留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

Field Capacity in Black Soil Region, Northeast China

DUAN Xingwu XIE Yun LIU Gang GAO Xiaofei LU Hongmei

DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. 中国地理科学, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
引用本文: DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. 中国地理科学, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. Chinese Geographical Science, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
Citation: DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. Chinese Geographical Science, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4

Field Capacity in Black Soil Region, Northeast China

doi: 10.1007/s11769-010-0414-4
基金项目: Under the auspices of National Natural Science Foundation of China(No.40671111);Major State Basic Research Development Program of China(No.2007CB407203)
详细信息
    通讯作者:

    XIE Yun.E-mail:xieyun@bnu.edu.cn

Field Capacity in Black Soil Region, Northeast China

Funds: Under the auspices of National Natural Science Foundation of China(No.40671111);Major State Basic Research Development Program of China(No.2007CB407203)
  • 摘要: In this work, 23 black soil profiles were surveyed and 113 soil samples were collected to determine the field capacity (FC) of the black soil in Northeast China. The effectiveness of three methods measuring FC, the Wilcox method (WM), the undisturbed soil pressure plate method (PUM) and the air-dried sieved soil pressure plate method (PDM) were compared to select a suitable laboratory measurement method. Results show that the FC values measured by PDM are greater than those measured by PUM, and the values measured by PUM are greater than those measured by WM. PUM is more suitable for the determination of FC in the study area. One regression equation between PUM and PDM has been established through which undisturbed soil can be replaced by air-dried sieved soil, which is easier to get, to measure FC. FCs vary from 23.50% to 37.00%, with an average of 31.65%, which differ greatly among the 23 black soil profiles. FC is found to be significantly positively correlated with the silt content, clay content and bulk density of the soil, but significantly negatively correlated with the sand content. An empirical pedotransfer function is established to estimate the FC using available soil physical and chemical properties.
  • [1] Acutis M,Donatelli M,2003.SOIL PAR 2.00:Software to estimate soil hydrological parameters and functions.European Journal of Agronomy,18(3-4):373-377.DOI:10.1016/S11610301(02)00128-4
    [2] Addiscott T M,Whitmore A P,1991.Simulation of solute leaching in soils of differing permeability.Soil Use Manage,7(2): 94-102.DOI:10.1111/j.1475-2743.1991.tb00856.x
    [3] Ahuja L R,Naney J W,Williams R D,1985.Estimating soil water characteristics from simpler properties or limited data.Soil Science Society of America Journal,49(4):1100-1105.
    [4] Aina P O,Periaswamy S P,1985.Estimating available water-holding capacity of western nigerian soil from soil texture and bulk density,using core and sieved samples.Soil Science, 140(1):55-58.
    [5] Bell M A,Keulen H V,1996.Effect of soil disturbance on pedotransfer function development for field capacity.Soil Technology,8(4):321-329.DOI:10.1016/0933-3630(95)00032-1
    [6] Bilal C,Ramazan M,Mehmet A et al.,2004.Pedotransfer functions for the estimation of the field capacity and permenent wilting point.Pakistan Journal of Biological Science,7(4): 535-541.
    [7] Cassel D K,Nielsen D R,1986.Field capacity and available water capacity.In:Klute A(ed.).Methods of Soil Analysis:Part I. Physical and Mineralogical Method.Wisconsin,USA:Soil Science Society of America Press,901-926.
    [8] Cassel D K,Ratliff L F,Ritchie J T,1983.Models for estimating in-situ potential extractable water using soil physical and chemical soil properties.Soil Science Society of America Journal,47(4):764-769.
    [9] Cavazza L A,Patruno E C,2007.Field capacity in soils with a yearly oscillating water table.Biosystems Engineering,98(3): 364-370.
    [10] Dane J H,Topp G C(eds.),2002.Methods of Soil Analysis:Part 4.Physical Methods.Wisconsin,USA:Soil Science Society of America Press,684-729.
    [11] Gebregiorgis M F,Savage M J,2006.Field,laboratory and estimated soil-water content limits.Water SA,32(2):155-162.
    [12] Givi J,Prasher S O,Patel R M,2004.Evaluation of pedotransfer functions in predicting the soil water contents at field capacity and wilting point.Agricultural Water Management,70(2): 83-96.DOI:10.1016/j.agwat.2004.06.009
    [13] Gong Zitong,Zhang Ganlin,Chen Zhicheng,2007.Pedogenesis and Soil Taxonomy.Beijing:Science Press,140-144.(in Chinese)
    [14] Hillel D,1998.Environmental Soil Physics.New York:Academic Press,464-468.
    [15] Jabro J D,Evans R G,Kim Y,2009.Estimating in situ soil-water retention and field water capacity in two contrasting soil textures.Irrigation Science,27(3):223-229.DOI:10.1007/s00271-008-0137-9
    [16] Jiang Peifu,Lei Tingwu,Liu Xiaohui et al.,2006.Principles and experimental verification of capillary suction method for fast measurement of field capacity.Transaction of China Society of Agriculture Engineering,22:1-5.(in Chinese)
    [17] Julie M T,Jay M H,1997.Measuring soil water in the laboratory and field with dual-probe heat-capacity sensors.Agronomy Journal,89(4):535-542.
    [18] Kirkham M B,2005.Principles of Soil and Plant Water Relations.San Diego:Elsevier Academic Press,101-110.
    [19] Lal R,2006.Encyclopedia of Soil Science.State of Florida,USA:Taylor&Francis,218-222.
    [20] Li Fapeng,Li Jingyu,Xu Zongxue,2006.The status quo of black soil degradation and water and soil loss in Northeast China. Research of Soil and Water Conservation,13(3):50-54.(in Chinese)
    [21] Liu Baoyuan,Yan Baixing,Shen Bo et al.,2008.Current status and comprehensive control strategies of soil erosion for cultivated land in the northeastern black soil area of China.Science of Soil and Water Conservation,6(1):1-8.(in Chinese)
    [22] Liu Guansong,1996.Soil Physics and Chemistry Analysis and Description of Soil Profiles.Beijing:China Standard Press.(in Chinese)
    [23] Liu Xianchun,Wen Meili,Liu Honghu,2005.Research on soil erosion and prevention and control measurements for black soils in northeastern China.Research of Soil and Water Conservation,12(2):74-79.(in Chinese)
    [24] Ministry of Water Resources of the People's Republic of China, 2007.Technical Standard for Soil Moisture Monitoring.SL 364-2006,10-13.(in Chinese)
    [25] Nan Duan,Zhang Zhiguo,Sun Shoujun,2003.The analysis of soil physical properties in Heilongjiang Province.Heilongjiang Meteorology,20(4):29-31.(in Chinese)
    [26] Ratliff L F,Ritchie J T,Cassel D K,1983.Field-measured limits of soil water availability as related to laboratory-measured properties.Soil Science Society of America Journal,47(4): 770-775.
    [27] Rawls W J,Brakensiek D L,Saxton K E,1992.Estimation of soil water properties.Transactions of the American Society of Agricultural Engineers,25(5):1316-1320.
    [28] Research Group and Cooperative Research Group on Chinese Soil Taxonomy,1995.Chinese Soil Taxonomy(Revised proposal).Beijing:Chinese Agriculture Science and Technology Press,16-52.(in Chinese)
    [29] Romano N,1993.Use of an inverse method and geostatistics to estimate soil hydraulic conductivity for spatial variable analysis.Geoderma,60(3):169-181.DOI:10.1016/0016-7061(93) 90025-G Scott H D,2000.Soil Physics:Agricultural and Environmental Applications.Iowa:Iowa State University Press,350-352.
    [30] Shao Ming'an,Wang Jiuquan,Huang Mingbin,2006.Soil Physics.Beijing:Higher Education Press,143-144.(in Chinese)
    [31] Soil Science Society of America,1997.Glossary of Soil Science Terms.Madison,USA:Soil Science Society of America Press.
    [32] Sumner M E,2000.Hand Book of Soil Science.Boca Raton:CRC Press,64-85.
    [33] The National Soil Survey Office,1995.Soil Species of China(Vol. 2).Beijing:China Agriculture Press,276-454.(in Chinese)
    [34] The National Soil Survey Office,1998.Soils of China.Beijing:China Agriculture Press,318-336.(in Chinese)
    [35] Wang Guanlu,Zhang Guozhi,1983.Soil Knowledge and General Detailed of Soil Survey Technology.Beijing:Water and Electric Power Press.(in Chinese)
    [36] Wosten J H M,Pachepsk Y A,Rawls W J,2001.Pedotransfer functions:Bridging the gap between available basic soil data and missing soil hydraulic characteristics.Journal of Hydrology, 251(3-4):123-150.DOI:10.1016/S0022-1694(01)004644
    [37] Zhu Zuxiang,1996.Agricultural Encyclopedia-soil Volume.Beijing:China Agriculture Press,230-231.(in Chinese)
  • [1] Haoyu DENG, Shaohong WU, Yunhe YIN, Jiangbo GAO, Dongsheng ZHAO.  Eco-geographical Regionalization of China: An Approach Using the Rough Set Method . Chinese Geographical Science, 2022, 32(1): 93-109. doi: 10.1007/s11769-022-1259-3
    [2] ZHENG Yaomin, NIU Zhenguo, GONG Peng, LI Mengna, HU Lile, WANG Lei, YANG Yuxiang, GU Haijun, MU Jinrong, DOU Gejia, XUE Hui, WANG Lin, LI Hua, DOU Gejie, DANG Zhicairang.  A Method for Alpine Wetland Delineation and Features of Border:Zoigê Plateau, China . Chinese Geographical Science, 2017, 27(5): 784-799. doi: 10.1007/s11769-017-0897-3
    [3] YANG Jiuchun, ZHANG Shuwen, CHANG Liping, LI Fei, LI Tianqi, GAO Yan.  Gully Erosion Regionalization of Black Soil Area in Northeastern China . Chinese Geographical Science, 2017, 27(1): 78-87. doi: 10.1007/s11769-017-0848-z
    [4] LI Taijun, LIU Guobin.  Age-related Changes of Carbon Accumulation and Allocation in Plants and Soil of Black Locust Forest on Loess Plateau in Ansai County, Shaanxi Province of China . Chinese Geographical Science, 2014, 0(4): 414-422. doi: 10.1007/s11769-014-0704-3
    [5] MAO Kebiao, MA Ying, XIA Lang, SHEN Xinyi, SUN Zhiwen, HE Tianjue, ZHOU Guanhua.  A Neural Network Method for Monitoring Snowstorm:A Case Study in Southern China . Chinese Geographical Science, 2014, 0(5): 599-606. doi: 10.1007/s11769-014-0675-4
    [6] FAN Ruqin, ZHANG Xiaoping, YANG Xueming, LIANG Aizhen, JIA Shuxia, CHEN Xuewen.  Effects of Tillage Management on Infiltration and Preferential Flow in a Black Soil, Northeast China . Chinese Geographical Science, 2013, 23(3): 312-320. doi: 10.1007/s11769-013-0606-9
    [7] mojiaqi LIN Yihua LIN Wantao CHEN Lihua.  Perturbed Solving Method for Interdecadal . Chinese Geographical Science, 2012, 22(1): 42-47.
    [8] FAN Jie, SUN Wei, ZHOU Kan, CHEN Dong.  Major Function Oriented Zone: New Method of Spatial Regulation for Reshaping Regional Development Pattern in China . Chinese Geographical Science, 2012, 22(2): 196-209.
    [9] SHI Xiaoliang, LI Ying, DENG Rongxin.  The Method Study of Spatial heterogeneity evaluation on the Landscape Pattern Of Farmland Shelterbelt Network . Chinese Geographical Science, 2011, 21(1): 48-56.
    [10] GU Lingjia, ZHAO Kai, ZHANG Shuang, et al..  An AMSR-E Data Unmixing Method for Monitoring Flood and Waterlogging Disaster . Chinese Geographical Science, 2011, 21(6): 666-675.
    [11] ZHENG Xingming, ZHAO Kai.  A Method for Surface Roughness Parameter Estimation in Passive Microwave Remote Sensing . Chinese Geographical Science, 2010, 20(4): 345-352. doi: 10.1007/s11769-010-0407-3
    [12] DENG Yu, LIU Shenghe, WANG Li, MA Hanqing, WANG Jianghao.  Field Modeling Method for Identifying Urban Sphere of Influence: A Case Study on Central China . Chinese Geographical Science, 2010, 20(4): 353-362. doi: 10.1007/s11769-010-0408-2
    [13] CHENG Qinjuan, CAI Qiangguo, MA Wenjun.  Comparative Study on Rain Splash Erosion of Representative Soils in China . Chinese Geographical Science, 2008, 18(2): 155-161. doi: 10.1007/s11769-008-0155-9
    [14] CAO Huicong, WANG Jinda, ZHANG Xuelin.  Ecotoxicity of Cadmium to Maize and Soybean Seedling in Black Soil . Chinese Geographical Science, 2007, 17(3): 270-274. doi: 10.1007/s11769-007-0270-z
    [15] YIN Shu-bai, LU Xian-guo.  THEORY AND METHOD FOR WETLAND BOUNDARY DELINEATION . Chinese Geographical Science, 2006, 16(1): 56-62.
    [16] REN Li-jun, SHANG Jin-cheng.  NECESSITY AND METHOD OF PUBLIC PARTICIPATION IN STRATEGIC ENVIRONMENTAL ASSESSMENT OF CHINA . Chinese Geographical Science, 2005, 15(1): 42-46.
    [17] ZHOU De-min, XU Jian-chun, John RADKE, MU Lan.  A SPATIAL CLUSTER METHOD SUPPORTED BY GIS FOR URBAN-SUBURBAN-RURAL CLASSIFICATION . Chinese Geographical Science, 2004, 14(4): 337-342.
    [18] WANG Ya-qin, WANG Ji-hong.  EFFECT OF ELECTRIC FERTILIZER ON SOIL PROPERTIES . Chinese Geographical Science, 2004, 14(1): 71-74.
    [19] 赵跃龙, 张玲娟.  STUDY ON METHOD OF QUANTITATIVE ASSESSMENT OF FRAGILE ENVIRONMENT . Chinese Geographical Science, 1999, 9(2): 141-145.
    [20] 曹桂发.  THE METHOD BASE OF GEOGRAPHIC ANALYSIS AND ITS APPLICATION . Chinese Geographical Science, 1994, 4(3): 268-276.
  • 加载中
计量
  • 文章访问数:  1323
  • HTML全文浏览量:  4
  • PDF下载量:  1216
  • 被引次数: 0
出版历程
  • 收稿日期:  2010-02-01
  • 修回日期:  2010-06-01
  • 刊出日期:  2010-09-15

Field Capacity in Black Soil Region, Northeast China

doi: 10.1007/s11769-010-0414-4
    基金项目:  Under the auspices of National Natural Science Foundation of China(No.40671111);Major State Basic Research Development Program of China(No.2007CB407203)
    通讯作者: XIE Yun.E-mail:xieyun@bnu.edu.cn

摘要: In this work, 23 black soil profiles were surveyed and 113 soil samples were collected to determine the field capacity (FC) of the black soil in Northeast China. The effectiveness of three methods measuring FC, the Wilcox method (WM), the undisturbed soil pressure plate method (PUM) and the air-dried sieved soil pressure plate method (PDM) were compared to select a suitable laboratory measurement method. Results show that the FC values measured by PDM are greater than those measured by PUM, and the values measured by PUM are greater than those measured by WM. PUM is more suitable for the determination of FC in the study area. One regression equation between PUM and PDM has been established through which undisturbed soil can be replaced by air-dried sieved soil, which is easier to get, to measure FC. FCs vary from 23.50% to 37.00%, with an average of 31.65%, which differ greatly among the 23 black soil profiles. FC is found to be significantly positively correlated with the silt content, clay content and bulk density of the soil, but significantly negatively correlated with the sand content. An empirical pedotransfer function is established to estimate the FC using available soil physical and chemical properties.

English Abstract

DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. 中国地理科学, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
引用本文: DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. 中国地理科学, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. Chinese Geographical Science, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
Citation: DUAN Xingwu, XIE Yun, LIU Gang, GAO Xiaofei, LU Hongmei. Field Capacity in Black Soil Region, Northeast China[J]. Chinese Geographical Science, 2010, 20(5): 406-413. doi: 10.1007/s11769-010-0414-4
参考文献 (37)

目录

    /

    返回文章
    返回