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[黄土高原黄土区长期施肥条件下土壤 Olsen-P 含量变化趋势及其与磷素盈余和作物产量的关系]

[Soil Olsen-P content changing trend and its relationship with phosphorus surplus and crop yield under long-term fertilization in loessial soil region on the Loess Plateau, China].

作者信息

E Sheng Zhe, Yang Zhi Qi, Zeng Xi Bai, Wang Ya Nan, Luo Zhao Xia, Yuan Jin Hua, Che Zong Xian

机构信息

1 Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China.

2 Institute of Soil and Fertilizer and Save Water Agriculture, Gansu Academy of Agricultural Sciences, Lanzhou 730070, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2017 Nov;28(11):3589-3598. doi: 10.13287/j.1001-9332.201711.037.

Abstract

The changing trend of soil available phosphorus (Olsen-P) content in soil and its relationship with soil phosphorus surplus and crop yield are fundamental when making appropriate phosphate fertilizer recommendations. In this paper, the influences of long-term fertilization on crops phosphorus uptake, soil phosphorus surplus, changing trend of soil available phosphorus content and relationships of soil available phosphorus content with soil phosphorus surplus and crop yield were investigated through 34 years (1981-2015) long-term trial in loessial soil region on the Loess Plateau. The experiment had a completely-randomized-block split-plot design in triplicate. Two main-plot treatments were no farmyard manure and farmyard manure (M), and four subplot treatments were CK (no fertilizer), N (application of chemical fertilizer N), NP (application of chemical fertilizer NP) and NPK (balanced application of chemical fertilizer NPK), respectively. The results showed that fertilization treatments and crop types significantly influenced uptake amount of phosphorus and soil phosphorus surplus. Averaged over time from 1981 to 2015, wheat mean phosphorus uptake amounts of CK, N, NP, NPK, M, MN, MNP and MNPK were 8.63, 10.64, 16.22, 16.21, 16.25, 17.83, 20.39 and 20.27 kg·hm, while rape phosphorus uptakeamounts of eight treatments were 4.40, 8.38, 15.08, 15.71, 10.52, 11.23, 17.96 and 17.66 kg·hm, respectively. The surplus amount of soil phosphorus significantly correlated with the amount of phosphorus applied to soil. When soil phosphorus surplus amount equal zero, wheat and rape phosphorus input amounts were 10.47 kg·hm and 6.97 kg·hm, respectively. Soil phosphorus surplus amount significantly influenced the changing trend of available phosphorus content in soil. CK and N treatments had no phosphorus input, and soil available phosphorus content exhibited a declining trend, annually decreased by 0.16 mg·kg and 0.15 mg·kg, respectively. In contrast, NP, NPK, M, MN, MNP and MNPK six treatments were applied with phosphate fertilizer every years, and available phosphorus content gradually increased along with the duration of trial, with annual increase by 0.02-0.33 mg·kg. Soil available phosphorus content significantly correlated with phosphorus accumulative surplus amount, and the linear models were y=0.012x+9.33 and y=0.009x+11.72 in manure and no manure treatments, respectively. In no manure treatments, wheat yields significantly positively correlated with soil available phosphorus content, however, in manure treatments, their relationships did not reach a significant level. The relationship of wheat grain yield with available phosphorus content could be significantly fitted by piecewise linear model, and available phosphorus agronomy threshold of wheat was 14.99 mg·kg. Rape grain yield also increased with increasing soil available phosphorus content, but the relationship was not significant. This indicated when soil available P content is higher than 14.99 mg·kg , application of phosphate fertili-zer should be reduced or even avoided for planting wheat in loessial soil region on the Loess Plateau.

摘要

在提出合理的磷肥推荐建议时,土壤有效磷(Olsen-P)含量的变化趋势及其与土壤磷盈余和作物产量的关系至关重要。本文通过黄土高原黄土区34年(1981—2015年)的长期试验,研究了长期施肥对作物磷吸收、土壤磷盈余、土壤有效磷含量变化趋势以及土壤有效磷含量与土壤磷盈余和作物产量关系的影响。试验采用完全随机区组裂区设计,重复3次。两个主区处理分别为不施农家肥和施农家肥(M),四个副区处理分别为CK(不施肥)、N(施化肥N)、NP(施化肥NP)和NPK(平衡施用化肥NPK)。结果表明,施肥处理和作物类型对磷吸收量和土壤磷盈余有显著影响。1981—2015年平均来看,小麦在CK、N、NP、NPK、M、MN、MNP和MNPK处理下的平均磷吸收量分别为8.63、10.64、16.22、16.21、16.25、17.83、20.39和20.27 kg·hm,而油菜在这8个处理下的磷吸收量分别为4.40、8.38、15.08、15.71、10.52、11.23、17.96和17.66 kg·hm。土壤磷盈余量与施入土壤的磷量显著相关。当土壤磷盈余量为零时,小麦和油菜的磷输入量分别为10.47 kg·hm和6.97 kg·hm。土壤磷盈余量显著影响土壤有效磷含量的变化趋势。CK和N处理没有磷输入,土壤有效磷含量呈下降趋势,每年分别下降0.16 mg·kg和0.15 mg·kg。相比之下,NP、NPK、M、MN、MNP和MNPK这6个处理每年都施磷肥,有效磷含量随试验年限逐渐增加,每年增加0.02~0.33 mg·kg。土壤有效磷含量与磷累积盈余量显著相关,在施农家肥和不施农家肥处理下的线性模型分别为y=0.012x+9.33和y=0.009x+11.72。在不施农家肥处理中,小麦产量与土壤有效磷含量显著正相关,然而,在施农家肥处理中,它们的关系未达到显著水平。小麦籽粒产量与有效磷含量的关系可用分段线性模型显著拟合,小麦的有效磷农学阈值为14.99 mg·kg。油菜籽粒产量也随土壤有效磷含量的增加而增加,但关系不显著。这表明在黄土高原黄土区种植小麦时,当土壤有效磷含量高于14.99 mg·kg时,应减少甚至避免施用磷肥。

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