanding the relationship between humans and their environment, especially the landscape; and it offers another means of getting at human behavior, either directly, as in studies of mound construction or agriculture, or more indirectly, as in studies of humaninduced soil erosion. Regardless, the subject has long been of interest in archaeology and geoarchaeology.


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