1. 水利部黄土高原水土保持重点实验室,郑州,400003
2. 黄河水利委员会黄河水利科学研究院,郑州,450003
[ "姚文艺(1957-),男,教授级高工,主要从事水土保持研究。E-mail:964144518@qq.com" ]
纸质出版:2023
移动端阅览
姚文艺, 焦鹏. 黄河流域水土保持综合治理空间均衡性分析[J]. 水土保持学报, 2023,37(1):1-7.
YAO Wenyi, JIAO Peng. Spatial Equilibrium Analysis of Comprehensive Control of Soil and Water Conservation in the Yellow River Basin[J]. 2023, 37(1): 1-7.
姚文艺, 焦鹏. 黄河流域水土保持综合治理空间均衡性分析[J]. 水土保持学报, 2023,37(1):1-7. DOI: 10.13870/j.cnki.stbcxb.2023.01.001.
YAO Wenyi, JIAO Peng. Spatial Equilibrium Analysis of Comprehensive Control of Soil and Water Conservation in the Yellow River Basin[J]. 2023, 37(1): 1-7. DOI: 10.13870/j.cnki.stbcxb.2023.01.001.
黄河流域具有多类别的泥沙来源区
水沙异源特性突出
研究水土保持综合治理空间均衡性
对于优化水土保持空间布局和有效持续减少入黄泥沙极为必要。基于黄河泥沙来源区特征和水土保持综合治理现状分析
利用统计学理论与方法
研究水土保持综合治理空间均衡性的概念、评价原理和评价方法
并对治理现状的均衡性进行评价。结果表明:(1)与流域水土流失强度空间分异性相对应、且在一定程度上能够有效控制侵蚀产沙强度的治理是空间治理均衡性的基本体现
其治理程度可以利用治理效应定量反映;(2)不同治理程度的减沙作用不同的
通过分析全流域系统内不同分区治理措施减沙作用度的差异
可以判识治理的空间均衡性;(3)治理空间均衡性的评价内容主要包括划分评价流域分区、计算水土保持措施减沙作用度和空间治理均衡系数判识弱治理区;(4)目前黄河流域空间治理是不均衡的
兰州—头道拐片区、头道拐—龙门区间陕西北片的水土保持措施减沙作用度、空间治理均衡系数都很低
属于典型的弱治理区。提出的水土保持综合治理空间均衡性评价方法可定量识别弱治理区
为优化水土保持发展格局提供新的技术方法。
The Yellow River Basin has a variety of sediment source areas
and the characteristics of water and sediment sources are prominent. Therefore
it is extremely necessary to study the Spatial equilibrium analysis of comprehensive control of soil and water conservation to optimize the spatial layout of soil and water conservation and to effectively and continuously reduce the sediment entering the Yellow River. Based on the analysis of the characteristics of the sediment source areas and the current situation of comprehensive control of soil and water conservation
we used statistical theory and methods to study the concept
principle and evaluation method of the spatial equilibrium of comprehensive control of the Yellow River soil and water conservation
and evaluated the equilibrium of control status. The results show that: (1) The spatial equilibrium of comprehensive control of soil and water conservation in the watershed refers to the control measures that corresponds to the spatial heterogeneity of soil erosion intensity and can effectively control the erosion and sediment yield intensity to a certain extent
and the degree of the control can be quantified by the effect; (2) The sediment reduction effects of different degrees of control are different
and the spatial equilibrium of control in the whole basin system can be identified by the differences in the degree of sediment reduction effect of different zoning control measures; (3) The evaluation method of spatial equilibrium of control is proposed
and the method mainly includes evaluation of watershed zoning
calculation of the degree of sediment reduction effect of soil and water conservation measures and spatial equilibrium coefficient of comprehensive control
and identification of weakly controlled areas; (4) At present
the spatial control of the Yellow River Basin is uneven
and the degree of sediment reduction effect of soil and water conservation measures and the spatial control equilibrium coefficient are very low in the Lanzhou-Toudaoquan area and the northern part of Shaanxi Province
which are typical weak control areas. The proposed method for evaluating the spatial equilibrium of comprehensive control of soil and water conservation can quantitatively identify weakly controlled areas and provide a new technical method for optimizing the development pattern of soil and water conservation.
李文学.黄河治理开发与保护70年效益分析[J].人民黄河,2016,38(10):1-6.
水利部.2021年全国水土流失动态监测显示我国水土流失状况持续向好,生态文明建设成效斐然.(2022-06-28).https://mp.weixin.qq.com/s/8o8Tv_3NjiEBeiRGQCcA-w.
贾善铭.区域经济增长空间均衡研究述评[J].区域经济评论,2014(1):124-129.
Walras L. Elements d'economic politique pure Lausanne:L.Corbaz. Transl.By William Jaffe as elements of pure economics,Homewood,Ⅰ11:Richard D.Irwin[J]Metroeconomica,1954,6(3):136-139.
陈雯.空间经济学研究的相关进展与评述[J].世界地理研究,2007,16(4):70-75.
挂云帆.空间均衡理论.(2021-03-06).https://www.guayunfan.com/lilun/82805.html,/2022-10-10.
姚文艺,刘国彬.新时期黄河流域水土保持战略目标的转变与发展对策[J].水土保持通报,2020,40(5):333-340.
徐伟铭,陆在宝,肖桂荣.基于遗传算法的水土保持措施空间优化配置[J].中国水土保持科学,2016,14(6):114-124.
陆在宝.基于遗传算法的水土保持措施空间优化配置:以福建省长汀县为例[D].福州:福州大学,2018.
许炯心,姚文艺,韩鹏,等.基于气候地貌植被耦合的黄河中游侵蚀过程[M].北京:科学出版社,2009.
薛頔.浑善达克沙地植物生长适宜性精准空间分布研究[D].北京:北京林业大学,2020.
张晓光,朝阳县下洼小流域水土保持措施空间配置[J].黑龙江水利科技,2020,48(7):143-146.
陈亮.基于辽宁省坡耕地水土保持措施的空间配置研究[J].水资源开发与管理,2017(12):31-34.
张海强,张满良,何秀红,等.甘肃黄河流域水土保持生态环境建设区域配置研究[J].现代农业科学2009,16(3):144-146.
张风香,刘培郎.基于生态安全的小流域水土保持措施空间配置研究:以灯台架小流域为例[J].水利规划与设计,2018(7):104-106.
苏长芳.基于多尺度影响因子的水土保持措施布局研究[J].水利技术监督,2020(1):161-164,268.
和继军,蔡强国,方海燕,等.张家口地区水土保持措施空间配置效应评价[J].农业工程学报,2009,25(10):69-75.
周毅,魏天兴,解建强,等.黄土高原不同林地类型水土保持效益分析[J].水土保持学报,2011,25(3):12-16,21.
何长高.水土保持在综合调控流域水资源配置中的作用[J].中国水土保持科学,2006,4(4):91-102.
傅伯杰.国土空间生态修复亟待把握的几个要点[J].中国科学院院刊,2021,36(1):64-69.
谢永生,李占斌,王继军,等.黄土高原水土流失治理模式的层次结构及其演变[J].水土保持学报,2011,25(3):211-214.
水利部黄河水利委员会.1919-1951年及1991-1998年黄河流域主要水文站实测水沙特征值统计[R].郑州:水利部黄河水利委员会,2001.
黄河水利委员会.黄河水沙变化研究[R].郑州:黄河水利委员会,2015.
张胜利,于一鸣,姚文艺.水土保持减沙减沙效益计算方法[M].北京:中国环境出版社,1994:106-145.
赵文林.黄河泥沙[M].郑州:黄河水利出版社,1996:43-48.
张兴军.黄河流域水土流失面积和强度实现"双下降".(2022-01-30). http://www.gov.cn/xinwen/2022-01/30/content_5671409.htm.
姚文艺,李长明,张攀,等.砒砂岩侵蚀机理研究与展望[J].人民黄河,2018,40(6):141-147.
殷宝库,苏鹏飞,张建国,等.1985-2020年黄河中游多沙粗沙区水土流失动态变化[J].水土保持通报,2021,41(5):123-126.
李占斌.黄河中游多沙粗沙区风水复合侵蚀协同治理技术与示范项目实施方案[R].西安:西安理工大学,2022:3.
陈正新.黄河十大孔兑水土保持减沙效益评价[M].郑州:黄河水利出版社,2021:236-237.
0
浏览量
928
下载量
4
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621