[1]郁耀闯,杨树瑶,王长燕,等.宝鸡地区L1-S5黄土和古土壤水分入渗及影响因素[J].水土保持研究,2023,30(06):78-85.[doi:10.13869/j.cnki.rswc.2023.06.010]
　Yu Yaochuang,Yang Shuyao,Wang Changyan,et al.Water Infiltration and Influencing Factors of L1-S5 Loess-Paleosol in Baoji Region[J].Research of Soil and Water Conservation,2023,30(06):78-85.[doi:10.13869/j.cnki.rswc.2023.06.010]
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宝鸡地区L1-S5黄土和古土壤水分入渗及影响因素

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 30 期数: 2023年06期 页码: 78-85 栏目: 出版日期: 2023-10-10
Title:
Water Infiltration and Influencing Factors of L1-S5 Loess-Paleosol in Baoji Region
文章编号:
1005-3409(2023)06-0078-08
作者:
郁耀闯1,2,3, 杨树瑶1,3, 王长燕1,3, 龚兰兰1,3, 赵景波2, 任媛媛1,3, 徐秋月1,3, 侯 英1,3
(1.宝鸡文理学院 地理与环境学院, 宝鸡 陕西 721013; 2.中国科学院 地球环境研究所 黄土与第四纪地质国家重点实验室, 西安 710075; 3.陕西省灾害监测与机理模拟实验室, 宝鸡 陕西 721013)
Author(s):
Yu Yaochuang1,2,3, Yang Shuyao1,3, Wang Changyan1,3, Gong Lanlan1,3, Zhao Jingbo2, Ren Yuanyuan1,3, Xu Qiuyue1,3, Hou Ying1,3
(1.College of Geography and Environment, Baoji University of Arts and Sciences, Baoji, Shaanxi 721013, China; 2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China; 3.Key Laboratory of Disaster Monitoring and Mechanism Simulation of Shaanxi Province, Baoji University of Arts and Sciences, Baoji, Shaanxi 721013, China)
关键词:
土壤入渗;  黄土和古土壤;  古气候变化;  中晚更新统;  宝鸡地区
Keywords:
soil infiltration;  loess and paleosol;  paleo climatic change;  middle and late Pleistocene series;  Baoji Region
分类号:
S152.7; P641
DOI:
10.13869/j.cnki.rswc.2023.06.010
文献标志码:
A
摘要:
[目的]探究宝鸡中晚更新统L1—S5层黄土和古土壤层水分稳定入渗率变化特征及其与土壤容重、土壤初始含水量和土壤毛管孔隙度等土壤属性的关系,为揭示宝鸡中晚更新统L1—S5层黄土和古土壤的入渗规律提供参考依据。[方法]运用双环法进行入渗试验,探讨了宝鸡中晚更新统L1—S5层黄土和古土壤水分入渗的变化特征及其影响因素。[结果](1)宝鸡中晚更新统L1—S5黄土层的平均稳定入渗率(2.38 mm/min)大于古土壤层的平均稳定入渗率(1.55 mm/min),其差异的原因可能与形成时的气候与风化成壤作用的强弱有关。(2)L1—S5层黄土和古土壤层水分入渗试验过程可以用考斯加可夫和通用经验公式进行很好地拟合。(3)土壤容重、土壤初始含水量和土壤毛管孔隙度等土壤属性是影响L1—S5层黄土和古土壤层水分稳定入渗率变化的重要因素。(4)利用土壤容重、土壤毛管孔隙度和毛管最大持水量等土壤参数可以很好地模拟宝鸡中晚更新统L1—S5层黄土和古土壤层的土壤稳定入渗率(R2=0.88,NSE=0.88)。[结论]宝鸡中晚更新统L1—S5层黄土和古土壤层水分稳定入渗率的变化主要由土壤容重、土壤初始含水量和土壤毛管孔隙度等土壤属性的变化所致,利用上述土壤参数可以较好地模拟该区中晚更新统L1—S5黄土和古土壤层土壤稳定入渗率的变化。
Abstract:
[Objective] In order to provide a reference for revealing the infiltration law of the L1—S5 layers of the Baoji loess-paleosol profiles in the middle and late Pleistocene, the variation characteristics of water stable infiltration rate of L1—S5 loess and paleosol in Baoji Middle Late Pleistocene Series and its relationship with soil properties such as soil bulk density, initial soil water content and soil capillary porosity are explored. [Methods] The characteristics and its influencing factors of stable infiltration rate of loess and paleosol in the middle and late Pleistocene of Baoji were studied by double ring method. [Results](1)The average stable infiltration rate(2.38 mm/min)of the loess is higher than that of the paleosol(1.55 mm/min)in the middle and late Pleistocene of the L1—S5 layers of the Baoji loess-paleosol profile, which may be related to the climate change at the time of formation and the strength of the weathering soil.(2)The infiltration experiment of loess and paleosol can be well fitted by using Kosgakov and general empirical formulas in the L1—S5 layers of the Baoji loess-paleosol profile in the middle and late Pleistocene.(3)Soil properties, such as soil bulk density, initial soil water content, saturated soil water content and so on are important factors affecting the stable infiltration rate of loess and paleosol in the L1—S5 layers of the middle and late Pleistocene of Baoji.(4)The soil stable infiltration rate(R2=0.88, NSE=0.88)of loess and paleosol in the L1—S5 layers of the Baoji loess-paleosol profile in the middle and late Pleistocene can be well simulated by using such parameters as soil bulk density, soil capillary porosity, maximum capillary water capacity, total soil porosity, soil saturated water content and soil initial water content. [Conclusion] The changes of stable water infiltration rate of loess and paleosol are mainly caused by the changes of soil bulk density, initial soil water content and capillary porosity. These soil parameters can be used to simulate the changes of stable water infiltration rate of L1—S5 loess and paleosol in the Middle Late Pleistocene in Baoji.

参考文献/References:

[1] Bird M I, Haig J, Hadeen X, et al. Stable isotope proxy records in tropical terrestrial environments[J]. Paleogeography, Palaeoclimatology, Palaeoecology, 2020,538:109445.
[2] Sun Y B, Yan Y, Nie J S, et al. Source-to-sink fluctuations of Asian aeolian deposits since the Late Oligocene[J]. Earth-Science Reviews, 2020,200:102963.
[3] Hou K, Qian H, Zhang Y T, et al. Seepage mechanisms and permeability differences between loess and paleosols in the critical zone of the Loess Plateau[J]. Earth Surface Processes and Landforms, 2021,46(10):2044-2059.
[4] Chen Y, Qian H, Hou K, et al. Permeability and paleoenvironmental implications of loess-paleosol sequence from Jingyang Loess Plateau[J]. Environmental Earth Sciences, 2021,80:1-16.
[5] Shao T J, Wang R J, Xu Z P, et al. Permeability and groundwater enrichment characteristics of the loess-paleosol sequence in the southern Chinese Loess Plateau[J]. Water, 2020,12(3).DOI:10.3390/w12030870.
[6] Wei T T, Fan W, Yuan W W, et al. Three-dimensional pore network characterization of loess and paleosol stratigraphy from South Jingyang Plateau, China[J]. Environmental Earth Sciences, 2019,78(11):123-133.
[7] Feng L, Lin H, Zhang M S, et al. Development and evolution of Loess vertical joints on the Chinese Loess Plateau at different spatiotemporal scales[J]. Engineering Geology, 2020,265:105372.
[8] Schlüter S, Albrecht L, Schwärzel K, et al. Long-term effects of conventional tillage and no-tillage on saturated and near-saturated hydraulic conductivity-Can their prediction be improved by pore metrics obtained with X-ray CT[J]. Geoderma, 2020,361:114082.
[9] Peri'/cZ, Adolphi E L, Stevens T, et al. Quartz OSL dating of late quaternary Chinese and Serbian loess: A cross Eurasian comparison of dust mass accumulation rates[J]. Quaternary International, 2019,502:30-44.
[10] Liu X X, Sun Y B, Vandenberghe J, et al. Palaeoenvironmental implication of grain-size compositions of terrace deposits on the western Chinese Loess Plateau[J]. Aeolian Research, 2018,32:202-209.
[11] Li Y Y, Yang S L, Xiao J L, et al. Hydrogen isotope ratios of leaf wax n-alkanes in loess and floodplain deposits in Northern China since the last glacial maximum and their paleoclimatic significance[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2018,509:91-97.
[12] 赵景波,王长燕,刘护军,等.陕西洛川黄土剖面上部土层水分入渗规律与含水条件研究[J].水文地质工程地质,2010,37(1):124-129,134.
Zhao J B, Wang C Y, Liu H J, et al. A study of water infiltration and water-bearing condition of the L1—S4 layers in Luochuan, Shaanxi[J]. Hydrogeology & Engineering Geology, 2010,37(1):124-129,134.
[13] 王长燕,郁耀闯.黄土丘陵区退耕草地土壤稳定入渗率生长季变化[J].干旱地区农业研究,2017,35(3):107-113.
Wang C Y, Yu Y C. Variation of soil stable infiltration rate in growing season for rehabilitated grassland in loess hilly region[J]. Agricultural Research the Arid Areas, 2017,35(3):107-113.
[14] 杨振奇,秦富仓,李旻宇,等.砒砂岩区不同土地利用类型土壤入渗性能及其影响因素研究[J].生态环境学报,2020,29(4):733-739.
Yang Z Q, Qin F C, Li M Y, et al. Soil infiltration capacity and its influencing factors of different land use types in feldspathic sandstone region[J]. Ecology and Environmental Sciences, 2020,29(4):733-739.
[15] 孙福海,肖波,张鑫鑫,等.黄土高原生物结皮覆盖对土壤积水入渗特征的影响及其模型模拟[J].西北农林科技大学学报:自然科学版,2020,48(10):82-91.
Sun F H, Xiao B, Zhang X X, et al. Effects of biocrust covering on soil water infiltration characteristics on the Loess Plateau and its simulation[J]. Journal of Northwest A&F University: Natural Science Edition, 2020,48(10):82-91.
[16] Mazloom H, Foladmand H. Evaluation and determination of the coefficients of infiltration models in Marvdasht region, Fars Province[J]. International Journal of Advanced Biological and Biomedical Research, 2013,1(8):822-829.
[17] 鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,2000.
Lu R K. Methods of Soil Agricultural Chemical Analysis[M]. Beijing: China Agricultural Science and Technology Press, 2000.
[18] 郑凯利,邓东周.若尔盖湿地土壤入渗性能及其影响因素[J].水土保持研究,2019,26(3):179-184,191.
Zheng K L, Deng D Z. Soil infiltration performance and influencing factors in Zoige Wetland[J]. Research of Soil and Water Conservation, 2019,26(3):179-184,191.
[19] 任宗萍,张光辉,王兵,等.双环直径对土壤入渗速率的影响[J].水土保持学报,2012,26(4):94-97.
Ren Z P, Zhang G H, Wang B, et al. Effects of double-ring diameter on soil infiltration rate[J]. Journal of Soil and Water Conservation, 2012,26(4):94-97.
[20] 宋爱云,董林水,刘世荣,等.不同亚高山草甸群落类型的土壤入渗特征及影响因素[J].水土保持研究,2018,25(3):41-45.
Song A Y, Dong L S, Liu S R, et al. Soil infiltration characteristics and influencing factors of different subalpine meadow community types[J]. Research of Soil and Water Conservation, 2018,25(3):41-45.
[21] 王鹏程,肖文发,张守攻,等.三峡库区主要森林植被类型土壤渗透性能研究[J].水土保持学报,2007,21(6):51-55.
Wang P C, Xiao W F, Zhang S G, et al. Study on soil permeability of main Forest vegetation types in Three Gorges Reservoir area[J]. Journal of Soil and Water Conservation, 2007,21(6):51-55.

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备注/Memo

收稿日期:2022-08-26 修回日期:2022-09-22
资助项目:中国科学院黄土与第四纪地质国家重点实验室项目(SKLLQG1934); 国家自然科学基金(41771048); 宝鸡文理学院博士科研启动费项目(ZK2017042)
第一作者:郁耀闯(1980—),男,河南南阳人,博士,副教授,主要从事气候变化及气溶胶研究。E-mail:yuyaochuang@126.com
通信作者:王长燕(1979—),女,山东烟台人,博士,副教授,主要从事黄土与第四纪地质研究。E-mail:wcyxa_1979@163.com

更新日期/Last Update: 2023-10-10