首页|222Rn示踪岩溶湿地地下水排泄及氮磷营养盐输入

222Rn示踪岩溶湿地地下水排泄及氮磷营养盐输入

扫码查看
以会仙湿地八仙湖为研究对象,通过2021年12月(枯水期)和2022年5月(丰水期)的湖水,地下水,沉积物,空气等样品采集,经原位理化性质,氡测量,营养盐等指标的检测,并建立222Rn质量平衡模型,估算八仙湖地下水排泄通量及其营养盐输入.八仙湖222Rn模型的输入项主要为母体226Ra衰变,地下水排泄通量和沉积物扩散量;输出项主要为河流流出通量,湖泊222Rn库衰变量和大气扩散量.通过222Rn质量平衡模型计算得枯水期八仙湖地下水排泄速率约为(110.60±23.75)mm/d,丰水期湖中地下水排泄速率为(238.04±46.58)mm/d.然后通过八仙湖周边地下水平均营养盐浓度,估算枯水期地下水排泄营养盐输入为 NH4+-N(2.24±0.52)× 10-3mol/(m2·d),NO3--N(1.93±0.42)× 10-2mol/(m2·d),TN(1.20±0.26)× 10-1mol/(m2·d),TP(1.97±0.42)× 10-4mol/(m2·d);丰水期地下水排泄营养盐输入为 NH4+-N(1.30±0.25)×10-2mol/(m2·d),NO3--N(2.71±0.53)×10-2mol/(m2·d),TN(2.18±0.43)×10-1mol/(m2·d),TP(4.51±0.89)× 104mol/(m2·d).本研究结果揭示地下水排泄给八仙湖环境带来的影响是不能忽略的,因此在治理会仙湿地环境时应重视地下水排泄对湿地水环境污染的贡献,以期为湿地水资源评价提供基础数据.
Application of radon-222 to assess groundwater discharge and associated nutrients input in the karst wetland
Baxian Lake,located in Huixian Wetland,was taken as the study's object in this paper to investigate the groundwater discharge flux and the associated nutrient input.The samples of lake water,groundwater,sediments,and air collected in December 2021(dry season)and May 2022(wet season)were tested for physical and chemical properties,222Rn and nutrients.The input items of 222Rn in Baxian Lake were 226Ra parent decay,sediment diffusion,and groundwater discharge.The output items included the runoff flux,decay of 222Rn inventory in the lake,and atmospheric diffusion.Then,the 222Rn mass balance model of Baxian Lake was established,and the groundwater discharge rate during the dry season and the rainy season were 110.60±23.75mm/d and 238.04±46.58mm/d,respectively.Based on the average nutrient concentration of groundwater around Baxian Lake,the nutrients flux from the groundwater discharge during the dry season were estimated as follows:(2.24±0.52)×10-3mol/m2×d(NH4+-N),(1.93±0.42)×10-2mol/(m2·d)(NO3--N),(1.20±0.26)×10-1mol/(m2·d)(TN),(1.97±0.42)×10-4mol/(m2·d)(TP).The nutrient fluxes from the groundwater discharge during the wet season were:(1.30±0.25)×10-2mol/(m2·d)(NH4+-N),(2.71±0.53)×10-2mol/(m2·d)(NO3--N),(2.18±0.43)×10-1mol/(m2·d)(TN),(4.51±0.89)×10-4mol/(m2·d)(TP).This study provides important information for water circulation and water ecosystem for the water resource management of Huixian Wetland.

Huixian karst wetlandradon isotopesgroundwater dischargenutrient inputs

张启元、赵雨晴、李远俊、李鑫鹏

展开 >

桂林理工大学环境科学与工程学院,广西桂林 541004

桂林理工大学,岩溶地区水污染控制与用水安全保障协同创新中心,广西桂林 541004

会仙岩溶湿地 氡同位素 地下水排泄 营养盐输入

广西科技基地和人才专项广西科技基地和人才专项

RZ2100002009RZ2300150851

2024

中国环境科学
中国环境科学学会

中国环境科学

CSTPCDCHSSCD北大核心
影响因子:2.174
ISSN:1000-6923
年,卷(期):2024.44(6)
  • 55