Source Analysis of Nitrate Nitrogen in Groundwater Based on Different Modes of Land use

L. Zejun, W. Yan, Liang Qiyang, J. Xia, Jian Li, Yong Huang
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Abstract

The study area is located in the Hebei province Luanxian section along the Luanhe River. The right of Luanhe River is arranged with 3 monitoring sections and is laid with 5 wells in the A-A section and B-B section and 1 well on the floodplain (inside the dike), the distance from the river level is about 10m. The distance between the 4 wells outside the dike is 20m, 50m, 200m and 1500m respectively. 2 wells are arranged on the C-C section, so there are 13 observation wells in the study area. 3# wells and 11# wells have used existing monitoring wells, so 11 wells have been set up actually. The monitoring wells are designed to monitor groundwater level, groundwater quality and isotope analysis. In the upstream of Luanhe’s A-A section of the No. 4 well near the edge of the woods and downstream of the B-B section of the No. 8 well near the edge of farmland (wheat), each point of soil is sampled to determine the content of nitrate nitrogen and 15N isotope ratio in soil profile. The depth of soil is sampled from surface to groundwater level, the total depth is about 2.5m. Taking about 1kg soil samples at 20cm every time from the ground surface and collect and seal in plastic bags and number. The sampling time was November 2015, March 2016, May 2016 and July 2016, taking 4 times. The analysis showed that higher nitrate content in soil is within 0-60cm, and is same as the depth of fertilizing the crops (including animal manure), so when estimating the proportion of groundwater in nitrate, nitrate content in 0-60cm is assumed as the initial value; which is close to the underground water level in the soil and is regarded as the final value of 60cm, that is, the final value of nitrate into the groundwater, which can estimate the soil nitrate into groundwater ratio. The sources of nitrate in groundwater are complex and related to many factors, such as river water, soil and so on. According to the content of nitrogen and oxygen isotopes, it determines the main source of nitrate nitrogen:soil and Luanhe River. The results showed that the ratio of nitrate to groundwater in the forest soil was 20%~80.8%, and the average value was 56.3%. The proportion of nitrate in the soil in the wheat field was 6.8%~98.2%, with an average value of 48.3%. Nitrate nitrogen from water in proportion of large changes with the seasons, the upper reaches of the Luanhe River (near No. 2 wells) for 0~19.6%; the Luanhe River (near No. 7 wells) for 0~31.5%.
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基于不同土地利用方式的地下水硝态氮来源分析
研究区位于河北省滦河沿岸滦县段。滦河右侧设置3个监测断面,a、b、b段各设5口井,河漫滩上(堤内)设1口井,距河面约10m。堤外4口井之间的距离分别为20m、50m、200m、1500m。C-C段布置2口井,研究区共有13口观测井。3口井和11口井利用现有监测井,实际建井11口。监测井设计用于监测地下水位、地下水水质和同位素分析。在滦河4号井A-A段上游靠近树林边缘,8号井B-B段下游靠近农田(小麦)边缘,对各点土壤进行取样,测定土壤剖面中硝态氮含量和15N同位素比值。土壤取样深度从地表至地下,总深度约2.5m。每次距地表20cm处取1公斤左右的土壤样本,收集后用塑料袋密封,并编号。采样时间为2015年11月、2016年3月、2016年5月、2016年7月,共4次。分析表明,0-60cm土壤中硝酸盐含量较高,且与作物施肥深度(含畜禽粪便)相同,因此在估算地下水中硝酸盐含量比例时,假设0-60cm土壤中硝酸盐含量为初始值;其中接近土壤中的地下水位,作为60cm的终值,即硝酸盐进入地下水的终值,可以估算出土壤中硝酸盐进入地下水的比例。地下水中硝酸盐的来源复杂,与河流、土壤等因素有关。根据氮、氧同位素含量,确定了硝态氮的主要来源:土壤和滦河。结果表明,森林土壤中硝酸盐与地下水的比值为20%~80.8%,平均值为56.3%。麦田土壤中硝酸盐含量为6.8%~98.2%,平均值为48.3%。水体中硝态氮占比随季节变化较大,滦河上游(2号井附近)为0~19.6%;滦河(7号井附近)为0~31.5%。
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