A simple approach to estimate daily loads of total, refractory, and labile organic carbon from their seasonal loads in a watershed

被引:1
作者
Ouyang, Ying [1 ]
Grace, Johnny M., III [2 ]
Zipperer, Wayne C. [3 ]
Hatten, Jeff [4 ]
Dewey, Janet [5 ]
机构
[1] US Forest Serv, Ctr Bottomland Hardwoods Res, Southern Res Stn, USDA, 775 Stone Blvd,Thompson Hall,Room 309, Mississippi State, MS 39762 USA
[2] US Forest Serv, Ctr Forest Watershed Res, Southern Res Stn, USDA, 1740 S Martin Luther King Jr Blvd, Tallahassee, FL 32307 USA
[3] US Forest Serv, Integrating Human & Nat Syst, Southern Res Stn, USDA, 2306 Mowry Rd, Gainesville, FL 32611 USA
[4] Oregon State Univ, Forest Engn Resources & Management, 280 Peavy Hall, Corvallis, OR 97333 USA
[5] Univ Wyoming, Dept Geol & Geophys, Laramie, WY 82071 USA
关键词
Daily load; Labile carbon; Method; Organic carbon; Refractory carbon; DISTURBED CATCHMENTS; TEMPORAL PATTERNS; NEW-ZEALAND; RIVER; MATTER; SOIL; DISCHARGE; TURNOVER; SEDIMENT; DYNAMICS;
D O I
10.1007/s11356-018-2301-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Loads of naturally occurring total organic carbons (TOC), refractory organic carbon (ROC), and labile organic carbon (LOC) in streams control the availability of nutrients and the solubility and toxicity of contaminants and affect biological activities through absorption of light and complex metals with production of carcinogenic compounds. Although computer models have become increasingly popular in understanding and management of TOC, ROC, and LOC loads in streams, the usefulness of these models hinges on the availability of daily data for model calibration and validation. Unfortunately, these daily data are usually insufficient and/or unavailable for most watersheds due to a variety of reasons, such as budget and time constraints. A simple approach was developed here to calculate daily loads of TOC, ROC, and LOC in streams based on their seasonal loads. We concluded that the predictions from our approach adequately match field measurements based on statistical comparisons between model calculations and field measurements. Our approach demonstrates that an increase in stream discharge results in increased stream TOC, ROC, and LOC concentrations and loads, although high peak discharge did not necessarily result in high peaks of TOC, ROC, and LOC concentrations and loads. The approach developed herein is a useful tool to convert seasonal loads of TOC, ROC, and LOC into daily loads in the absence of measured daily load data.
引用
收藏
页码:21731 / 21741
页数:11
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