Rajagopalan Srinath, Anderson Todd, Cox Stephen, Harvey Greg, Cheng Qiuqiong, Jackson W Andrew
Department of Civil and Environmental Engineering, Texas Tech University, Lubbock, Texas 79409-1023, USA.
Environ Sci Technol. 2009 Feb 1;43(3):616-22. doi: 10.1021/es801737u.
Natural perchlorate is believed to be of atmospheric origin, yet no systematic study has been conducted to evaluate perchlorate deposition rate and possible seasonal or spatial variations. This study evaluated perchlorate concentrations in weekly composite wet deposition samples acquired through the National Atmospheric Deposition Program from 26 sites across the continental United States, Alaska, and Puerto Rico for a 1-3 year period. Perchlorate concentrations varied from <5 ng/L to a high of 102 ng/L with a mean of 14.1 +/- 13.5 ng/L for the 1578 total samples. The annual perchlorate flux by site ranged from a low of 12.5 (TX) to 157 mg/ha-year (NE) and averaged 65 +/- 30 mg/ha-year for all sites. Perchlorate concentrations and flux in wet deposition were generally highest in May-August declining to lows in December-February. Average annual perchlorate flux was correlated (r > 0.5; p < 0.001) with Ca2+, K+, NH4+, NO3(-), Cl(-), and SO4(-2). Wet deposition rate of ClO4(-) in the conterminous United States (excluding Alaska, Hawaii, and Puerto Rico) while diffuse, represents a potential annual net mass flux of 51,000 kg, a value comparable to the estimated annual environmental releases from other known ClO4(-) sources.
天然高氯酸盐被认为源于大气,但尚未进行系统研究来评估高氯酸盐的沉积速率以及可能的季节或空间变化。本研究评估了通过美国国家大气沉积计划,在1 - 3年期间从美国本土、阿拉斯加和波多黎各的26个地点采集的每周混合湿沉降样品中的高氯酸盐浓度。在总共1578个样品中,高氯酸盐浓度从<5纳克/升变化到高达102纳克/升,平均值为14.1±13.5纳克/升。各地点的年高氯酸盐通量范围从低至12.5(德克萨斯州)到157毫克/公顷·年(新英格兰地区),所有地点的平均通量为65±30毫克/公顷·年。湿沉降中的高氯酸盐浓度和通量通常在5月至8月最高,在12月至2月降至最低。年平均高氯酸盐通量与Ca2 +、K +、NH4 +、NO3(-)、Cl(-)和SO4(-2)相关(r>0.5;p<0.001)。在美国本土(不包括阿拉斯加、夏威夷和波多黎各),ClO4(-)的湿沉降速率虽然分散,但代表着每年51,000千克的潜在净质量通量,这一数值与其他已知ClO4(-)来源的估计年度环境释放量相当。