2020
DOI: 10.1007/s11368-019-02508-y
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Responses of organic and inorganic phosphorus fractions in brown earth to successive maize stover and biochar application: a 5-year field experiment in Northeast China

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Cited by 13 publications
(7 citation statements)
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“…A previous study reported stable SOM reported under a minimum tillage system [ 43 ]. Similar to the findings of this study, Cao et al [ 44 ] reported increased recalcitrant NaOH-Po under maize stover retention co-applied with NPK. The higher residual P under MTCrGF probably was due to the transformation of P fractions (from stover residues, goat manure, and inorganic fertilizer), resulting in a build-up of residual P and occluded within soil micro-aggregates.…”
Section: Discussionsupporting
confidence: 91%
“…A previous study reported stable SOM reported under a minimum tillage system [ 43 ]. Similar to the findings of this study, Cao et al [ 44 ] reported increased recalcitrant NaOH-Po under maize stover retention co-applied with NPK. The higher residual P under MTCrGF probably was due to the transformation of P fractions (from stover residues, goat manure, and inorganic fertilizer), resulting in a build-up of residual P and occluded within soil micro-aggregates.…”
Section: Discussionsupporting
confidence: 91%
“…The characteristics of the biochar included a pH of 9.2, total C (TC) content of 660 g kg À1 , total N (TN) content of 12.7 g kg À1 , total P (TP) content of 8.87 g kg À1 , a surface area of 8.9 m 2 g À1 , an ash content of 15.6%, an average pore size of 16.2 nm, a fixed C content of 62.49% and volatile matter of 21.9%. The methods of determining the characteristics of biochar are shown in detail in Cao et al (2020).…”
Section: Preparation and Property Analysis Of Biocharmentioning
confidence: 99%
“…The basic properties of soil were a pH of 7.4, organic matter 13.84 g kg À1 , total N 1.2 g kg À1 and total P 0.38 g kg À1 . The determination of soil properties is shown in detail in Cao et al (2020).…”
Section: Environmental Location and Designmentioning
confidence: 99%
“…The non-labile P fractions which are stable and insoluble P form, such as occluded P (O-P) and apatite P (Ca 10 -P), are known as the unavailable P pools for plant uptake (Cao et al, 2020). The Ca 10 -P fraction is dominated by all the P fractions in the soils.…”
Section: Changes In Soil P Fractionationmentioning
confidence: 99%