Scientia Agricultura Sinica ›› 2019, Vol. 52 ›› Issue (21): 3866-3877.doi: 10.3864/j.issn.0578-1752.2019.21.015

• SPECIAL FOCUS: CHANGE OF SOIL PHOSPHRUS AND ITS EFFICIENT UTILIZATION • Previous Articles     Next Articles

Phosphorus Adsorption and Desorption Characteristics and Its Response to Soil Properties of Black Soil Under Long-Term Different Fertilization

WANG Qiong1,2,ZHAN XiaoYing1,3,ZHANG ShuXiang1(),PENG Chang4,GAO HongJun4,ZHANG XiuZhi4,ZHU Ping4,GILLES Colinet2   

  1. 1 Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences/National Engineering Laboratory for Improving Quality of Arable Land, Beijing 100081, China
    2 Gembloux Agro-Bio Tech, University of Liege, Passage des deportes 2, 5030 Gembloux, Belgium
    3 Institute of Environment and Sustainable Development in Agriculture /Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China
    4 Agricultural Environment and Resources Center, Jilin Academy of Agricultural Sciences, Changchun 130033, China
  • Received:2019-07-01 Accepted:2019-08-21 Online:2019-11-01 Published:2019-11-12
  • Contact: ShuXiang ZHANG E-mail:zhangshuxiang@caas.cn

Abstract:

【Objective】 Fertilizer is generally added to agricultural soil to meet the needs of crop production, but long-term over fertilization changes soil phosphorus (P) pool and soil properties. This study evaluated the characteristics change of P adsorption and desorption and its response to soil properties under long-term fertilization, to do a favor to provide theoretical basis of rational fertilizer application and improve the P availability of black soil.【Method】 Four treatments, including no fertilizer (CK), urea and potash sulphate (NK), urea, super-calcium phosphate and potash sulphate (NPK), and NPK plus pig manure (NPKM), were investigated in a 21-year (1989-2010) long-term fertilization experiment at Gongzhuling (Jilin Province) of China. The crop of cropping system was maize. Soil samples were collected in 1990, 2000 and 2010 at 0-20 cm depth to analyze soil properties and to measure soil P adsorption and desorption characteristics. Langmuir equation was used to fit the P adsorption curve, and then the maximum adsorption capacity (Qmax), adsorption constant (K), buffering capacity of soil P (MBC), and P sorption saturation (DPS) were calculated according to Langmuir equation.【Result】 There was a good fitness between the P adsorption curve and Langmuir equation (R 2=0.93-0.99, P<0.01). There existed difference for P adsorption and desorption characteristic under the four treatments. Over time, compared with initial year, for CK and NK treatments, the Qmax value increased by 1.83 and 1.61 times, MBC value increased by 0.80% and 49.40%, DPS value decreased by 92.04% and 87.50%, Readily Desorbable Phosphorus (RDP) value decreased by 20.00% and 82.83%, respectively; for NPK treatment, Qmax and DPS value increased by 81.87% and 79.56%, MBC and RDP value decreased by 79.37% and 48.57%, respectively, while under NPKM treatment, the Qmax and MBC value decreased by 33.35% and 78.52%, DPS and RDP values increased by 11.36 and 1.48 times, respectively. After 21 years experiments, compared with CK and NPK treatments, the Qmax and MBC value of NPKM treatment decreased by 64.66% and 49.52%, 81.87% and 79.56%, respectively; the DPS and RDP value of NPKM treatment increased by 110 and 3.81 times, 4.36 times and 78.57%, respectively. Compared with other treatments, the Total-P, Olsen-P, soil organic matter (SOM) and CaCO3 contents increased and SSA decreased significantly, but the pH, free Fe2O3 and Al2O3 value kept unchanged under NPKM treatment. RDA test showed that SOM and Total-P were the main factors that explained 49.5% and 18.7% of the total variation (P<0.05) which caused the difference of P adsorption desorption characteristic parameters among four treatments.【Conclusion】 Long-term combination of NPK fertilizers with manures could significantly increase SOM and P accumulation contents, decrease the soil adsorption capacity and increase desorption capacity, and improve P availability in soil, but it significantly increased the DPS value, easily thereby caused the risk of phosphorus loss. Therefore, various management practices and inorganic and organic P fertilizer input amounts should be considered to reduce P losses from this area.

Key words: long-term fertilization, black soil, P adsorption and desorption, soil properties

Table 1

Amount of inorganic and organic fertilizer dosage in each treatment"

处理
Treatment
无机肥
Inorganic
N-P2O5-K2O (kg·hm-2)
猪粪 Pig manure
用量
Dosage (t·hm-2)
N-P2O5-K2O
(kg·hm-2)
CK 0-0-0 - -
NK 165-0-68 - -
NPK 165-36-68 - -
NPKM 50-36-68 23-30 115-39-77

Fig. 1

Phosphate isothermal adsorption curves of different treatments in black soils under long-term fertilization. (a) 1990, (b) 2000, (c) 2010"

Table 2

Phosphorus sorption characteristics of different treatments in black soils under long-term fertilization"

年份
Year
处理
Treatment
Langmuir 曲线方程
Langmuir equation
相关系数
R2
最大吸附量
Maximum adsorption capacity (Qmax) (mg·kg-1)
吸附亲和力常数
Adsorption constant K
最大缓冲容量
Max buffering capacity of soil P (MBC) (mg·kg-1)
吸附饱和度
Phosphorus sorption saturation (DPS) (%)
1990 CK C/Q=0.0091Q+0.0778 0.9905 109.96 0.12 12.85 9.71a
NK C/Q=0.0058Q+0.0913 0.9796 170.71 0.06 10.95 6.16a
NPK C/Q=0.0083Q+0.0179 0.9778 120.34 0.46 55.75 8.86a
NPKM C/Q=0.0060Q+0.0914 0.9300 165.34 0.07 10.94 6.58a
2000 CK C/Q=0.0035Q+0.0558 0.9732 283.45 0.06 17.91 1.17b
NK C/Q=0.0038Q+0.0533 0.9520 259.47 0.07 18.77 2.05b
NPK C/Q=0.0058Q+0.0371 0.9611 171.50 0.16 26.94 12.59ab
NPKM C/Q=0.0770Q+0.0198 0.9751 130.01 0.39 50.42 55.62a
2010 CK C/Q=0.0032Q+0.0799 0.9821 311.82a 0.04 12.96a 0.73c
NK C/Q=0.0024Q+0.0600 0.9985 446.23a 0.04 16.36a 0.77c
NPK C/Q=0.0046Q+0.0917 0.9533 218.29ab 0.05 11.5a 16.90b
NPKM C/Q=0.0050Q+0.5000 0.9425 110.19b 0.01 2.35b 81.33a
P value ** * NS * *

Fig. 2

Changes in desorption rate of different treatments in black soils under long-term fertilization"

Fig. 3

Readily desorbable phosphorus (RDP) of different treatments in black soils under long-term fertilization Different capital letters above the bars indicate significantly difference among the different fertilizing years at the same treatment, and the lowercase letter indicated the difference among the different treatments at the same year (P<0.05)"

Fig. 4

RDA showing the relationships between the soil properties and sorption-desorption parameters of different treatments in black soils under long-term fertilization"

Table 3

Mean values of soil properties of different treatments in black soils under long-term fertilization"

指标 Parameter CK NK NPK NPKM P值 P value
全磷Total-P (g·kg-1) 0.56±0.0536b 0.56±0.1037b 0.60±0.0448b 0.94±0.2153a *
有效磷Olsen-P (mg·kg-1) 5.42±0.6431c 6.35±0.1641c 22.99±2.5584b 81.95±4.0825a *
有机质SOM (g·kg-1) 21.58±1.6196b 23.77±2.4263b 24.28±2.4191b 29.91±3.2205a *
酸碱度pH 7.42±0.0504a 6.63±0.1667b 6.38±0.1938b 7.25±0.0764a *
比表面积SSA (m2·g-1) 19.82±0.8184a 15.76±2.7509a 17.06±2.8656a 6.25±0.7227b *
游离氧化铁Free Fe2O3 (g·kg-1) 8.66±0.8741 8.74±1.0689 8.55±0.7679 8.02±1.0075 NS
游离氧化铝Free Al2O3 (g·kg-1) 2.00±0.1927 1.97±0.2463 1.94±0.1550 1.80±0.1898 NS
碳酸钙CaCO3 (g·kg-1) 16.35±0.9500a 13.40±0.9000b 13.90±0.3000b 17.80±0.3000a *

Table 4

The relationship between soil properties and sorption-desorption parameters"

SOM SSA pH Al2O3 Fe2O3 CaCO3 Total-P Qmax K MBC DPS
SSA -0.592
pH -0.040 -0.129
Al2O3 -0.041 -0.181 -0.159
Fe2O3 0.077 -0.218 -0.248 0.954**
CaCO3 0.353 -0.541 0.719** -0.134 -0.150
Total-P 0.678* -0.656* 0.222 -0.198 -0.251 0.581*
Qmax -0.749* 0.624* 0.018 -0.401 -0.401 -0.408 -0.634*
K 0.508 -0.351 -0.144 0.273 0.378 0.005 0.019 -0.447
MBC 0.376 -0.230 -0.199 0.217 0.346 -0.095 -0.145 -0.248 0.969**
DPS 0.815** -0.565 0.197 -0.463 -0.400 0.568* 0.877** -0.511 0.146 0.042
RDP 0.760* -0.744** 0.306 -0.343 -0.249 0.658* 0.752** -0.499 0.342 0.250 0.913**
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