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不同灌溉时长的污水灌溉土壤的特性以及碳氮动态

Characteristics, and carbon and nitrogen dynamics in soil irrigated with wastewater for different lengths of time.

作者信息

Ramirez-Fuentes E, Lucho-constantino C, Escamilla-Silva E, Dendooven L

机构信息

Department of Biotechnology and Bioengineering, Cinvestav, Instituto Politécnico Nacional, Mexico DF.

出版信息

Bioresour Technol. 2002 Nov;85(2):179-87. doi: 10.1016/s0960-8524(02)00035-4.

Abstract

Irrigation of agricultural land with wastewater will increase crop production, but also heavy metal concentrations and the rate of infection of farmers with pathogens. The risks associated with the use of wastewater are reduced by treating the wastewater, but treatment also reduces organic material, phosphorus and inorganic N for crops. We investigated characteristics, e.g. heavy metal concentrations, of soils of the valley of the Mezquital (Mexico) irrigated with waste from Mexico City water since 1912, 1925, 1965, 1976, 1996 or 1997, or not irrigated at all, and dynamics of C and N when soil was amended with wastewater or drainage water. Concentrations of total Mg, Hg, Mo, Ca, Cu and Cr, available concentrations of Pb, Cd and Cu increased significantly with length of irrigation (P < 0.05), but were not at hazardous concentrations. Although organic C, total N, microbial biomass C and N, and microbial activity, as witnessed by CO2 production, increased with length of irrigation, N mineralization did not. Oxidation of NO2- was inhibited and could be due to increases in salinity, toxic compounds or heavy metals. We found that N mineralization was low or absent so it will not compensate for the loss of N when the wastewater is treated and application of N fertilizer will be required to maintain the same level of crop production. The characteristics of the soils appear not to have deteriorated after years of application of wastewater, but further irrigation even with treated wastewater might increase sodicity and salinity and pose a threat to future crop production.

摘要

用废水灌溉农田会增加作物产量,但也会提高重金属浓度以及农民感染病原体的几率。通过处理废水可降低使用废水带来的风险,但处理过程也会减少用于作物的有机物质、磷和无机氮。我们调查了自1912年、1925年、1965年、1976年、1996年或1997年以来用墨西哥城水的废水灌溉的(墨西哥)梅斯基塔尔山谷土壤的特性,如重金属浓度,以及从未灌溉过的土壤特性,还研究了用废水或排水改良土壤时碳和氮的动态变化。总镁、汞、钼、钙、铜和铬的浓度,铅、镉和铜的有效浓度随灌溉时长显著增加(P < 0.05),但未达到危险浓度。尽管有机碳、总氮、微生物生物量碳和氮以及由二氧化碳产生所表明的微生物活性随灌溉时长增加,但氮矿化并未增加。亚硝酸根的氧化受到抑制,这可能是由于盐度、有毒化合物或重金属增加所致。我们发现氮矿化程度低或不存在,因此在处理废水时它无法弥补氮的损失,需要施用氮肥来维持相同的作物产量水平。经过多年废水灌溉后,土壤特性似乎并未恶化,但即使使用处理后的废水进一步灌溉也可能会增加土壤碱化度和盐度,对未来作物生产构成威胁。

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