Threshold of Ecological Geo-indicators of Green Coating on High-steep Slope of Limestone

YUAN Lei, ZHOU Jian-wei, WEN Bing, OU Hong-bing

Journal of Changjiang River Scientific Research Institute ›› 2017, Vol. 34 ›› Issue (7) : 36-40.

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Journal of Changjiang River Scientific Research Institute ›› 2017, Vol. 34 ›› Issue (7) : 36-40. DOI: 10.11988/ckyyb.20160307
WATER-SOIL CONSERVATION AND ECO-CONSTRUCTION

Threshold of Ecological Geo-indicators of Green Coating on High-steep Slope of Limestone

  • YUAN Lei1, ZHOU Jian-wei1, WEN Bing2, OU Hong-bing1
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Abstract

In the aim of exploring the underground habitat conditions for vegetation reconstruction of high and steep slopes, we investigated the habitat conditions of fractures where plants grow by measuring body fracture rate, temperature and humidity of fractures, and soil fertility in the fractures. Furthermore, we summarized the threshold of ecological geo-indicators through statistics of root mass of plants in limestone slopes by using sampling land method. The high-steep slopes of limestone in Shandong and Henan Regions were taken as research objects. Results revealed that the thresholds of ecological geo-indicators of green coating of high-steep slopes of limestone in North China include: 1) the adaptive range of body fracture rate of rock is 1.2‰~5%; 2)the root mass depth of small arbor and shrub is 20~40 cm which is the stable layer of plant species in underground habitat and the thresholds of adaptable temperature and humidity are 0~26 ℃, 90%~100%, respectively; 3) the soil also needs to meet certain fertility standards. Connected fracture network, adaptable and relatively stable temperature and humidity,given soil nutrient are important elements in the process of vegetation reconstruction of the limestone slopes,guaranteeing the stable underground habit needed for plant growth.

Key words

high-steep slope of limestone / green coating / threshold of ecological geo-indicator / condition of underground habit / body fracture rate

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YUAN Lei, ZHOU Jian-wei, WEN Bing, OU Hong-bing. Threshold of Ecological Geo-indicators of Green Coating on High-steep Slope of Limestone[J]. Journal of Changjiang River Scientific Research Institute. 2017, 34(7): 36-40 https://doi.org/10.11988/ckyyb.20160307

References

[1] 杨悦舒, 夏振尧, 肖 海,等. 系统工程原理在边坡生态防护工程中的应用[J]. 长江科学院院报, 2013, 30(10):32-36.
[2] 刘中亮,郝岩松,万福绪.我国石质困难地植被恢复与重建[J].南京林业大学学报(自然科学版),2010,34(2):137-141.
[3] 杨悦舒, 夏振尧, 肖 海,等. 恢复生态学理论在水电工程扰动区边坡生态修复中的应用[J]. 长江科学院院报, 2015, 32(7):52-57.
[4] JIM C Y. Ecological and Landscape Rehabilitation of a Quarry Site in Hong Kong[J]. Restoration Ecology,2001,9(1):85-94.
[5] 周 琼,许建新,秦永宏,等.黄石市岩质边坡生态修复综合技术应用探讨[J].中国水利,2011,(2):36-38.
[6] 徐恒力,孙自永,马 瑞.植物地境及物种地境稳定层[J].地球科学——中国地质大学学报,2004,29(2):239-246.
[7] 陈 刚,徐恒力,孙自永,等.太湖流域生态系统结构分析及其演化研究[M].北京:地质出版社,2008.
[8] 李瑞敏,鞠建华,王 轶,等.地质环境问题的地质指标体系框架及其构建方法[J].地质通报,2011,30(11):1738-1743.
[9] 贾昊冉,宁立波,李 明,等.岩体裂隙的生态学意义研究:以河南省宜阳县锦屏山采石场为例[J].环境科学与技术,2014,37(9):48-54.
[10]聂云鹏,陈洪松,王克林.土层浅薄地区植物水分来源研究方法[J].应用生态学报,2010,21(9):2427-2433.
[11]ZWIENIECKI M A,NEWTON M. Roots Growing in Rock Fissures: Their Morphological Adaptation[J].Plant and Soil,1995,172(2):181-187.
[12]DOBCHUK B S,BARBOUR S L,ZHOU J. Prediction of Water Vapor Movement Through Waste Rock[J].Journal of Geotechnical & Geoenvironmental Engineering,2014,130(3):293-302.
[13]陈建余.非稳定饱和-非饱和渗流场数值计算关键技术及其应用研究[D].南京:河海大学,2003.
[14]韩广轩,周广胜,许振柱.中国农田生态系统土壤呼吸作用研究与展望[J].植物生态学报,2008,32(3):719-733.
[15]冯全洲,徐恒力.土地复垦的覆土厚度及覆土基质确定[J].安徽农业科学,2009,37(25):12091-12094.
[16]骆东奇,白 洁,谢德体.论土壤肥力评价指标和方法[J].土壤与环境,2002,11(2):202-205.
[17]刘洪鹄, 赵玉明, 王秀颖,等. 土壤肥力评价方法探讨[J]. 长江科学院院报, 2008, 25(3):62-66.
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