陕北黄土坡面典型退耕草本植物对土壤侵蚀过程的调控效应与机理
批准号:
42107359
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
陈浩
依托单位:
学科分类:
土壤侵蚀与土壤肥力
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
陈浩
中文摘要
退耕还草是调控坡面侵蚀的有效措施,退耕草本植物调控土壤侵蚀通过同步调控侵蚀动力与侵蚀阻力而实现。以往研究缺乏同步观测研究草本植物对土壤侵蚀、侵蚀动力及侵蚀阻力的调控效应,以及草本植物对侵蚀动力、侵蚀阻力调控效应对侵蚀调控效应的同步影响贡献,严重制约了对退耕还草坡面草本植物调控土壤侵蚀过程机理的全面与深入认识。本研究针对陕北黄土地区坡面典型退耕草本植物(白羊草)对土壤侵蚀的调控作用,通过草地坡面与裸地坡面模拟降雨与定流量供水组合试验观测,研究典型退耕草本植物对坡面侵蚀过程的调控效应、对坡面侵蚀动力的调控效应与机理、对坡面侵蚀阻力的调控效应与机理,量化草本植物对侵蚀动力调控效应与对侵蚀阻力调控效应对侵蚀调控效应同步影响的分别贡献,阐明典型退耕草本植物对坡面侵蚀的调控机理,实现陕北黄土坡面典型退耕草本植物对土壤侵蚀过程调控效应与机理的研究揭示,为黄土高原坡面侵蚀控制及生态建设提供科学依据。
英文摘要
Returning farmland to grassland is an effective measure to control slope erosion. Recovered herbaceous plants can control soil erosion by regulating erosion dynamics and erosion resistance, simultaneously. However, there is a lack of studies to systematically study the synchronization contribution of effects of herbaceous plants reducing erosion dynamics and increasing erosion resistance on controlling soil erosion. The lacking of these studies greatly restricts the in-depth and comprehensive understanding of the kinetic mechanism of recovered herbaceous plants controlling soil erosion. Accordingly, the effects of typical recovered herbaceous plants (Bothriochloa ischaemum) on soil erosion will be studied in this project, based on laboratory simulated rainfall and constant-flow supply experiments, on loess slope in northern Shaanxi Province.The effectiveness of the typical recovered herbaceous plants in controlling soil erosion of loess slope will be studied. As well as the effectiveness and mechanism of the typical recovered herbaceous plants in reducing erosion dynamics and increasing erosion resistance also will be analyzed. The contribution rates of the typical recovered herbaceous plants on reducing erosion dynamics and increasing erosion resistance to its effect of controlling soil erosion will be quantified. The results can reveal of regulation effects and mechanisms of the typical recovered herbaceous plants on soil erosion processes on loess slope in northern Shaanxi Province, and provide scientific support for soil erosion controlling and ecological constructions on the Leoss Plateau.
退耕还草是调控坡面侵蚀的有效措施,退耕草被调控土壤侵蚀通过同步调控侵蚀动力与侵蚀阻力而实现。本项目针对陕北黄土区典型退耕草本植物对土壤侵蚀的调控作用,通过草地坡面与裸地坡面人工模拟降雨试验观测方法,研究了草被对坡面侵蚀过程的调控效应、对坡面侵蚀动力的调控效应与机理、对坡面侵蚀阻力(土壤可蚀性)的调控效应与机理,量化了草被对侵蚀动力调控效应与对侵蚀阻力调控效应对侵蚀调控效应同步影响的分别贡献。主要结果为:.(1)坡面径流深随坡度的增加而减小,土壤侵蚀模数和径流含沙量则随坡度的增加而增大。坡面径流深、侵蚀模数和径流含沙随雨强的增加而增大,随草被盖度的增加而减小。次降雨径流深对雨强、坡度和盖度的综合响应可用H=2.597S-0.1I1.325C-0.204(R2=0.986,P<0.01)表示。次降雨侵蚀模数对雨强、坡度和盖度的综合响应可用EM=0.021S+1.59I-2.097C-0.43(R2=0.877,P<0.01)表示。次降雨径流含沙量对雨强、坡度和盖度的综合响应可用SC=0.013S+0.228I-0.614C+0.0602(R2=0.771,P<0.01)表示。草被的径流调控效应、侵蚀调控效应和径流含沙量调控效应皆与草被盖度呈正相关关系。.(2)侵蚀模数对不同径流水动力学参数的响应方程表明,表征坡面侵蚀的关键水动力学特征参数为水流功率和径流流速。草被对水流功率和径流流速的调控效应均与植基盖度和冠层盖度呈极显著正相关关系(P<0.01),且植基盖度比冠层盖度更能解释草被对径流水动力学参数的削减作用。.(3)坡面土壤可蚀性调控效应随盖度的增加而增加。根系体积密度(RV)和土壤团聚体平均质量直径(MWD)为与坡面土壤可蚀性调控效应密切相关的特征参数。土壤可蚀性调控效应对二者的综合响应可用RPK=6.262RV+5.335MWD-0.761(R2=0.937,p<0.01)表示。根系的缠绕固结土体作用和改善土壤性质作用对土壤可蚀性增强效应的贡献分别为54%和39%。.(4)同坡度不同雨强下,草被调控水流功率效应及调控土壤可蚀性效应分别对其调控土壤侵蚀效应同步影响的分别贡献率为49.6%和49.7%;同雨强不同坡度下,草被调控水流功率效应及调控土壤可蚀性效应分别对其调控土壤侵蚀效应同步影响的分别贡献率为13%和78%。
国内基金
海外基金