|Table of Contents|

Effect of Water Treatments on Soil Water Dynamics in Soybean Field of Mollisols Area in Northeast China(PDF)

《大豆科学》[ISSN:1000-9841/CN:23-1227/S]

Issue:
2014年01期
Page:
73-78
Research Field:
Publishing date:

Info

Title:
Effect of Water Treatments on Soil Water Dynamics in Soybean Field of Mollisols Area in Northeast China
Author(s):
YANG Chun-bao1ZOU Wen-xiu2JIANG Heng23HAN Xiao-zeng2HAO Xiang-xiang2LI Meng2
1.Collage of Resources and Environment,Northeast Agricultural University,Harbin 150030,China;2.Key Laboratory of Mollisols Agroecology,National Observation Station of Hailun Agroecology System,Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences,Harbin 150081,China;3.Graduate School of the Chinese Academy of Sciences,Beijing 100049,China
Keywords:
Soil water entryVariation coefficientSoil water storageSoil water regulation
PACS:
S565.1
DOI:
10.11861/j.issn.1000-9841.2014.01.0073
Abstract:
Black soil had strong water capacity.The impact of different water entry amount(precipitation+irrigation)including excessive water(I1),suitable water(I2),drought(I3)and rainfed(R)treatments on the migration of soil water in soil profile was conducted based on controlled water treatment located in Hailun Agricultural Ecology Station of Chinese Academy of Sciences.The soil profile impacted by different water entry amount was as deep as 130 cm.For I1 treatment,the water infiltrated depth was 110 cm and the accumulated water entry was as high as 514 mm during soybean growing season.Compared with other treatments,soil water storage in 0-90 cm soil layer reduced 38 mm in I3,suggesting soil water stored in 0-90 cm soil layer could be utilized by soybean under drought stress.The similar temporal variation of soil water storage in 0-150 cm soil layer was observed in R and I1,I2 and I3,respectively.Therefore,the variation of soil water in soil profile was affected by the frequency and amount of water entry,water cycle depth increased when soil was in drought status.It also suggested that black soil has strong soil water regulation capacity,which was very important for the occurrence of seasonal drought.

References:

[1]韩晓增,王守宇,宋春雨,.海伦地区黑土农田土壤水分动态平衡特征研究[J].农业系统科学与综合研究,2003,19(4):252-255.(Han X Z,Wang S Y,Song C Y,et al.Research of feature of the dynamic balance on the soil moisture in farmland of black soil in Hailun district[J].System Science and Comprehensive Studies in Agriculture,2003,19(4):252-255.)

[2]孟凯,张兴义,隋跃宇,等.黑龙江海伦农田黑土水分特征[J].土壤通报,2003,34(1):11-14.(Meng K,Zhang X Y,Sui Y Y,et al.Black soil water characteristic in Hailun,Heilongjiang[J].Chinese Journal of Soil Science,2003,34(1):11-14.)

[3]陈宝群,赵景波.黄土高原土壤水分环境评价初步研究[J].干旱区资源与环境,2010,24(5):184-189.(Chen B Q,Zhao J B.Soil moisture environmental assessment in Loess Plateau[J].Journal of Arid Land Resources and Environment,2010,24(5):184-189.)

[4]杨新民.黄土高原灌木林地水分环境特性研究[J].干旱区研究,2001,18(1):8-13.(Yang X M.Study on the characteristics of water environmental in shrubbery land of Loess Plateau[J].Arid Zone Research,2001,18(1):8-13.)

[5]李笑吟,毕华兴,李俊,.晋西黄土区土壤剖面水分动态研究[J].中国水土保持科学,2006,4(4):72-77.(Li X Y,Bi H X,Li J,et al.Dynamics of moisture of soil profile in Loess area of western Shanxi[J].Science of Soil and Water Conservation,2006,4(4):72-77.)

[6]李洪建,王孟本,柴宝峰.黄土高原土壤水分变化的时空特征分析[J].应用生态学报,2003,14(4):515-519.(Li H J,Wang M B,Chai B F.Spatial and temporal characteristics of soil moisture dynamics in Loess Plateau[J].Chinese Journal of Applied Ecology,2003,14(4):515-519.)


[7]邹文秀,韩晓增,江恒,.东北黑土区降水特征及其对土壤水分的影响[J].农业工程学报,2011,27(9):196-202.(Zou W X,Han X Z,Jiang H,et al.Characteristics of precipitation in black soil region and response of soil moisture dynamics in Northeast China[J].Transactions of the Chinese Society of Agricultural Engineering,2011,27(9):196-202.)

[8]Ekren S,S-nmez z-akal E,et al.The effect of different irrigation water levels on yield and quality characteristics of purple basil[J].Agricultural Water Management,2012,109:155-161.

[9]Daniel W,Georgr V.Effect on a single irrigation at different reproductive growth stages on soybean planted in early July and late June[J].Irrigation Sciences,2002,21:69-73.

[10]Korte L L,Specht J E,Williams J H,et al.Irrigation of soybean genotypes during reproductive ontogeny.II.Yield component responses[J].Crop Science,1983,23:528-533.

[11]Korte L L,Williams J H,Specht J E,et al.Irrigation of soybean genotypes during reproductive ontogeny.I.Agronomic responses[J].Crop Science,1983,23:521-527.

[12]邹文秀,韩晓增,王守宇,.降水年型对黑土区土壤水分动态变化的影响[J].水土保持学报,2009,23(5):138-142.(Zou W X,Han X Z,Wang S Y,et al.Impact of different yearly rainfall patterns on dynamic changes of soil moisture in black soil region[J].Journal of Soil and Water Conservation,2009,23(5):138-142.)

[13]邹文秀,韩晓增,王守宇,.长期施肥对大豆地土壤蒸发和水分利用效率的影响[J].大豆科学,2009,28(3):487-490,494.(Zou W X,Han X Z,Wang S Y,et al.Effect of long-term fertilization on soil evaporation and water use efficiency in soybean field[J].Soybean Science,2009,28(3):487-490,494.)

[14]王风,乔云发,韩晓增,.冻融过程黑土2m土体固液态水分含量动态特征[J].水科学进展,2008,19(3):361-366.(Wang F,Qiao Y F,Han X Z,et al.Study on the dynamic characteristics of solid and liquid water in the process of freezing-thawing in black soil[J].Advances in Water Science,2008,19(3):361-366.)

[15]邹文秀,韩晓增,王守宇,.不同水分处理下农田黑土水分特征[J].生态与农村环境学报,2009,25(3):35-38.(Zou W X,Han X Z,Wang S Y,et al.Effect of water treatment on water regime in farm land black soil[J].Journal of Ecology and Rural Environment,2009,25(3):35-38.)


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Last Update: 2014-08-04