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首页> 外文期刊>Biology and fertility of soils: Cooperating Journal of the International Society of Soil Science >The alleviation of acid soil stress in rice by inorganic or organic ameliorants is associated with changes in soil enzyme activity and microbial community composition
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The alleviation of acid soil stress in rice by inorganic or organic ameliorants is associated with changes in soil enzyme activity and microbial community composition

机译:无机或有机改良剂缓解水稻酸性土壤胁迫与土壤酶活性和微生物群落组成的变化有关

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摘要

The effects of calcium-magnesium phosphate, rock phosphate, lime, fly ash, and animal manure as liming agents on the microbial community composition, enzyme activities involved in C, N, P, and S cycling and rice yields of acid sulfate soils were studied in a three-year field trial. Significant increases in soil pH caused by five ameliorants, particularly lime and fly ash, were observed after 3 years. Both soil exchangeable Al3+ and H+ were significantly (P 0.05) and negatively correlated with soil pH. Increased pH led to 61-102 % increase in rice yield after 2 and 3 years but not after 1 year. Soil phospholipid fatty acid (PLFA) profiles and enzyme activities were significantly changed after 3 years of application of the soil amendments. Enzyme activities increased along gradients of soil pH, indicating that the influences of inorganic or organic ameliorants on soil enzyme activities were mainly due to the effect on soil pH value. PLFA analysis showed that this pH effect played a more important role in shaping microbial community composition than specific effects of organic and inorganic amendments. All rice yield-associated enzymes and PLFA biomarkers (e.g., gram-negative bacteria and actinomycetes) were regulated by soil pH after 3 years. These results revealed that pH-induced changes in soil enzyme activity and microbial composition might be an important mechanism in alleviating acid stress in soil cropped to rice by various ameliorants.
机译:研究了钙镁磷酸盐,磷矿石,石灰,粉煤灰和动物粪便作为石灰剂对酸性硫酸盐土壤微生物群落组成,碳,氮,磷和硫循环涉及的酶活性以及水稻产量的影响。在三年的现场试验中。 3年后观察到由5种改良剂引起的土壤pH值显着增加,尤其是石灰和粉煤灰。土壤可交换的Al3 +和H +均显着(P <0.05),与土壤pH呈负相关。 pH增加导致2年和3年后水稻产量增加61-102%,但1年后没有增加。施用土壤改良剂3年后,土壤磷脂脂肪酸(PLFA)概况和酶活性发生了显着变化。酶活性随土壤pH值的升高而增加,说明无机或有机改良剂对土壤酶活性的影响主要是由于对土壤pH值的影响。 PLFA分析表明,这种pH效应在塑造微生物群落组成方面比有机和无机修饰剂的特定效应更重要。 3年后,所有与水稻产量相关的酶和PLFA生物标志物(例如革兰氏阴性细菌和放线菌)都受到土壤pH的调节。这些结果表明,pH诱导的土壤酶活性和微生物组成的变化可能是减轻各种改良剂对水稻种植土壤的酸胁迫的重要机制。

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