资源科学 ›› 2019, Vol. 41 ›› Issue (2): 394-404.doi: 10.18402/resci.2019.02.17
贯丛1,2,3(), 张树文2(
), 王让虎4, 杨久春2, 岳书平5, 于灵雪2, 王文娟6
收稿日期:
2018-06-26
修回日期:
2018-12-03
出版日期:
2019-02-25
发布日期:
2019-02-25
作者简介:
作者简介: 贯丛,女,吉林长春人,博士生,研究方向为土地利用/覆被变化监测。E-mail:
基金资助:
Cong GUAN1,2,3(), Shuwen ZHANG2(
), Ranghu WANG4, Jiuchun YANG2, Shuping YUE5, Lingxue YU2, Wenjuan WANG6
Received:
2018-06-26
Revised:
2018-12-03
Online:
2019-02-25
Published:
2019-02-25
摘要:
黑土区坡耕地的侵蚀沟发育发展与耕作措施密切相关,垄向分布对沟蚀的影响机制研究能够为黑土区采取更合理有效的耕种措施提供科学依据。本文以东北典型黑土区的三岔河流域为研究区,基于2013年地理国情普查提供的高精度基础数据获取耕地垄向和侵蚀沟数据,对沟蚀密度和裂度与耕地垄向角之间的关系进行定量分析,并研究了不同垄向下沟蚀与地形的耦合作用。研究结果表明:①研究区坡耕地横坡耕作的趋势非常明显;②研究区耕地沟蚀强度为中度侵蚀;③耕地垄向角与沟蚀密度和裂度显著负相关,即随着垄向角的增大,研究区耕地的平均沟蚀密度和裂度呈线性下降趋势,横坡垄中的侵蚀沟密度和裂度最大,其中垄向角和沟蚀密度的线性拟合效果最好,沟蚀裂度稍差;④不同耕地垄向中的侵蚀沟分布具有明显的地形分异特征:当海拔大于280 m时,各垄向耕作都不能有效地抵御侵蚀沟的产生;当坡度大于15°时,横坡垄中的沟蚀裂度最小,但仍高于缓坡各垄向耕地中的沟蚀裂度;各耕作垄向在阴坡对侵蚀沟面积的影响无明显差异。
贯丛, 张树文, 王让虎, 杨久春, 岳书平, 于灵雪, 王文娟. 三岔河流域坡耕地垄向与侵蚀沟分布耦合分析[J]. 资源科学, 2019, 41(2): 394-404.
Cong GUAN, Shuwen ZHANG, Ranghu WANG, Jiuchun YANG, Shuping YUE, Lingxue YU, Wenjuan WANG. Coupling analysis between ridge direction and gully erosion of sloping cultivated lands in the Sancha River watershed[J]. Resources Science, 2019, 41(2): 394-404.
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