干旱区生态环境知识资源中心(Arid): 半干旱矿区排土场苜蓿恢复过程中土壤颗粒分形的演变特征

Arid

	半干旱矿区排土场苜蓿恢复过程中土壤颗粒分形的演变特征
其他题名	The fractal characteristics of soil particles during the restoration of Medicago Sativa in a semi-arid mining dump
	王东丽; 刘阳; 郭莹莹; 谢伟; 郭建军; 汤国水; 赵晓亮; 连昭; 于百和
来源期刊	生态学报
ISSN	1000-0933
出版年	2020
卷号	40 期号:13 页码:4585-4593
中文摘要	种植苜蓿恢复模式在半干旱矿区植被恢复中占重要地位。为掌握其恢复过程中土壤颗粒分形的演变特征,选择恢复年限分别为2 a、4 a、6 a和10 a(M2、M4、M6和M10)的苜蓿种植地为研究对象,通过野外分层采样与室内测定,依据颗粒体积分形理论,研究了排土场苜蓿恢复过程中土壤颗粒分形的演变特征及与土壤特性的关系。结果表明:研究区土壤各粒径含量以砂粒为主,粉粒次之,粘粒最少;随着苜蓿恢复过程,粘粒与粉粒含量整体表现为先增加后下降的趋势,且在M4阶段达到最佳,砂粒反之。土壤分形维数变化在2.092.57,在苜蓿恢复过程中先增大后减小,在M4阶段达到最大。土壤分形维数与粘粒、粉粒具有极显著正相关性(P <0.01),与砂粒具有极显著负相关性(P <0.01);土壤分形维数与电导率呈极显著负相关关系(P<0.01),与pH值和速效钾含量呈显著负相关关系(P<0.05),与碱解氮含量呈显著正相关关系(P<0.05)。在半干旱矿区排土场采用苜蓿恢复模式,可用土壤分形维数表征土壤特性,应重视恢复年限的调控,适时进行适宜的利用与改造,确保矿区生态恢复的可持续性。
英文摘要	The ecological environment of semi-arid mining area is fragile with the severe site conditions, so it is difficult for the ecological reconstruction and vegetation restoration. Medicago. Sativa, as an important restoration plant, not only has strong resistance to stress, but also is useful to improve soil structure and nutrients. Thus, restoration model of planting M. Sativa plays an important role in vegetation restoration in semi-arid mining areas. To assess the effects of planting time on soil improvement, the evolution of soil particles fractal characteristics were studied by using methods of field stratified sampling and indoor measuring. Planting fields of M. Sativa with 2, 4, 6 and 10 years(M2, M4, M6 and M10) were selected as the research objects, while the new dump without planting and that with natural restoration were chosen as control treatment. Based on the particle size of fractal theory, the soil particles fractal characteristics of different planting years and its relationship with soil properties were measured and analyzed. The results showed that the content of soil particle size in the study dump was mainly sand, followed by silt and least clay. Compared with the new dump without planting and that with natural restoration, the content of clay and silt particles as a whole showed a trend of first increasing and then decreasing as the recovery of planting M. Sativa processed, and reached the optimal level at M4 stage, while sand particles showed the opposite trend. The vertical profile of soil particle size varied in different models. The soil particle size of the new dump with natural restoration tended to be clay and silt particles on 010 cm soil, while that of M2 and M4 stage tended to clay and silt particles on 2060 cm soil. The fractal dimension of soil varied from 2.09 to 2.57, first increasing and then decreasing during the recovery process of planting M. Sativa, and reaching the maximum at M4 stage. The fractal dimension of soil had extreme significantly positive correlation with clay and silt (P <0.01), and extreme significantly negative correlation with sand (P <0.01). The fractal dimension of soil was extreme significantly negative correlated with conductivity (P <0.01), significantly negative correlated with pH value and rapidly available potassium content (P< 0.05), and significantly correlated positive with available nitrogen content (P < 0.05). The soil fractal dimension can be used to determine the soil characteristics in the semi-arid mining dump. To sum up, the soil and vegetation population of planting M. Sativas will degrade after some restoration time, so it is necessary to pay attention to regulation of restoration time of planting M. Sativas. It is suggested that appropriate utilization and transformation should be carried out timely to ensure the sustainability of ecological restoration of mining abandon land in semi-arid region.
中文关键词	半干旱矿区 ; 排土场 ; 苜蓿恢复 ; 颗粒组成 ; 分形维数
英文关键词	semi-arid mining areas dump recovery of M. Sativa particle composition fractal dimension
类型	Article
语种	中文
收录类别	CSCD
WOS类目	Agriculture
CSCD记录号	CSCD:6770705
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/353755
作者单位	王东丽, 辽宁工程技术大学环境科学与工程学院, 阜新, 辽宁 123000, 中国. 刘阳, 辽宁工程技术大学环境科学与工程学院, 阜新, 辽宁 123000, 中国. 郭莹莹, 辽宁工程技术大学环境科学与工程学院, 阜新, 辽宁 123000, 中国. 赵晓亮, 辽宁工程技术大学环境科学与工程学院, 阜新, 辽宁 123000, 中国. 连昭, 辽宁工程技术大学环境科学与工程学院, 阜新, 辽宁 123000, 中国. 谢伟, 神东天隆集团有限责任公司生态研究院, 鄂尔多斯, 内蒙古 017000, 中国. 郭建军, 神东天隆集团有限责任公司生态研究院, 鄂尔多斯, 内蒙古 017000, 中国. 于百和, 神东天隆集团有限责任公司生态研究院, 鄂尔多斯, 内蒙古 017000, 中国. 汤国水, 辽宁工程技术大学矿业学院, 阜新, 辽宁 123000, 中国.
推荐引用方式 GB/T 7714	王东丽,刘阳,郭莹莹,等. 半干旱矿区排土场苜蓿恢复过程中土壤颗粒分形的演变特征[J],2020,40(13):4585-4593.
APA	王东丽.,刘阳.,郭莹莹.,谢伟.,郭建军.,...&于百和.(2020).半干旱矿区排土场苜蓿恢复过程中土壤颗粒分形的演变特征.生态学报,40(13),4585-4593.
MLA	王东丽,et al."半干旱矿区排土场苜蓿恢复过程中土壤颗粒分形的演变特征".生态学报 40.13(2020):4585-4593.