Smith Lisa M, Engle Virginia D, Summers J Kevin
USEPA Gulf Ecology Division, Gulf Breeze, FL, USA.
Environ Monit Assess. 2006 Apr;115(1-3):291-305. doi: 10.1007/s10661-006-6555-3. Epub 2006 Apr 13.
The U.S. Environmental Protection Agency Environmental Monitoring and Assessment Program (EMAP) uses water clarity as a water quality indicator for integrated assessments of coastal waters. After the publication of the first National Coastal Condition Report (USEPA, 2001c), the national water clarity reference value of 10% of ambient surface light at 1 m depth was reevaluated and modified to reflect expected differences in regional reference light conditions. These regional differences range from naturally turbid estuaries like those found in Mississippi and Louisiana to clear water estuaries expected to support extensive beds of submerged aquatic vegetation in, e.g., Florida and Tampa Bays. For the second National Coastal Condition Report, water clarity was assessed based on regional reference values (USEPA, 2004). Different regional water clarity reference values and data collection methods necessitated the development of a water clarity index based on light attenuation coefficients (k). This index incorporates regional reference conditions and is interchangeable with secchi depth and percent light transmission calculated from light meter measurements. Evaluation of the water clarity index shows that k values based on transmissivity at 1 m can be estimated from secchi depth measurements and successfully used as a surrogate for transmissivity calculated from light meter data. An approach for assessing water clarity in Gulf of Mexico estuaries using light meter data and secchi depth is presented.
美国环境保护局环境监测与评估计划(EMAP)将水体透明度用作沿海水域综合评估的水质指标。在第一份《国家沿海状况报告》(美国环境保护局,2001c)发布后,对1米深度处环境表面光的10%这一国家水体透明度参考值进行了重新评估和修改,以反映区域参考光照条件的预期差异。这些区域差异范围从像密西西比州和路易斯安那州那样自然浑浊的河口,到预期能支持大量沉水水生植被床的清澈河口,比如佛罗里达州和坦帕湾的河口。对于第二份《国家沿海状况报告》,水体透明度是根据区域参考值进行评估的(美国环境保护局,2004)。不同的区域水体透明度参考值和数据收集方法使得有必要开发一种基于光衰减系数(k)的水体透明度指数。该指数纳入了区域参考条件,并且与根据光度计测量计算得出的塞氏盘深度和透光率百分比可互换。对水体透明度指数的评估表明,基于1米处透光率的k值可以从塞氏盘深度测量值估算出来,并成功用作根据光度计数据计算得出的透光率的替代指标。本文介绍了一种利用光度计数据和塞氏盘深度评估墨西哥湾河口水体透明度的方法。