Effect of crevice density on biological soil crust development on rock cut slope in mountainous regions, Sichuan, China

被引:0
作者
Maoqiang Zhao [1 ,2 ]
Wanqiu Pu [1 ]
Jie Du [3 ]
Wenhu Liu [1 ]
Qian Zhang [1 ]
Yanmei Liu [1 ]
Li Xiao [1 ]
Yingwei Ai [4 ]
Chengmin Huang [1 ]
机构
[1] Department of Environmental Science and Engineering, Sichuan University
[2] Sichuan Institute of Geological Engineering Investigation Group Co, Ltd
[3] Jiuzhaigou Administration Bureau
[4] School of Life Science, Sichuan
关键词
D O I
暂无
中图分类号
Q948 [植物生态学和植物地理学];
学科分类号
071012 ; 0713 ;
摘要
Background The rock cut slope(RCS) could cause damage to regional ecological functions and landscapes and requires recovery. Biological soil crusts(BSCs) are pioneer and dominant colonizers during the initial recovery stage. To accelerate the natural recovery of RCS, the development process and influencing agents of BSC should be revealed.Thus, the area index of crevices(IR), BSC coverage(COV) and biomass(BM), soil weight(SW), and major soil nutrients [organic carbon(OC), total nitrogen(TN) and total phosphorus(TP)] content, collected from 164 quadrats on 13 RCSs in the mountainous area of west Sichuan Province, China, were measured, to explore the effect of crevice of RCS on BSC development.Results Soil OC, TN and TP on RCSs ranged from 18.61 to 123.03 g kg-1, 0.96 to 6.02 g kg-1 and 0.52 to 2.46 g kg-1,respectively, and were approximately to or higher than those on natural slopes. The OC, TN and TP contents in soils elevated unsystematically with recovery time of RCSs. BSCs on RCS distributed along crevices generally and firstly.During the first 13 years of natural recovery, COV, BM and SW ranged from 6.5 to 28.2%, 14.43 to 67.25 g m-2, and 127.69 to 1277.74 g m-2, respectively. COV, BM and SW increased linearly with IR on RCSs. The positive correlation between COV and BM and IR was insignificantly impacted by bedrock, slope aspect and altitude within the recovery time less than 13 years. COV and BM on RCSs increased significantly when the recovery time is more than 27 years.Conclusions Crevice on RCSs could be a major environmental factor which is conducive to BSC development and soil accumulation through creating a space for water and soil particle. Furthermore, with the increase of recovery time of RCSs, BSCs may grow and reach a stable state with the promotion of soil nutrients, plant growth and microbial activity. These results provide a development process of BSC that from inside to outside the crevices on RCSs. In the areas with stable rock strata and a low risk of geological disasters, purposeful improvement in crevice density on RCS may effectively accelerate BSC development.
引用
收藏
页码:48 / 65
页数:18
相关论文
共 106 条
[11]   生物结皮对沙质土壤水含量和水分入渗的影响 [J].
龚萍 ;
党晓宏 ;
蒙仲举 ;
迟文峰 ;
常江 .
干旱区资源与环境, 2022, 36 (09) :120-125
[12]  
毛乌素沙地区域尺度生物结皮有机碳空间分布特征及其影响因素.[J].庞景文;卜崇峰;郭琦;鞠孟辰;江熳;莫秋霞;王鹤鸣;.应用生态学报.2022, 07
[13]  
黄土丘陵区草本植物覆盖下生物结皮对坡面径流流速的削减作用.[J].郭雅丽;赵允格;高丽倩;杨凯;孙会;谷康民;.应用生态学报.2022, 07
[14]  
Aspects of forest restoration and hydrology:the hydrological function of litter.[J].Luara Castilho Pereira;Leonardo Balbinot;Marcelle Teodoro Lima;Julieta Bramorski;Kelly Cristina Tonello;.Journal of Forestry Research.2022, 02
[15]   生物土壤结皮对东祁连山高寒草甸土壤特性的影响 [J].
卢研 ;
张倩 ;
张彩军 ;
孙小妹 ;
苏军虎 .
草原与草坪, 2022, 42 (01) :13-20
[16]  
Aspects of forest restoration and hydrology:linking passive restoration and soil-water recovery in Brazilian Cerrado.[J].Luara Castilho Pereira;Leonardo Balbinot;Gregorio Nolazco Matus;Herly Carlos Teixeira Dias;Kelly Cristina Tonello;.Journal of Forestry Research.2021, 06
[17]   喀斯特石漠化区典型生境下石生苔藓的固土持水作用 [J].
涂娜 ;
严友进 ;
戴全厚 ;
任青青 ;
蒙文萍 ;
朱列坤 ;
岑龙沛 .
生态学报, 2021, 41 (15) :6203-6214
[18]   黄土高原生物土壤结皮研究进展与展望 [J].
张丙昌 ;
武志芳 ;
李彬 .
土壤学报, 2021, 58 (05) :1123-1131
[19]   岩石创面“植被-土壤”系统恢复:影响因素与生态演替 [J].
赵茂强 ;
蒲婉秋 ;
刘文虎 ;
黄成敏 .
环境生态学, 2020, 2 (09) :1-11
[20]   大渡河流域降水时空分布特征 [J].
肖杨 ;
袁淑杰 ;
张碧 ;
何兴潼 ;
于飞 .
人民长江, 2019, 50(S1) (S1) :60-67