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秦岭地区土壤侵蚀时空变化及景观格局

郭思琪1,2,韩磊1,2,赵永华1,2*,员学锋1,2,王达1,2,李蕴琪1,2   

  1. (1长安大学地球科学与资源学院/土地工程学院, 西安 710054;2陕西省土地整治重点实验室, 西安 710054)
  • 出版日期:2019-07-10 发布日期:2019-07-10

Spatiotemporal variation and landscape pattern of soil erosion in Qinling Mountains.

GUO Si-qi1,2, HAN Lei1,2, ZHAO Yong-hua1,2*, YUAN Xue-feng1,2, WANG Da1,2, LI Yun-qi1,2   

  1. (1School of Earth Science and Resources/School of Land Engineering, Chang’an University, Xi’an 710054, China; 2Shaanxi Key Laboratory of Land Consolidation, Xi’an 710054, China).
  • Online:2019-07-10 Published:2019-07-10

摘要: 土壤侵蚀是制约秦岭地区可持续发展的重要因素,为了解秦岭地区的土壤侵蚀状况及景观格局的变化,基于2005年、2010年和2015年遥感解译结果,采用通用土壤侵蚀方程RUSLE计算各年的土壤侵蚀量,分析研究区土壤侵蚀的时空变化特征,量化秦岭地区5个流域的土壤侵蚀状况,探讨土壤侵蚀与土地利用及地形因子之间的关系,并对研究区土壤侵蚀景观格局变化进行分析。结果表明:2005—2015年秦岭地区土壤侵蚀强度及面积均有明显改善,2005年和2015年总侵蚀量分别为0.90×108和0.33×108 t,减少了63.33%;研究区内土壤侵蚀在空间上呈现由西向东、由南至北减弱的特征;位于研究区西部的嘉陵江流域土壤侵蚀最为严重,其2005年、2010年和2015年土壤侵蚀模数分别为3872.80、1454.31和1461.91 t·km-2·a-1;土壤侵蚀模数与坡度、高程等地形因子呈正相关,具有明显的时空变化特征;区内不同土地利用类型的土壤侵蚀均有减弱的趋势,其中未利用土地土壤侵蚀的降低最为明显;秦岭地区的整体侵蚀景观破碎化程度有所降低,斑块总数减少,破碎度指数变小,景观异质性降低,人类活动对秦岭地区景观的干扰随时间而减弱,生态环境向良性方向发展。

关键词: 可口革囊星虫, 富集, 重金属, 生长, 蛋白质, 脂肪

Abstract: Soil erosion is an important factor restricting the sustainable development of Qinling Mountains region. This study aims to explore the soil erosion status and landscape pattern change in Qinling Mountains. Based on the results of remote sensing interpretation in 2005, 2010 and 2015, the general soil erosion equation (RUSLE) was used to calculate the soil erosion in those three years. After that, soil erosion status of the five major watersheds in Qinling Mountains was quantified. The relationships among soil erosion, land use, and topographic factors were analyzed, and the changes of soil erosion landscape pattern in the study area were clarified. Intensity and area of the soil erosion in Qinling Mountains significantly decreased from 2005 to 2015. The total erosion amounts in 2005 and 2015 were 0.90×108 and 0.33×108 t respectively, with a reduction of 63.33%. Soil erosion decreased from west to east and from south to north. Soil erosion was the most serious in the Jialing River basin, situated in the western part of the study area. The soil erosion modulus in 2005, 2010 and 2015 were 3872.80, 1454.31 and 1461.91 t·km-2·a-1, respectively. The soil erosion modulus was positively correlated with topographic factors such as slope and elevation, and showed obvious temporal and spatial variations. Soil erosion showed a weakening trend in different land use types in the region, with the most obvious reduction for the unused land. The fragmentation degree of the overall erosion landscape and the total number of patches in Qinling Mountains reduced, and the fragmentation index and the landscape heterogeneity decreased. The anthropogenic disturbance on the landscape of Qinling Mountains weakened over time, and the ecological environment was developing in a benign direction.

Key words: Phascolosoma esculenta, enrichment, heavy metal, growth, protein, lipid.