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广西中东部9县区农田土壤As输入通量研究
引用本文:陈雪,杨忠芳,陈岳龙,杨琼,王磊,韦雪姬. 广西中东部9县区农田土壤As输入通量研究[J]. 现代地质, 2019, 33(3): 525-534. DOI: 10.19657/j.geoscience.1000-8527.2019.03.06
作者姓名:陈雪  杨忠芳  陈岳龙  杨琼  王磊  韦雪姬
作者单位:1.中国地质大学(北京) 地球科学与资源学院,北京 1000832.中国人民武装警察部队 黄金地质研究所,河北 廊坊 0650003.广西壮族自治区第四地质队,广西 南宁 5300314.广西土地质量地球化学评价办公室,广西 南宁 5300235.广西地球物理勘察院,广西 柳州 545005
基金项目:广西壮族自治区国土资源厅“广西中东部地区土壤硒元素和重金属元素地球化学研究”(桂国土资发[2015]44 号)
摘    要:对广西中东部9县区农田土壤中的As输入通量进行了初步研究。综合各方面因素,计算获取了大气干湿沉降、施肥和灌溉水输入通量。结果表明,研究区大气干湿沉降和施肥As输入通量基本相当,平均值分别为9.92 g/(hm^2·a)和7.83 g/(hm^2·a),灌溉水通量最高,平均值为14.98 g/(hm^2·a),三者对土壤As污染的贡献率分别为30.31%、23.92%和45.77%。9个不同县区大气干湿沉降、施肥和灌溉水As输入通量占比略有不同,其中6个县区灌溉水和施肥输入通量占主导地位,另外3个县区大气干湿沉降输入通量比例较高。因此,灌溉水是研究区农田土壤As的主要输入途径,应重视灌溉水水质控制。在未考虑农田土壤As输出通量的情况下,以当前的As年平均输入通量估算得到耕层土壤As的质量分数每年升高0.01 mg/kg。与土壤As含量现状相比,As年增量比例很小,因此判断在短期内,外源输入对土壤As分布现状影响不大。该区土壤p H值较低,铁氧化物含量较高,因此外源输入农田土壤的As生物有效性较低。

关 键 词:输入通量  AS  农田土壤  广西
收稿时间:2018-10-30
修稿时间:2019-02-18

Arsenic Input Flux in Farmland Soil of 9 Counties in the Middle East of Guangxi
CHEN Xue,YANG Zhongfang,CHEN Yuelong,YANG Qiong,WANG Lei,WEI Xueji. Arsenic Input Flux in Farmland Soil of 9 Counties in the Middle East of Guangxi[J]. Geoscience of Geosciences, 2019, 33(3): 525-534. DOI: 10.19657/j.geoscience.1000-8527.2019.03.06
Authors:CHEN Xue  YANG Zhongfang  CHEN Yuelong  YANG Qiong  WANG Lei  WEI Xueji
Affiliation:1. School of Earth Sciences and Resources, China University of Geosciences , Beijing 100083, China2. Gold Geological Institute of CAPF, Langfang , Hebei 065000, China3. Geology Team No.4 of Guangxi Zhuang Autonomic Region, Nanning, Guangxi 530031, China4. Project Office of Land Quality Geochemical Assessment of Guangxi, Nanning, Guangxi 530023, China5. Guangxi Geophysical Investigation Institute, Liuzhou , Guangxi 545005, China
Abstract:The input fluxes of As in farmland soil of 9 counties in the middle east of Guangxi were studied.By integrating various factors, the authors took the atmospheric wet and dry depositions, fertilizers and irrigation water as As inputs.Calculation results show that the atmospheric wet and dry depositions and the fertilizers fluxes are about the same, which of the average fluxes are 9.92 g/(hm2·a) and 7.83 g/(hm2·a), while the irrigation water flux is much higher,which of the average flux is 14.98/g/(hm2·a).They contribute 30.31%, 23.92% and 45.77% of As in soil respectively. Their proportions are somewhat different among 9 counties of the study area.The irrigation and fertilizers in 6 counties are dominant, and the proportion of atmospheric wet and dry depositions is higher in the other 3 counties.Therefore, the irrigations is the main input way of As in the study area.Adequate attention should be paid to the water quality controlling.Ignoring the outputs, it is estimated that the As content in farmland soil may increase by 0.01 mg/kg due to the present average flux of arsenic.The proportion of annual As increment in farmland soil is very small, so outside-sourced As will cause little change in As distribution in soil in a short time.The soil of the study area has low pH value and high iron oxides content, so the bioavailability of As is low when it is imported into farmland soil.
Keywords:input flux  As  farmland soil  Guangxi  
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