Soil physical properties response to grassland conversion from cropland on the semi-arid area

Ecohydrology ◽  
2016 ◽  
Vol 9 (8) ◽  
pp. 1471-1479 ◽  
Author(s):  
Gao-Lin Wu ◽  
Yu Liu ◽  
Nu-Fang Fang ◽  
Lei Deng ◽  
Zhi-Hua Shi
2015 ◽  
Vol 7 (1) ◽  
pp. 1007-1024
Author(s):  
B. Turgut

Abstract. The aim of this study was to compare the soils of the wheat cultivation area (WCA) and the safflower cultivation area (SCA) within semi-arid climate zones in terms of their total carbon, nitrogen, sulphur contents, particle size distribution, aggregate stability, organic matter content, and pH values. This study presents the results from the analyses of 140 soil samples taken at two soil layers (0–10 and 10–20 cm) in the cultivation areas. At the end of the study, it has been established that there were significant differences between the cultivation areas in terms of soil physical properties such as total carbon (TC), total nitrogen (TN), total sulphur (TS) contents and pH, while only the TN content resulted in significantly different between the two soil layers. Moreover significant differences were identified in the cultivation areas in terms of soil physical properties including clay and sand contents, aggregate stability and organic matter content, whereas the only significant difference found among the soil layers was that of their silt content. Since safflower contains higher amounts of biomass than wheat, we found higher amounts of organic matter content and, therefore, higher amounts of TN and TS content in the soils of the SCA. In addition, due to the fact that wheat contains more cellulose – which takes longer to decompose – the TC content of the soil in the WCA were found to be higher than that of the SCA. The results also revealed that the WCA had a higher carbon storage capacity.


1993 ◽  
Vol 27 (1-4) ◽  
pp. 125-147 ◽  
Author(s):  
R. Nicou ◽  
C. Charreau ◽  
J.-L. Chopart

2012 ◽  
Vol 454 ◽  
pp. 273-278
Author(s):  
Xiao Wei Zhang ◽  
En De Wang

Semi-arid region of Soil repair in Mine spoils is a problem of worthy of attention and research, this paper assesses Fuxin mining area and YuanBaoShan mining area for test site, five kinds of site types are divided based on the investigation of mine spoils damage situation, and testing each sitetype of soil physical properties and the change of soil nutrient systematically, and doing the five kinds of sitetypes’phytoremediation research based on it. The evaluation results indicate: Mine spoils soil along with the increasing length of stopping discharging the gangue, the soil physical and chemical characteristics improve gradually. Through the research of vegetation and soil interaction relations we get the best Reclamation vegetation types of the Mine spoils. Mine spoils is an important form of land degradation, is one of the major environmental problems of today's world. This paper assesses Fuxin mining area and YuanBaoShan mining area for test site, testing each site type of soil physical properties and the change of soil nutrient systematically, and on the basis of experiments, putting forward the best Reclamation vegetation types for mine spoils.


Solid Earth ◽  
2015 ◽  
Vol 6 (2) ◽  
pp. 719-725 ◽  
Author(s):  
B. Turgut

Abstract. The aim of this study was to compare the soils of the wheat cultivation area (WCA) and the safflower cultivation area (SCA) within semi-arid climate zones in terms of their total carbon, nitrogen, and sulphur contents, particle size distribution, aggregate stability, organic matter content, and pH values. This study presents the results from the analyses of 140 soil samples taken at two soil layers (0–10 and 10–20 cm) in the cultivation areas. At the end of the study, it was established that there were significant differences between the cultivation areas in terms of soil physical properties such as total carbon (TC), total nitrogen (TN), total sulphur (TS) contents and pH, while only the TN content was significantly different between the two soil layers. Moreover, significant differences were identified between the cultivation areas in terms of soil physical properties including clay and sand contents, aggregate stability, and organic matter content, whereas the only significant difference found among the soil layers was that of their silt content. Since safflower contains higher amounts of biomass than wheat, we found higher amounts of organic matter content and, therefore, higher amounts of TN and TS content in the soils of the SCA. In addition, due to the fact that wheat contains more cellulose – which takes longer to decompose – the TC content of the soil in the WCA was found to be higher than that in the SCA. The results also revealed that the WCA had a higher carbon storage capacity.


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