Urea persistence in floodwater and soil used for flooded rice production

被引:8
作者
Daigh, A. L. [1 ]
Savin, M. C. [2 ]
Brye, K. [2 ]
Norman, R. [2 ]
Miller, D. [2 ]
机构
[1] N Dakota State Univ, Dept Soil Sci, Fargo, ND 58108 USA
[2] Univ Arkansas, Dept Crop & Soil Environm Sci, Fayetteville, AR 72701 USA
关键词
Urea; soil; floodwater; rice; N-(n-butyl)-thiophosphoric triamide; urease inhibitor; nitrogen; NITROGEN; MANAGEMENT; GROWTH;
D O I
10.1111/sum.12142
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Urea is a common fertilizer in delayed-flood rice production in the United States, and its use worldwide has increased dramatically in recent decades. This study aimed to directly quantify urea-N persistence in floodwater and soil used for rice production. We conducted a set of three laboratory experiments to investigate urea-N presence in the floodwater and soil. Untreated urea was applied to dry or wet soil and flooded immediately or urea treated with the urease inhibitor N-(n-butyl)-thiophosphoric triamide (NBPT), or untreated urea was applied to dry soil and flooded after a 5-day delay. Urea-N was analysed colorimetrically (using the microplate-adapted, diacetyl monoxime method) in the floodwater, and at 2-cm intervals in soil after 10-cm long, silt-loam soil columns were flooded for 12, 24, 48 and 96h. The only management practice that led to insignificant urea-N concentrations in floodwaters was the application of urea followed by a 5-day delay before flooding. Urea-N can persist in floodwaters for an estimated 98 and 120h after immediately flooding dry-soil-applied or wet-soil-applied untreated urea, respectively. Urea-N concentrations in floodwaters were up to 33 times less when dry-soil-applied than wet-soil-applied. Average NBPT-treated urea-N concentrations in soil ranged up to 63mg/kg after 24h of flooding and were <1mg/kg after 96h of flooding. The 5-day delay resulted in 1mg urea-N/kg soil when untreated urea was applied. Generally, the threat of N entering adjacent waterways in the form of urea is likely to be limited because of its short-term persistence (120h) in rice floodwater.
引用
收藏
页码:463 / 470
页数:8
相关论文
共 28 条
[21]  
Savin M.C., 2007, BR WELLS RICE RES ST, P325
[22]  
Smil V., 2001, Enriching the Earth: Fritz Haber, Carl Bosch, and the Transformation of World Agriculture
[23]  
Tucker M. R., 1992, SERIES B VIRGINIA AG, V374
[24]  
United States Department of Agriculture-Natural Resource Conservation Service (USDA-NRCS), 2011, OFF SOIL SER DESCR
[25]   THE EFFECT OF SOIL ENVIRONMENT AND FERTILIZER MODIFICATIONS ON THE RATE OF UREA HYDROLYSIS [J].
VLEK, PLG ;
CARTER, MF .
SOIL SCIENCE, 1983, 136 (01) :56-63
[26]   EFFECT OF NITROGEN-SOURCE AND MANAGEMENT ON AMMONIA VOLATILIZATION LOSSES FROM FLOODED RICE-SOIL SYSTEMS [J].
VLEK, PLG ;
CRASWELL, ET .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (02) :352-358
[27]   SEASONAL UPTAKE PATTERNS OF FERTILIZER NITROGEN APPLIED IN SPLIT APPLICATIONS TO RICE [J].
WILSON, CE ;
NORMAN, RJ ;
WELLS, BR .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (06) :1884-1887
[28]   The spatial and temporal characteristics of harmful algal blooms in the southwest Bohai sea [J].
Wu, Zaixing ;
Yu, Zhiming ;
Song, Xiuxian ;
Yuan, Yongquan ;
Cao, Xihua ;
Liang, Yubo .
CONTINENTAL SHELF RESEARCH, 2013, 59 :10-17