中部森林草原灰色森林土壤坡面泉水径流的影响因素

A.T. BARABANOV, A.I. PETELKO
{"title":"中部森林草原灰色森林土壤坡面泉水径流的影响因素","authors":"A.T. BARABANOV, A.I. PETELKO","doi":"10.55959/10.55959/msu0579-9414.5.78.4.2","DOIUrl":null,"url":null,"abstract":"The results of long-term studies of several generations of scientists at the Novosilskaya zonal agroforestry and reclamation experimental station named after A.S. Kozmenko (a branch of the Federal Research Center of Agroecology of the Russian Academy of Sciences), initiated by Professor G.P. Surmach, were summarized and analyzed. The task was to assess the nature of the spring slope runoff formation and show the role of natural factors and agricultural activities. The methodological basis of the research was the method of runoff sites. As a result of a long (64 year long) study, a number of important dependencies and features of the runoff formation under different natural and climatic conditions were identified, as well as the influence of natural factors and agricultural activities on it (structure of sown areas, cultivation history, tillage methods, etc.). Scientific materials on the elements of the spring water balance give an idea of their patterns. It has been established that only three natural factors out of a large number of them have a significant impact on the slope spring runoff, i. e. the depth of soil freezing, snow reserves and humidity of the upper soil layer (down to 30 cm). Other factors almost do not affect the amount of runoff and they could be ignored in the process of calculation. The limiting levels of these three factors have been established, under which no runoff is formed. During 64 years of study, runoff was absent for 33 years, ranging from 1 to 146 mm in other years. Among anthropogenic factors, tillage methods and the state of agricultural backgrounds have a profound influence. The runoff regulatory importance of finching and the runoff forming role of perennial grasses and winter crops are discussed. On average, runoff from compacted arable land was 10 mm higher compared to loose chick; in some years the difference was significantly greater. The results of the study are necessary for the design of erosion-control adaptive landscape farming system.","PeriodicalId":158808,"journal":{"name":"Lomonosov Geography Journal","volume":"35 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"FACTORS OF SLOPE SPRING RUNOFF ON GRAY FOREST SOILS IN THE CENTRAL FOREST-STEPPE\",\"authors\":\"A.T. BARABANOV, A.I. PETELKO\",\"doi\":\"10.55959/10.55959/msu0579-9414.5.78.4.2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The results of long-term studies of several generations of scientists at the Novosilskaya zonal agroforestry and reclamation experimental station named after A.S. Kozmenko (a branch of the Federal Research Center of Agroecology of the Russian Academy of Sciences), initiated by Professor G.P. Surmach, were summarized and analyzed. The task was to assess the nature of the spring slope runoff formation and show the role of natural factors and agricultural activities. The methodological basis of the research was the method of runoff sites. As a result of a long (64 year long) study, a number of important dependencies and features of the runoff formation under different natural and climatic conditions were identified, as well as the influence of natural factors and agricultural activities on it (structure of sown areas, cultivation history, tillage methods, etc.). Scientific materials on the elements of the spring water balance give an idea of their patterns. It has been established that only three natural factors out of a large number of them have a significant impact on the slope spring runoff, i. e. the depth of soil freezing, snow reserves and humidity of the upper soil layer (down to 30 cm). Other factors almost do not affect the amount of runoff and they could be ignored in the process of calculation. The limiting levels of these three factors have been established, under which no runoff is formed. During 64 years of study, runoff was absent for 33 years, ranging from 1 to 146 mm in other years. Among anthropogenic factors, tillage methods and the state of agricultural backgrounds have a profound influence. The runoff regulatory importance of finching and the runoff forming role of perennial grasses and winter crops are discussed. On average, runoff from compacted arable land was 10 mm higher compared to loose chick; in some years the difference was significantly greater. The results of the study are necessary for the design of erosion-control adaptive landscape farming system.\",\"PeriodicalId\":158808,\"journal\":{\"name\":\"Lomonosov Geography Journal\",\"volume\":\"35 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-09-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Lomonosov Geography Journal\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.55959/10.55959/msu0579-9414.5.78.4.2\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Lomonosov Geography Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.55959/10.55959/msu0579-9414.5.78.4.2","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

总结和分析了由G.P. Surmach教授发起的以A.S. Kozmenko命名的Novosilskaya地带性农林业和开垦实验站(俄罗斯科学院联邦农业生态研究中心的一个分支)几代科学家长期研究的结果。任务是评估春季坡面径流形成的性质,并显示自然因素和农业活动的作用。本研究的方法学基础是径流点法。经过长达64年的长期研究,确定了不同自然和气候条件下径流形成的一些重要依赖关系和特征,以及自然因素和农业活动对径流形成的影响(播种面积结构、耕作历史、耕作方法等)。有关泉水平衡要素的科学资料可以说明它们的模式。在众多自然因素中,只有土壤冻结深度、积雪储量和上层土壤湿度(30cm以下)三个因素对坡面泉径流有显著影响。其他因素几乎不影响径流量,在计算过程中可以忽略。这三个因素的极限水平已经确定,在此限度下不会形成径流。在64年的研究中,有33年没有径流,其他年份为1 ~ 146 mm。在人为因素中,耕作方式和农业背景状况影响深远。讨论了雀类对径流的调节作用以及多年生禾草和冬季作物对径流的形成作用。压实耕地的径流量比松散耕地平均高10 mm;在某些年份,差异明显更大。研究结果对水土保持适应性景观耕作系统的设计具有一定的指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
FACTORS OF SLOPE SPRING RUNOFF ON GRAY FOREST SOILS IN THE CENTRAL FOREST-STEPPE
The results of long-term studies of several generations of scientists at the Novosilskaya zonal agroforestry and reclamation experimental station named after A.S. Kozmenko (a branch of the Federal Research Center of Agroecology of the Russian Academy of Sciences), initiated by Professor G.P. Surmach, were summarized and analyzed. The task was to assess the nature of the spring slope runoff formation and show the role of natural factors and agricultural activities. The methodological basis of the research was the method of runoff sites. As a result of a long (64 year long) study, a number of important dependencies and features of the runoff formation under different natural and climatic conditions were identified, as well as the influence of natural factors and agricultural activities on it (structure of sown areas, cultivation history, tillage methods, etc.). Scientific materials on the elements of the spring water balance give an idea of their patterns. It has been established that only three natural factors out of a large number of them have a significant impact on the slope spring runoff, i. e. the depth of soil freezing, snow reserves and humidity of the upper soil layer (down to 30 cm). Other factors almost do not affect the amount of runoff and they could be ignored in the process of calculation. The limiting levels of these three factors have been established, under which no runoff is formed. During 64 years of study, runoff was absent for 33 years, ranging from 1 to 146 mm in other years. Among anthropogenic factors, tillage methods and the state of agricultural backgrounds have a profound influence. The runoff regulatory importance of finching and the runoff forming role of perennial grasses and winter crops are discussed. On average, runoff from compacted arable land was 10 mm higher compared to loose chick; in some years the difference was significantly greater. The results of the study are necessary for the design of erosion-control adaptive landscape farming system.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
VOLGA-CASPIAN CANAL IN THE 18TH CENTURY: HISTORICAL AND GEOGRAPHICAL RECONSTRUCTION OF A SHIPPING ROUTE SENSITIVITY OF THE KOLYMA RIVER RUNOFF TO MODERN CLIMATE CHANGE CONDITIONS OF THE OAK FORESTS GROWTH AND CULTIVATION ON THE TOP SURFACES AND SLOPES OF THE NEAR-VOLGA AND ERGENI UPLANDS AND THE PLAINS OF THE SAL-MANYCH INTERFLUVE HEAT BUDGET OF THE BARENTS SEA SURFACE IN WINTER ADAPTATION OF AN AGRICULTURAL PROJECT TO THE REGULATION OF GREENHOUSE GAS EMISSIONS
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1