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Field Capacity in Black Soil Region, Northeast China

DUAN Xingwu,  XIE Yun,  LIU Gang,  GAO Xiaofei,  LU Hongmei

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文章导航 > Chinese Geographical Science  > 2010 >  20(5): 406-413
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
shu
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
shu

Field Capacity in Black Soil Region, Northeast China

doi: 10.1007/s11769-010-0414-4
  • 1.

    Institute of Natural Science, Yunnan University, Kunming 650091, China;

  • 2.

    State Key Laboratory of Earth Surface Processes and Resource Ecology, School of Geography, Beijing Normal University, Beijing 100875, China

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

  • 1.

    Institute of Natural Science, Yunnan University, Kunming 650091, China;

  • 2.

    State Key Laboratory of Earth Surface Processes and Resource Ecology, School of Geography, Beijing Normal University, Beijing 100875, 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.
    Abstract: 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.
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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
  • 1. Institute of Natural Science, Yunnan University, Kunming 650091, China;
  • 2. State Key Laboratory of Earth Surface Processes and Resource Ecology, School of Geography, Beijing Normal University, Beijing 100875, China
    • 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
  • 收稿日期: 2010-02-01
  • 修回日期: 2010-06-01
  • 刊出日期: 2010-09-15

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
shu
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
shu

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