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Position: Home > Articles > Nitrate Distribution and Accumulation in Deep Unsaturated Zone Soils in Piedmont of North China Plain Soils 2017 (6) 1179-1186

华北山前平原典型厚包气带硝态氮分布累积规律

作  者:
梁慧雅;王仕琴;魏守才
单  位:
中国科学院大学;中国科学院遗传与发育生物学研究所农业资源研究中心中国科学院农业水资源重点实验室河北省节水农业重点实验室
关键词:
厚包气带;硝态氮;分布;累积
摘  要:
包气带是连接大气层和含水层水分和养分转换的纽带,也是农田NO_3~–-N分布和累积的重要场所和向含水层淋失的通道,因此研究包气带土壤中NO_3~–-N的分布累积规律对防止地下水NO_3~–-N污染至关重要。本文以中国科学院栾城试验站典型的厚包气带为对象,在无施肥处理(N0)和施氮肥600 kg/(hm~2·a)(N600)两种处理的多年试验田中,利用Geoprobe获取0~10.5 m深度土壤样品,研究厚包气带NO_3~–-N垂向分布、累积规律,并分析其影响因素。结果表明:N0中NO_3~–-N基本保持不变,长年施氮肥600 kg/(hm~2·a)使得NO_3~–-N淋溶至10.5 m,并在深层包气带中形成累积,累积的峰值由土壤的质地和含水量决定;NO_3~–-N的分布和累积主要受水分运移、土壤质地和反硝化作用影响。
译  名:
Nitrate Distribution and Accumulation in Deep Unsaturated Zone Soils in Piedmont of North China Plain
作  者:
LIANG Huiya;WANG Shiqin;WEI Shoucai;Key Laboratory of Agricultural Water Resources, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences;University of Chinese Academy of Sciences;
关键词:
Deep unsaturated zone;;Nitrate;;Distribution;;Accumulation
摘  要:
The unsaturated zone is the link which water and nutrient transforms between atmosphere and aquifer, and it is crucial to study the distribution and accumulation of NO_3~–-N for preventing nitrate pollution in groundwater because it is the place where farmland nitrate distribute and accumulate and is the channel that nitrate leaches to the aquifer. In this study, the Geoprobe direct push system was employed to obtain 10.5 meters of continuous soil core samples from the typical deep unsaturated zones in croplands under two different fertilization(N0, no nitrogen fertilizer applied; and N600, 600 kg/(hm~2·a) nitrogen fertilizer applied in North China Plain in order to analyze the profile distribution, accumulation and key influential factors of NO_3~–-N in soils. The results showed that NO_3~–-N remained stable in N0, however, in a long-term application of 600 kg/(hm~2·a) nitrogen fertilizer(N600), NO_3~–-N leached to 10.5 m and accumulated in the deep unsaturated zone, the peak of accumulation was determined by soil texture and moisture content. The distribution and accumulation of NO_3~–-N were mainly affected by water migration, soil texture and denitrification.

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