首页> 外文期刊>Indian Journal of Fertilisers >Nitrate Contamination of Groundwaters in Haryana Is Nitrogen Fertilisation Responsible?
【24h】

Nitrate Contamination of Groundwaters in Haryana Is Nitrogen Fertilisation Responsible?

机译:哈里亚纳邦地下水的硝酸盐污染是否对氮肥负责?

获取原文
获取原文并翻译 | 示例
       

摘要

Investigations of randomly collected tube well water samples from Khera Jhanjrola, Mehendwara and Dhankot villages of Gurgaon district revealed that majority of the wells in Khera Jhanjrola (54 %) had NO3 concentration beyond 50 mgL~(-1). Pumping test at different discharge rates suggested that the aquifer was semi-confined and not much variation in nitrate content of pumped water with pumping rate and duration. There was high total N (0.14%) with not much variation in different layers in profile up to 15m and more than 95% of the total N was in organic forms being a result of saturation of the soil's column by nitrate consequent upon irrigations with nitrate rich waters. Available N was < 250 kg ha~(-1) throughout the soil profile of 15m. Organic C at different depths was close to the average value for the whole profile. Results of spatial and temporal variation (pre- and post-monsoon) showed not much variation in the nitrate (slightly higher in pre-monsoon than in the post-monsoon) whereas EC differed considerably. A positive correlation indicated a general increase in NO3 as EC increased. Calibrated and validated model (LEACHN model) predicted leaching to the tune of 3.1 in pearl millet and 9.6 kg ha~(-1) in wheat meaning losses as nitrate to the tune of 13 kg ha~(-1) yr~(-1). Simulated nitrate leaching under normally practised irrigation depth was 9.0 and 32.8 kg/ha for pearl millet and wheat, respectively with nitrate rich waters. With more efficient irrigation (depth of 40 mm), simulated nitrate losses decreased to 6.0 and 13.7 kg/ha for pearl millet and wheat, respectively. In -situ measurement of nitrate movement in the profile, measured values of nitrate leaching at 30, 60 and 90 cm soil depth was 27.86, 28.95 and 23.19 kg/ha, respectively. The model predicted nitrate leaching at the rate of 33.3 kg/ha at 120 cm and predicted and actual measured values exhibited a reasonably good agreement. Results indicated that leaching from fertilisers might not be a major contributing factor to high NO- concentration in groundwater at theselected sites.
机译:对古尔冈地区Khera Jhanjrola,Mehendwara和Dhankot村随机收集的管井水样品进行的调查显示,Khera Jhanjrola中的大多数井(54%)中的NO3浓度均超过50 mgL〜(-1)。在不同流量下的抽水试验表明,含水层是半封闭的,并且随抽水速度和持续时间的变化,抽水的硝酸盐含量变化不大。总氮较高(0.14%),直到15m为止,不同剖面的剖面变化不大,并且总氮的95%以上是有机形式,这是由于用硝酸盐灌溉土壤后土壤被硝酸盐饱和丰富的水域。在15m的整个土壤剖面中,有效氮均<250 kg ha〜(-1)。不同深度的有机碳接近于整个剖面的平均值。空间和时间变化的结果(季风前后)在硝酸盐中变化不大(季风前略高于季风后),而EC差异很大。正相关表明随着EC的增加,NO3总体增加。校准和验证的模型(LEACHN模型)预测珍珠小米的淋失为3.1,小麦的淋溶为9.6 kg ha〜(-1),这意味着硝酸盐损失为13 kg ha〜(-1)yr〜(-1)。 )。在富含硝酸盐的水域下,通常的灌溉深度下,珍珠粟和小麦的模拟硝酸盐浸出分别为9.0和32.8 kg / ha。随着灌溉效率的提高(深度为40毫米),珍珠粟和小麦的模拟硝酸盐损失分别降至6.0和13.7公斤/公顷。对剖面中硝酸盐运动的原位测量,在30、60和90 cm土深处的硝酸盐淋失测量值分别为27.86、28.95和23.19 kg / ha。该模型预测硝酸盐在120 cm处的浸出速率为33.3 kg / ha,预测值与实际测量值显示出相当好的一致性。结果表明,从肥料中浸出可能不是造成选​​定地点地下水中高NO含量的主要因素。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号