Nine-year organic fertilization enhances poorly crystalline iron hydroxide formation and phosphorus availability in a temperate rice–wheat cropping system

Jiali Qin, Xinci Han, Zhixin Jia, Yunyan Li, Dandan Zhang, Lina Li, Junyu Xie, Li Li, Tingliang Li, Xiaolei Huang, Ning Ling, Guanghui Yu
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Abstract

Phosphorus (P) is typically associated with iron (Fe) hydroxides in paddy soils. Our study investigated the impact of different fertilization treatments on the availability of P regulated by Fe redox transformation in a rice (Oryza sativa L.)–wheat (Triticum aestivum L.) cropping system in the mid-low reaches of the Yangtze River. Five fertilization treatments were examined: control (CK), chemical fertilizer (CF), 35% CF (P) plus pig manure compost (CFM), 100% CF (P) plus straw (CFS), and 35% CF (P) plus pig manure compost and straw (CFMS). Nine-year rice–wheat rotations increased the oxalate-extractable poorly crystalline Fe hydroxides (i.e., Feo) by 33%–87% compared with the initial soil, while fertilization further accelerated this process. Compost application increased the proportion of labile P by 75%–108% and decreased the proportion of non-labile P by 14%–22% compared with the single chemical fertilization treatment. Furthermore, organic fertilization increased the mass proportions of macroaggregates and macroaggregate-associated labile P. The Feo was positively correlated with the content of labile P but negatively correlated with the proportion of non-labile P. Moreover, the reductive dissolution of Fe hydroxides was accompanied by the transformation of P from NaOH-extractable to NaHCO3- and H2O-extractable phases. These results indicate that seasonal alternation of drying and wetting can progressively drive the redox transformation of Fe hydroxides and promote the formation of Feo, thereby affecting the availability of P. Therefore, we suggested that P fertilizer should be reduced in the rice season due to the reduction of Fe hydroxides, particularly in the compost-amended soils in the temperate rice–wheat cropping system.

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九年有机施肥提高了温带稻麦种植系统中结晶性差的氢氧化铁的形成和磷的有效性
在水稻土中,磷(P)通常与铁(Fe)氢氧化物伴生。本研究研究了长江中下游水稻-小麦系统不同施肥处理对铁氧化还原转化调控的磷有效性的影响。试验采用对照(CK)、化肥(CF)、35% CF (P) +猪粪堆肥(CFM)、100% CF (P) +秸秆(CFS)、35% CF (P) +猪粪堆肥+秸秆(CFMS) 5种施肥处理。与初始土壤相比,9年稻麦轮作使草酸盐可提取的低结晶铁氢氧化物(即Feo)增加了33%-87%,而施肥进一步加速了这一过程。与单一施肥相比,施用堆肥可使土壤中不稳定磷的比例提高75% ~ 108%,使土壤中不稳定磷的比例降低14% ~ 22%。有机肥增加了大团聚体和大团聚体伴生的活性磷的质量比例,Feo与活性磷含量呈正相关,与非活性磷含量呈负相关。铁氢氧化物的还原溶解伴随着磷从naoh可萃取相向NaHCO3-相和h2o可萃取相的转变。上述结果表明,季节干湿交替可逐步推动铁氢氧化物的氧化还原转化,促进Feo的形成,从而影响磷的有效性。因此,我们建议,由于铁氢氧化物的减少,应在水稻季节减少磷肥,特别是在温带稻麦种植系统中堆肥改良的土壤中。
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