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浙江大学学报(农业与生命科学版)  2020, Vol. 46 Issue (5): 591-598    DOI: 10.3785/j.issn.1008-9209.2019.11.081
资源利用与环境保护     
浙西石灰岩发育土壤镉的积累及其成土过程中镉的淋失特征
张爽(),章明奎()
浙江大学环境与资源学院,杭州 310058
Cadmium accumulation in soils developed from limestone and leaching characteristics of cadmium during development of the soils in western Zhejiang Province
Shuang ZHANG(),Mingkui ZHANG()
College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
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摘要:

为了解石灰岩风化成土过程中镉的土壤地球化学特征,从浙西地区同时采集3类石灰土表层和剖面分层土样,开展石灰岩丘陵及其附近沟谷地带土壤镉的富集及土壤剖面中镉的垂直分布特征研究;以稳定元素锆为参照,采用物质质量平衡法分析成土过程中土壤镉的淋失特征,并与当地泥页岩发育的黄红壤进行比较。结果表明:石灰岩成土过程中土壤镉同时发生了明显淋失与强烈富集现象。由于石灰岩成土过程比较特殊,土壤中锆和镉呈现明显的富集;石灰岩丘陵及其附近沟谷地带土壤镉的富集量明显高于同一地区泥页岩发育的土壤。3种石灰土剖面土壤镉的垂直分布有明显差异,不同石灰土镉的化学形态也有差异。石灰岩风化过程中土壤镉的高淋失特征及含镉较高的石灰土的地表侵蚀可能是石灰岩分布区及附近地区土壤镉积累较高的主要原因。

关键词: 石灰岩富集淋失地质高背景    
Abstract:

In order to understand the geochemical characteristics of soil cadmium (Cd) during weathering and soil formation of limestone, three types of limestone soils were sampled at the same time from western Zhejiang Province. The Cd enrichment in limestone hills and nearby valleys and the vertical distribution of Cd in the soil profiles were studied. The leaching characteristics of Cd during development of the soils were analyzed by mass balance method with reference to stable element zirconium (Zr), and the results were also compared with those of yellowish red soils developed from local shale. The results showed that the leaching and accumulation of Cd in the limestone soils occurred simultaneously. Because of the special soil-forming process of limestone, the enrichment of Zr and Cd in the soils was obvious, and the enrichment amounts of soil Cd in limestone hills and nearby valleys were obviously higher than that of shale-derived hilly soil in the same area. The vertical distribution of Cd in three kinds of limestone soils had obvious differences and the chemical forms of Cd in different limestone soils were also different. The high leaching characteristics of Cd in the soils during weathering of limestone and the surface erosion of the limestone soils with high Cd content may be the main reasons for the high Cd accumulation in the soils in the limestone distribution area and its vicinity.

Key words: limestone    cadmium    enrichment    leaching    high geological background
收稿日期: 2019-11-08 出版日期: 2020-11-19
CLC:  S 151  
基金资助: 国家重点研发计划专项“农田地质高背景重金属污染机理研究”(2017YFD0800305)
通讯作者: 章明奎     E-mail: 11714047@zju.edu.cn;mkzhang@zju.edu.cn
作者简介: 张爽(https://orcid.org/0000-0003-3945-9655),E-mail:11714047@zju.edu.cn
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引用本文:

张爽,章明奎. 浙西石灰岩发育土壤镉的积累及其成土过程中镉的淋失特征[J]. 浙江大学学报(农业与生命科学版), 2020, 46(5): 591-598.

Shuang ZHANG,Mingkui ZHANG. Cadmium accumulation in soils developed from limestone and leaching characteristics of cadmium during development of the soils in western Zhejiang Province. Journal of Zhejiang University (Agriculture and Life Sciences), 2020, 46(5): 591-598.

链接本文:

http://www.zjujournals.com/agr/CN/10.3785/j.issn.1008-9209.2019.11.081        http://www.zjujournals.com/agr/CN/Y2020/V46/I5/591

统计值

Statistical value

石灰岩丘陵土壤

Soils on limestone

hills (n=38)

石灰岩丘陵附近沟谷土壤

Soils in valley near

limestone hills (n=27)

泥页岩丘陵土壤

Soils on shale

hills (n=27)

泥页岩丘陵附近沟谷土壤

Soils in valley near shale

hills (n=27)

范围 Range/(mg/kg)0.173~3.5410.154~0.6280.105~0.4160.115~0.367

平均值±标准差

Average±standard deviation/(mg/kg)

0.850±0.868a0.315±0.115b0.178±0.073c0.219±0.062bc
变异系数 Coefficient of variation/%102374128
表1  表层土壤镉含量
图1  4种土壤有机质(A)和pH(B)的垂直分布RLS:红色石灰土;BRLS:棕色石灰土;BLLS:黑色石灰土;YRS:黄红壤。
图2  4种土壤黏粒(A)、全镉(B)、全钙(C)和全锆(D)含量的垂直分布RLS:红色石灰土;BRLS:棕色石灰土;BLLS:黑色石灰土;YRS:黄红壤。
图3  4种土壤全钙(A)和全镉(B)的迁移比例RLS:红色石灰土;BRLS:棕色石灰土;BLLS:黑色石灰土;YRS:黄红壤。

土壤类型

Soil type

交换态

Exchangeable form

碳酸盐结合态

Carbonate

bounded form

有机质结合态

Organic matter bounded form

氧化物结合态

Oxide bounded form

残留态

Residual form

红色石灰土 Red limestone soil20.181.8710.3522.9844.62
棕色石灰土 Brown limestone soil11.547.2515.9820.1445.09
黑色石灰土 Black limestone soil9.147.1420.1413.2550.33
黄红壤 Yellowish red soil13.144.1211.8719.8751.00
表2  4种土壤0~5 cm处镉的化学形态及占比 (%)
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