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[水旱轮作下土壤剖面中溶解有机物质的垂直分级]

[Vertical fractionation of dissolved organic matter in soil profile under water-dry cultivation].

作者信息

Zhan Xinhua, Cui Chunhong, Lu Yanyu, Zhou Lixiang

机构信息

College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2004 Jun;15(6):1025-9.

Abstract

Dissolved organic matter (DOM) is the most active component of organic matters, and plays an important role in the translocation and transformation of pollutants and nutrients in terrestrial ecosystem. In this paper, the vertical fractionation of DOM in a yellow brown soil under water-dry cultivation was investigated by field experiment and physico-chemical analyses. The results showed that in treatments CK, chemical fertilizer and sewage sludge, the DOM concentration decreased from 145.8, 117.7 and 114.8 mg x kg(-1) to 21.57, 23.23 and 13.78 mg x kg(-1) with soil depth, respectively. In control and fertilizer-treated soils, the hydrophilic fraction of DOM was increased respectively from 19.01% and 18.47% to 34.97% and 44.37% with soil depth, and the biodegradable rate of DOM also increased with soil depth. In sludge-treated soil, a reverse tendency was found for the concentration of hydrophilic DOM and its biodegradable rate. Hydrophilic fraction decreased from 36.96% to 17.07%, the increase of hydrophobic fraction was from 63.04% to 82.93%, and the biodegradable rate decreased from 53.19% to 30.75% with soil depth. The biodegradable rate of DOM was positively correlated to the hydrophilic fraction of DOM, and UV spectra analysis also suggested this.

摘要

溶解性有机物(DOM)是有机物中最活跃的成分,在陆地生态系统中污染物和养分的迁移转化过程中发挥着重要作用。本文通过田间试验和理化分析,研究了水旱轮作条件下黄棕壤中DOM的垂直分馏情况。结果表明,在对照、化肥和污泥处理中,DOM浓度分别随土壤深度从145.8、117.7和114.8 mg x kg(-1)降至21.57、23.23和13.78 mg x kg(-1)。在对照和化肥处理的土壤中,DOM的亲水性组分分别随土壤深度从19.01%和18.47%增加到34.97%和44.37%,DOM的生物降解率也随土壤深度增加。在污泥处理的土壤中,亲水性DOM浓度及其生物降解率呈现相反的趋势。亲水性组分随土壤深度从36.96%降至17.07%,疏水性组分从63.04%增加到82.93%,生物降解率从53.19%降至30.75%。DOM的生物降解率与DOM的亲水性组分呈正相关,紫外光谱分析也表明了这一点。

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