1.黑龙江大学 现代农业与生态环境学院, 黑龙江;哈尔滨 150080
2.黑龙江省水利科学研究院, 黑龙江 哈尔滨 150000
梁欣平(2000—),女(汉族),黑龙江省哈尔滨市人,硕士研究生,研究方向为水土保持与农业资源。Email:2500715239@qq.com。
肖洋(1978—),男(汉族),黑龙江省哈尔滨市人,博士,教授,硕士研究生导师,主要从事水土保持与农业资源方面的研究。Email:xiaoyang@hlju.edu.cn。
收稿:2025-06-12,
修回:2025-08-01,
纸质出版:2025-12-10
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梁欣平, 肖洋, 王倡宪, 等.不同水土保持耕作措施对黑土坡耕地产流产沙的影响机制[J].水土保持通报,2025,45(6):33-40.
Liang Xinping, Xiao Yang, Wang Changxian, et al. Influencing mechanisms of different soil and water conservation tillage measures on runoff and sediment yield of slope cropland in black soil region [J]. Bulletin of Soil and Water Conservation,2025,45(6):33-40.
梁欣平, 肖洋, 王倡宪, 等.不同水土保持耕作措施对黑土坡耕地产流产沙的影响机制[J].水土保持通报,2025,45(6):33-40. DOI: 10.13961/j.cnki.stbctb.2025.06.016. CSTR: 32312.14.stbctb.2025.06.016.
Liang Xinping, Xiao Yang, Wang Changxian, et al. Influencing mechanisms of different soil and water conservation tillage measures on runoff and sediment yield of slope cropland in black soil region [J]. Bulletin of Soil and Water Conservation,2025,45(6):33-40. DOI: 10.13961/j.cnki.stbctb.2025.06.016. CSTR: 32312.14.stbctb.2025.06.016.
目的
2
探究在天然降雨条件下不同水土保持耕作措施对黑土区坡耕地产流产沙的影响机制,为东北黑土区水土流失的防控和治理提供科学依据和技术支撑。
方法
2
选取黑龙江省典型黑土区坡耕地为研究对象,布设径流小区,以传统顺坡垄作为对照,分析横坡垄作、横坡垄作+植物篱、秸秆还田和垄作区田4种水土保持耕作措施下的产流和产沙特征,探究不同水土保持耕作措施的减流减沙规律。
结果
2
①横坡垄作+植物篱、横坡垄作、秸秆还田和垄作区田4种水土保持耕作措施均能减少坡耕地产流量和产沙量,与顺坡垄作相比,产流量分别减少74%,67%,29%和64%,产沙量分别减少88%,87%,67%和66%。 ②横坡垄作+植物篱措施减流率和减沙率最为显著(
p
<
0.05)。 ③横坡垄作+植物篱措施下坡耕地产生径流和泥沙持续时间最短。 ④坡耕地产生径流量与泥沙量呈显著正相关(
p
<
0.01)。
结论
2
横坡垄作+植物篱措施能显著增大减流率和减沙率,建议在该地区推广应用。
Objective
2
The influencing mechanisms of different soil and water conservation tillage measures on runoff and sediment yield of slope cropland in the black soil region under natural rainfall conditions were analyzed, in order to provide a scientific basis and technical support for the prevention, control, and management of soil erosion in the black soil region in northeast China.
Methods
2
Typical slope cropland in the black soil region of Heilongjiang Province was selected as the research object. Runoff plots were established, with traditional downslope ridging as the control. The characteristics of runoff and sediment yield under four soil and water conservation tillage measures-cross-slope ridging, cross-slope ridging + plant hedges, straw return to the field, and ridge field-were analyzed to investigate the patterns of runoff and sediment reduction under different soil and water conservation tillage measures.
Results
2
① All four soil and water conser
vation tillage measures-cross-slope ridging + plant hedges, cross-slope ridging, straw return to the field, and ridge field-could reduce the runoff and sediment yield of slope cropland. Compared with downslope ridging, runoff decreased by 74%, 67%, 29%, and 64%, respectively, and sediment yield decreased by 88%, 87%, 67%, and 66%, respectively. ② The measures of cross-slope ridging + plant hedges showed the most significant rates of runoff and sediment reduction (
p
<
0.05). ③ The duration of runoff and sediment yield from the slope cropland under the cross-slope ridging + plant hedge measure was the shortest. ④ The runoff volume and sediment yield from the slope cropland showed a significant positive correlation (
p
<
0.01).
Conclusion
2
The cross-slope ridging plant hedge measure demonstrates significant runoff and sediment reduction rates, and it is recommended for wider application in this region.
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