Proceedings of the 2016 5th International Conference on Civil, Architectural and Hydraulic Engineering (ICCAHE 2016)

Effects of Different Soil Water Potential at Tillering Stage on Rice Yield and Physiological Traits in Saline-alkali Soil

Authors
Feng Jin, Yanqiu Geng, Shuang Hua, Xiaoxuan Huang, Yueyue Liu, Xiwen Shao
Corresponding Author
Feng Jin
Available Online October 2016.
DOI
10.2991/iccahe-16.2016.1How to use a DOI?
Keywords
rice, tillering stage, saline-alkali soil, water stress, physiological traits, yield
Abstract

To explore the effects of different soil water potential of tillering stage on rice yield and physiological traits in saline-alkali soil, using four treatment levels of soil water potential of 0 kPa (H1: soil moisture), soil water potential of -15 kPa (H2), soil water potential of -30kPa (H3), and CK (continuously flooded), a comparative study of different soil water potential of tillering stage on grain yield, dry matter production, leaf physiological treats and growth dynamic was conducted. The results showed that the period of water stress, the leaf relative water content of the soda saline soil of rice had declined rapidly, and the falling range with the same level of water stress. The H1 had recovering the level of CK after 15days of rewatering. The tiller number from high to low showed a trend of CK>H1>H2>H3 with the drop of water potential in saline-alkali soil, the date of top tillering was the same from CK to H1, but H2 and H3 had 5-10 days later than CK. Water stress could restricted the expansion of the rice leaf area and with the exacerbation of the water stress degree, the rice leaf area index decreased. The date ofH1,H2 and H3 come to maximum LAI were delayed 5days compared with CK. There had a significantly different among all treatments as to the dry matter accumulation, showed a trend of H1>CK>H2>H3, and the difference between H1,CK and H2,H3 had reached significant level(P<0.05).The rice yield from high to low showed a trend of CK>H1>H2>H3, compared with the CK, the H1H2 and H3 decreased 11.45 % , 24.92% and60.24% respectively in the soda saline- alkali soil under moist irrigation at the tillering stage. So in soda saline-alkali soil continuously flooded irrigation is necessary.

Copyright
© 2016, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

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Volume Title
Proceedings of the 2016 5th International Conference on Civil, Architectural and Hydraulic Engineering (ICCAHE 2016)
Series
Advances in Engineering Research
Publication Date
October 2016
ISBN
10.2991/iccahe-16.2016.1
ISSN
2352-5401
DOI
10.2991/iccahe-16.2016.1How to use a DOI?
Copyright
© 2016, the Authors. Published by Atlantis Press.
Open Access
This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

Cite this article

TY  - CONF
AU  - Feng Jin
AU  - Yanqiu Geng
AU  - Shuang Hua
AU  - Xiaoxuan Huang
AU  - Yueyue Liu
AU  - Xiwen Shao
PY  - 2016/10
DA  - 2016/10
TI  - Effects of Different Soil Water Potential at Tillering Stage on Rice Yield and Physiological Traits in Saline-alkali Soil
BT  - Proceedings of the 2016 5th International Conference on Civil, Architectural and Hydraulic Engineering (ICCAHE 2016)
PB  - Atlantis Press
SP  - 1
EP  - 8
SN  - 2352-5401
UR  - https://doi.org/10.2991/iccahe-16.2016.1
DO  - 10.2991/iccahe-16.2016.1
ID  - Jin2016/10
ER  -