[Construction effect of fertile cultivated layer in albic soil Ⅰ Effects of inversion tillage with organic mate-rials on the redistribution of organic matter in surface layer of albic soil].

Q3 Environmental Science
Rui-Min Gao, Jun Yan, Xiao-Zeng Han, Xu Chen, Wen-Xiu Zou, Xin-Chun Lu, Yong-Jie Piao, Rui Jiang
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引用次数: 0

Abstract

Soil organic matter serves as a crucial indicator for soil quality. Albic soil, characterized by a barrier layer, exhibits limitations in organic matter content, which can adversely affect crop growth and development. To elucidate the impact of deep mixing of various organic materials on the redistribution of organic matter in the surface soil of albic soil could provide theoretical and technical insights for establishing suitable plough layers for albic soil in Northeast China. We conducted a two-year positioning experiment in Shuangyashan, Heilongjiang Province with five treatments, conventional shallow tillage (0-15 cm, CK), inversion tillage (0-35 cm) without or with straw return (T35 and T35+S), inversion tillage with cattle manure (T35+M) and cattle manure plus maize straw (T35+S+M). The results showed that soil fertilization via deep mixing of organic materials to a depth of 35 cm significantly increased maize yield in albic soil, with the T35+S+M treatment demonstrating the most pronounced effect, yielding an average production of 2934.76 kg·hm-2. Compared to CK, the T35 treatment resulted in a significant 8.4% decrease in organic matter content in the tillage layer, a significant 7.6% increase in organic matter in the sub-tillage layer, and a relative richness degree of soil organic matter in the sub-tillage layer increased by 17.5%. Deep mixed return of organic materials following deep ploughing markedly increased organic matter content of the plough layer, with organic matter conversion ranging from 16.3% to 31.0%. In comparison to the T35 treatment, there was no significant increase in soil organic matter content in the T35+S tillage layer and sub-tillage layer. Conversely, soil organic matter content increased by 4.6% and 6.9% in the T35+M and T35+S+M treatments, with corresponding increase of 11.2% and 15.4% in sub-tillage layer, respectively. Additionally, the soil organic matter richness index in sub-tillage layer increased by 2.5% and 5.1%, respectively. There was a significant positive correlation between organic matter content in the entire plough layer and maize yield, with a contribution rate of 17.5%. Therefore, the utilization of organic fertilizer or a combination of organic fertilizer and straw deep mixing can quickly fertilize albic soil by increasing soil organic matter content in both the whole tillage layer (0-35 cm) and the sub-tillage layer (15-35 cm).

[白化土壤肥沃耕作层的构建效应 Ⅰ 使用有机辅料翻耕对白化土壤表层有机质重新分布的影响]。
土壤有机质是衡量土壤质量的重要指标。白化土壤的特点是有阻隔层,有机质含量有限,会对作物生长发育产生不利影响。阐明各种有机物深层混合对白化土壤表层土壤有机质再分布的影响,可为东北地区建立适合白化土壤的耕层提供理论和技术启示。我们在黑龙江省双鸭山市进行了为期两年的定位试验,共设五个处理,分别为常规浅耕(0-15 厘米,CK)、不加或加秸秆还田的反耕作(0-35 厘米)(T35 和 T35+S)、加牛粪的反耕作(T35+M)和牛粪加玉米秸秆(T35+S+M)。结果表明,在白化土壤中,将有机物深层混合 35 厘米的土壤施肥可显著提高玉米产量,其中 T35+S+M 处理效果最明显,平均产量达 2934.76 kg-hm-2。与 CK 相比,T35 处理使耕作层有机质含量显著减少 8.4%,耕作层下有机质显著增加 7.6%,耕作层下土壤有机质相对富集度增加 17.5%。深耕后有机物的深层混合还田显著提高了耕作层的有机质含量,有机质转化率从 16.3% 到 31.0%。与 T35 处理相比,T35+S 耕层和底耕层的土壤有机质含量没有显著增加。相反,在 T35+M 和 T35+S+M 处理中,土壤有机质含量分别增加了 4.6% 和 6.9%,耕作层下的土壤有机质含量也相应增加了 11.2% 和 15.4%。此外,底耕层土壤有机质富集指数也分别增加了 2.5%和 5.1%。整个耕作层的有机质含量与玉米产量之间存在明显的正相关,贡献率为 17.5%。因此,施用有机肥或将有机肥与秸秆深翻混合施用,可通过增加全耕层(0-35 厘米)和亚耕层(15-35 厘米)的土壤有机质含量,快速培肥白化土壤。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
自引率
0.00%
发文量
11393
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