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减施矿质氮肥与有机肥替代对滴灌棉田土壤生物学性质及团聚体特征的影响。

[Effect of mineral N fertilizer reduction and organic fertilizer substitution on soil biological properties and aggregate characteristics in drip-irrigated cotton field.].

作者信息

Li Rui, Tai Rui, Wang Dan, Chu Gui-Xin

机构信息

Key Laboratory of Oasis Ecological Agriculture, Xinjiang Production and Construction Group/College of Agronomy, Shihezi University, Shihezi 832003, Xinjiang, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2017 Oct;28(10):3297-3304. doi: 10.13287/j.1001-9332.201710.029.

Abstract

A four year field study was conducted to determine how soil biological properties and soil aggregate stability changed when organic fertilizer and biofertilizer were used to reduce chemical fertilizer application to a drip irrigated cotton field. The study consisted of six fertilization treatments: unfertilized (CK); chemical fertilizer (CF, 300 kg N·hm; 90 kg P2O5 · hm, 60 kg K2 O·hm); 80% CF plus 3000 kg·hmorganic fertilizer (80%CF+OF); 60% CF plus 6000 kg·hmorganic fertilizer (60%CF+OF); 80% CF plus 3000 kg·hmbiofertilizer (80%CF+BF); and 60% CF plus 6000 kg·hmbiofertilizer (60%CF+BF). The relationships among soil organic C, soil biological properties, and soil aggregate size distribution were determined. The results showed that organic fertilizer and biofertilizer both significantly increased soil enzyme activities. Compared with CF, the biofertilizer treatments increased urease activity by 55.6%-84.0%, alkaline phosphatise activity by 53.1%-74.0%, invertase activity by 15.1%-38.0%, β-glucosidase activity by 38.2%-68.0%, polyphenoloxidase activity by 29.6%-52.0%, and arylsulfatase activity by 35.4%-58.9%. Soil enzyme activity increased as the amount of organic fertilizer and biofertilizer increased (i.e., 60%CF+OF > 80%CF+OF, 60%CF+BF > 80%CF+BF). Soil basal respiration decreased significantly in the order BF > OF > CF > CK. Soil microbial biomass C and N were 22.3% and 43.5% greater, respectively, in 60%CF+BF than in CF. The microbial biomass C:N was significantly lower in 60%CF+BF than in CF. The organic fertilizer and the biofertilizer both improved soil aggregate structure. Soil mass in the >0.25 mm fraction was 7.1% greater in 80%CF+OF and 8.0% greater in (60%CF+OF) than in CF. The geometric mean diameter was 9.2% greater in 80%CF+BF than in 80%CF+OF. Redundancy analysis and cluster analysis both demonstrated that soil aggregate structure and biological activities increased when organic fertilizer and biofertilizer were used to reduce chemical fertilizer application. In conclusion, the organic fertilizer and the biofertilizer significantly increased SOC, soil enzyme activity, and soil microbial biomass C and N. The organic fertilizers also improved soil aggregation. Therefore, soil quality could be improved by using these fertilizers to reduce chemical fertilizer application, especially under drip-irrigation.

摘要

进行了一项为期四年的田间研究,以确定在滴灌棉田减少化肥施用量时,使用有机肥和生物肥料对土壤生物学特性和土壤团聚体稳定性有何影响。该研究包括六种施肥处理:不施肥(CK);化肥(CF,300 kg N·hm;90 kg P2O5·hm,60 kg K2O·hm);80%CF加3000 kg·hm有机肥(80%CF+OF);60%CF加6000 kg·hm有机肥(60%CF+OF);80%CF加3000 kg·hm生物肥料(80%CF+BF);60%CF加6000 kg·hm生物肥料(60%CF+BF)。测定了土壤有机碳、土壤生物学特性和土壤团聚体粒径分布之间的关系。结果表明,有机肥和生物肥料均显著提高了土壤酶活性。与CF相比,生物肥料处理使脲酶活性提高了55.6%-84.0%,碱性磷酸酶活性提高了53.1%-74.0%,转化酶活性提高了15.1%-38.0%,β-葡萄糖苷酶活性提高了38.2%-68.0%,多酚氧化酶活性提高了29.6%-52.0%,芳基硫酸酯酶活性提高了35.4%-58.9%。土壤酶活性随有机肥和生物肥料用量的增加而增加(即60%CF+OF>80%CF+OF,60%CF+BF>80%CF+BF)。土壤基础呼吸以BF>OF>CF>CK的顺序显著降低。60%CF+BF处理的土壤微生物生物量碳和氮分别比CF处理高22.3%和43.5%。60%CF+BF处理的微生物生物量碳氮比显著低于CF处理。有机肥和生物肥料均改善了土壤团聚体结构。80%CF+OF处理中>0.25 mm粒径部分的土壤质量比CF处理高7.1%,(60%CF+OF)处理高8.0%。8组CF+BF处理的几何平均直径比80%CF+OF处理大9.2%。冗余分析和聚类分析均表明,使用有机肥和生物肥料减少化肥施用量时,土壤团聚体结构和生物活性增强。总之,有机肥和生物肥料显著提高了土壤有机碳、土壤酶活性以及土壤微生物生物量碳和氮。有机肥还改善了土壤团聚性。因此,使用这些肥料减少化肥施用量可改善土壤质量,特别是在滴灌条件下。

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