Effects of soil erosion on soil quality in rocky mountain areas of northern China

2011 ◽  
Author(s):  
Mingli Zhang ◽  
Wenjing Cui ◽  
Hao Yang
Keyword(s):  
Soil Erosion ◽  
Soil Quality ◽  
Rocky Mountain ◽  
Northern China ◽  
Mountain Areas

Causes and its Impacts of Soil Erosion in the Rocky Mountain Area of Northern China

2013 ◽  
Vol 726-731 ◽  
pp. 3807-3810
Author(s):  
Zi Jun Li ◽  
Qiao Qin Liu
Keyword(s):  
Soil Erosion ◽  
Water Conservation ◽  
Land Surface ◽  
Rocky Mountain ◽  
Northern China ◽  
Land Utilization ◽  
Rocky Desertification ◽  
Mountain Area ◽  
Slope Farmland ◽  
Ecological Construction

Soil erosion has been the most prominent issue in Chinas ecological environment. The rocky mountain area of Northern China is an important typical area of soil erosion and one of the most dangerous regions of potential erosion in China characterized by more stones in thinner soils and the land surface is easily reduced to sand gravel or rocky desertification. Concentrated rainfall with frequent rainstorms, broken topography with steep slope and highly dense gully are important natural factors resulting in soil erosion. However, unreasonable land utilization especially slope farmland aggravates soil erosion. Soil erosion results in land degradation, threatens regional water resources security, intensifies regional poverty and restricts socio-economic development. Sloping cultivated land transformation will be the necessary choice for soil and water conservation and ecological construction in this region.

scholarly journals Effect of Forest Management Operations on Aggregate-Associated SOC Dynamics Using a 137Cs Tracing Method

Forests ◽  
2021 ◽  
Vol 12 (7) ◽  
pp. 859
Author(s):  
Geng Guo ◽  
Xiao Li ◽  
Xi Zhu ◽  
Yanyin Xu ◽  
Qiao Dai ◽  
...  
Keyword(s):  
Forest Management ◽  
Soil Erosion ◽  
Management Practices ◽  
Negative Impact ◽  
Dynamic Change ◽  
Aggregate Size ◽  
Nutrient Loss ◽  
Vegetation Coverage ◽  
Forest Conversion ◽  
Mountain Areas

Although forest conversions have long been a focus in carbon (C) research, the relationship between soil erosion and the dynamic change of soil organic carbon (SOC) has not been well-quantified. The objective of this study was to investigate the effects of converting CBF (coniferous and broad-leaved mixed forests) to economic forests, including CF (chestnut forest), HF (hawthorn forest), and AF (apple forest), on the soil structure and nutrient loss in the Huaibei Rocky Mountain Areas, China. A 137Cs tracer method was used to provide soil erosion data in order to quantify the loss of aggregate-associated SOC. The results showed that forest management operations caused macro-aggregates to decrease by 1.69% in CF, 4.52% in AF, and 3.87% in HF. Therefore, the stability of aggregates was reduced. The SOC contents in each aggregate size decreased significantly after forest conversion, with the largest decreases occurring in AF. We quantified the loss of 0.15, 0.38, and 0.31 Mg hm−2 of aggregate-associated SOC after conversion from CBF to CF, AF, and HF, respectively. These results suggest that forest management operations have a negative impact on soil quality and fertility. CF has better vegetation coverage and less human interference, making it more prominent among the three economic forests species. Therefore, when developing forest management operations, judicious selection of tree varieties and appropriate management practices are extremely critical. In addition, measures should be taken to increase surface cover to reduce soil erosion and achieve sustainable development of economic forests.

Soils

2019 ◽  
pp. 67-90
Author(s):  
Nicola P. Randall ◽  
Barbara Smith
Keyword(s):  
Soil Erosion ◽  
Soil Quality ◽  
Agricultural Practices ◽  
Soil Formation ◽  
Soil Biology ◽  
Soil Processes ◽  
Soil Biodiversity ◽  
Productive Land ◽  
And Function ◽  
Agriculture And Food

This chapter gives a basic introduction to soil formation and fundamental soil processes in agroecosystems. The types of soils found in agroecosystems and their importance for agriculture is explored, with a principal focus on soil biodiversity, i.e. soil-dwelling organisms, their variety and function, and the interaction between soil biology, agriculture, and food production. The chapter describes some of the issues associated with soils in agroecosystems. These include interactions between agricultural practices and soil erosion and soil quality issues such as salinization and desertification. The major challenges to maintaining ‘healthy’ soils on productive land are outlined, and approaches and techniques for managing soils described.

scholarly journals Estimation of soil redistribution rates due to snow cover related processes in a mountainous area (Valle d'Aosta, NW Italy)

2012 ◽  
Vol 16 (2) ◽  
pp. 517-528 ◽  
Author(s):  
E. Ceaglio ◽  
K. Meusburger ◽  
M. Freppaz ◽  
E. Zanini ◽  
C. Alewell
Keyword(s):  
Soil Erosion ◽  
Sediment Yield ◽  
Mountainous Area ◽  
Mountain Areas ◽  
Spatial And Temporal Scales ◽  
Erosion Rates ◽  
Soil Redistribution ◽  
Erosion Processes ◽  
Soil Accumulation ◽  
Snow Gliding

Abstract. Mountain areas are widely affected by soil erosion, which is generally linked to runoff processes occurring in the growing season and snowmelt period. Also processes like snow gliding and full-depth snow avalanches may be important factors that can enhance soil erosion, however the role and importance of snow movements as agents of soil redistribution are not well understood yet. The aim of this study was to provide information on the relative importance of snow related processes in comparison to runoff processes. In the study area, which is an avalanche path characterized by intense snow movements, soil redistribution rates were quantified with two methods: (i) by field measurements of sediment yield in an avalanche deposition area during 2009 and 2010 winter seasons; (ii) by caesium-137 method, which supplies the cumulative net soil loss/gain since 1986, including all the soil erosion processes. The snow related soil accumulation estimated with data from the deposit area (27.5 Mg ha−1 event−1 and 161.0 Mg ha−1 event−1) was not only higher than the yearly sediment amounts, reported in literature, due to runoff processes, but it was even more intense than the yearly total deposition rate assessed with 137Cs (12.6 Mg ha−1 yr−1). The snow related soil erosion rates estimated from the sediment yield at the avalanche deposit area (3.7 Mg ha−1 and 20.8 Mg ha−1) were greater than the erosion rates reported in literature and related to runoff processes; they were comparable to the yearly total erosion rates assessed with the 137Cs method (13.4 Mg ha−1 yr−1 and 8.8 Mg ha−1 yr−1). The 137Cs method also showed that, where the ground avalanche does not release, the erosion and deposition of soil particles from the upper part of the basin was considerable and likely related to snow gliding. Even though the comparison of both the approaches is linked to high methodological uncertainties, mainly due to the different spatial and temporal scales considered, we still can deduce, from the similarity of the erosion rates, that soil redistribution in this catchment is driven by snow movement, with a greater impact in comparison to the runoff processes occurring in the snow-free season. Nonetheless, the study highlights that soil erosion processes due to the snow movements should be considered in the assessment of soil vulnerability in mountain areas, as they significantly determine the pattern of soil redistribution.

scholarly journals Evaluation of Forest Conversion Effects on Soil Erosion, Soil Organic Carbon and Total Nitrogen Based on 137Cs Tracer Technique

Forests ◽  
2019 ◽  
Vol 10 (5) ◽  
pp. 433 ◽  
Author(s):  
Xi Zhu ◽  
Jie Lin ◽  
Qiao Dai ◽  
Yanying Xu ◽  
Haidong Li
Keyword(s):  
Soil Erosion ◽  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Nutrient Loss ◽  
Vegetation Coverage ◽  
Forest Conversion ◽  
Tracer Technique ◽  
Mountain Areas ◽  
Clear Cutting ◽  
Average Annual Loss

Soil erosion can affect the horizontal and the vertical distribution of soil carbon at the landscape scale. The 137Cs tracer technique can overcome the shortcomings of traditional erosion research and has proven to be the best method to study soil erosion. To understand the responses of soil organic carbon and nitrogen to soil erosion and forest conversion in the development of slope economic forests in rocky mountain areas, three representative types of economic forests that were all formed after clear-cutting and afforestation on the basis of CBF (coniferous and broad-leaved mixed forests) were selected: CF (chestnut forests) with small human disturbance intensity, AF (apple forests), and HF (hawthorn forests) with high interference intensity. The results showed that all land use types have significantly eroded since 1950; the average annual loss of soil was 0.79 mm in the CBF, 2.31 mm in the AF, 1.84 mm in the HF, and 0.87 mm in the CF. The results indicated aggravation of soil erosion after the transformation of the CBF into an economic forest. The economic forest management reduced the average carbon storage and accelerated nutrient loss. The better vegetation coverage and litter coverage of CF made them stand out among the three economic forest varieties. Therefore, when developing economic forests, we should select species that can produce litter to ensure as much soil conservation as possible to reduce the risk of soil erosion.

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