[1]刘东,张健,付强.三江平原井灌区地下水人工回灌量测算[J].水土保持研究,2012,19(02):240-243.
　LIU Dong,ZHANG Jian,FU Qiang.Estimation of Groundwater Artificial Recharge Quantity in Area of Well Irrigation in Sanjiang Plain[J].Research of Soil and Water Conservation,2012,19(02):240-243.
点击复制

三江平原井灌区地下水人工回灌量测算

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 19 期数: 2012年02期 页码: 240-243 栏目: 出版日期: 2012-04-20
Title:
Estimation of Groundwater Artificial Recharge Quantity in Area of Well Irrigation in Sanjiang Plain
作者:
刘东1, 张健2, 付强1
1. 东北农业大学, 水利与建筑学院, 哈尔滨 150030;
2. 黑龙江农垦总局红兴隆分局水务局, 黑龙江 双鸭山 155100
Author(s):
LIU Dong1, ZHANG Jian2, FU Qiang1
1. School of Water Conservancy & Civil Engineering, Northeast Agricultural University, Harbin 150030, China;
2. Water Affairs Bureau of Hongxinglong Branch Bureau of Land Reclamation General Bureau in Heilongjiang Province, Shuangyashan, Heilongjiang 155100, China
关键词:
三江平原; 井灌区; 地下水; 水量均衡法; 人工回灌量
Keywords:
Sanjiang Plain; well irrigation area; groundwater; water balance method; artificial recharge quantities
分类号:
S273.4
摘要:
针对近些年来三江平原大面积发展井灌水稻所导致的地下水位持续下降问题，以853农场为例，采用水量均衡法，测算了853农场2006—2009年维持地下水收支平衡及地下水恢复至适宜埋深条件下的人工回灌量，结果表明：维持地下水收支平衡所需回灌量均小于5000万m3；地下水恢复至适宜埋深所需回灌量均为2亿m3左右，远远超过维持地下水收支平衡所需回灌量；若继续沿用现状地下水利用模式，未来所需回灌量会更大，建议当地加大地下水资源管理力度。研究成果为853农场乃至整个三江平原地下水资源恢复及可持续利用提供了科学依据。
Abstract:
In recent years,the rapid increase of well irrigation paddy field area has led to continually descending of groundwater level in Sanjiang Plain.Aimed at the problem mentioned above,the artificial recharge quantities from 2006 to 2009 under the condition of maintaining the groundwater balance and recovering the groundwater to suitable burial depth were estimated in Farm 853 through using the water balance method.The results show that the artificial recharge quantities of maintaining the groundwater balance are all less than 5×107m3,and the artificial recharge quantities of recovering the groundwater to suitable burial depth are all about 2×108m3,which are far greater than the artificial recharge quantities of maintaining the groundwater’s balance.If the utilization pattern of groundwater resources is maintained,the artificial recharge quantities will be greater in the future,so local government should reinforce the management strength towards groundwater resources.The research achievements can provide scientific gist for groundwater resources recovery and its sustainable utilization in Farm 853 and even the entire Sanjiang Plain.

参考文献/References:

[1] 刘正茂,夏广亮,吕宪国,等.近50年来三江平原水循环过程对人类活动和气候变化的响应[J].南水北调与水利科技,2011,9(1):68-74.
[2] 陶洁,张兴波.发展水稻生产是三江平原抗旱除涝的一项有效措施[J].黑龙江水利科技,2010,38(3):214-215.
[3] 赵清,丁红,刘东.支持向量机在三江平原井灌水稻需水量预测中的应用[J].水资源与水工程学报,2010,21(2):72-74.
[4] 黄妮,刘殿伟,王宗明.1986—2005年三江平原水田与旱地的转化特征[J].资源科学,2009,31(2):324-329.
[5] 沃晓岚,孙香泰,彭振.三江平原地区地下水资源开发利用状况及可持续利用对策[J].黑龙江水利科技,2009,37(4):45-46.
[6] 王韶华,田园.三江平原地下水埋深变化及成因的初步分析[J].灌溉排水学报,2003,22(2):61-64.
[7] 刘正茂,夏广亮,赵艳波.三江平原地下水开采对生态过程的影响[J].水利发展研究,2006(12):38-41.
[8] 谢乐云,杨文涛.浅谈地下水人工补给问题[J].西部探矿工程,2003(9):174-175.
[9] 丁昆仑.人工回灌地下水的有效途径和方法探讨[J].中国农村水利水电(农田水利与小水电),1996(1/2):14-17.
[10] 张元禧,施鑫源.地下水水文学[M].北京:中国水利水电出版社,1998.
[11] 张顺联.地下水水文学[M].北京:水利电力出版社,1986.
[12] 张顺联.地下水资源计算与评价[M].北京:水利电力出版社,1992.
[13] 张臣,林湘杰,谭玉龙.浅析八五三农场水土流失成因及治理措施[J].科技创新导报,2010(20):136.
[14] 吕文龙.浅议八五三农场水资源量及水资源开发利用现状[J].水利科技与经济,2008,14(12):1007-1008.
[15] 王立权,王忠玉,姚章村.井水增温对水稻产量的影响研究[J].黑龙江水专学报,2005,32(4):56-58.
[16] 袁斌,杜绍敏,杨伟清,等.三江平原浅层地下水超采问题探讨(二)[J].黑龙江水专学报,2008,35(1):18-21.
[17] 李怀正,白月华,邢绍文,等.雨水回灌地下的必要性和可行性[J].中国给水排水,2002,18(4):29-30.

相似文献/References:

[1]殷嘉迪,雷国平,乐容潮,等.三江平原农村居民点时空格局演变——以富锦市为例[J].水土保持研究,2017,24(06):300.
　YIN Jiadi,LEI Guoping,LE Rongchao,et al.Spatiotemporal Evolution of Rural Settlements in Sanjiang Plain—A Case Study in Fujin City[J].Research of Soil and Water Conservation,2017,24(02):300.
[2]刘东,付强.基于小波变换的三江平原井灌区主汛期降水序列多时间尺度分析[J].水土保持研究,2008,15(06):42.
　LIU Dong,FU Qiang.Multi-Time Scales Analysis of Main Flood Season Precipitation Series Based on Wavelet Transform in Area of Well-Irrigation in Sanjiang Plain[J].Research of Soil and Water Conservation,2008,15(02):42.
[3]陈红光,李晨洋,李晓丹.基于风险分析的三江平原灌区多水源联合调度方案优化决策研究[J].水土保持研究,2013,20(04):273.
　CHEN Hong-guang,LI Chen-yang,LI Xiao-dan.Study on the Water Joint Operation Scheme Optimization in Sanjiang Plain Irrigation Area Based on Risk Analysis[J].Research of Soil and Water Conservation,2013,20(02):273.
[4]韩丽伟,付强,刘东,等.三江平原地下水承载能力综合评价模型的构建及其应用[J].水土保持研究,2010,17(02):182.
　HAN Li-wei,FU Qiang,LIU Dong,et al.Construction and Application of the Model on Groundwater Resources Carrying Capacity in Sanjiang Plain[J].Research of Soil and Water Conservation,2010,17(02):182.
[5]孙海清.降水量与地下水埋深的小波分析——以广饶县井灌区为例[J].水土保持研究,2007,14(02):55.
　SUN Hai-qing.Wavelet Analysis on Annual Precipitation and Groundwater Depth Changes——A Case Study on Well-irrigated Area, Guangrao[J].Research of Soil and Water Conservation,2007,14(02):55.
[6]马吉巍,郭翔宇,付强,等.区域农业水土资源复杂适应系统配置研究——以三江平原为例[J].水土保持研究,2014,21(03):256.
　MA Ji-wei,GUO Xiang-yu,FU Qiang,et al.Study on Complex Adaptive Allocation of Regional Agricultural Water and Soil Resources—Taking Sanjiang Plain for Example[J].Research of Soil and Water Conservation,2014,21(02):256.
[7]申月静,雷国平,曲晓涵,等.基于加权Voronoi图扩展断裂点的农村居民点布局优化[J].水土保持研究,2017,24(04):284.
　SHEN Yuejing,LEI Guoping,QU Xiaohan,et al.Layout Optimization of Rural Settlements Based on the Extended Break-Point Model of Weighted Voronoi diagram[J].Research of Soil and Water Conservation,2017,24(02):284.
[8]杜嘉,张柏,宋开山,等.基于NOAA/AVHRR数据估算三江平原蒸散量研究初探[J].水土保持研究,2009,16(02):56.
　DU Jia,ZHANG Bai,SONG Kai-shan,et al.Estimated Evapotranspiration Based on NOAA/AVHRR Data in the Sanjiang Plain[J].Research of Soil and Water Conservation,2009,16(02):56.
[9]王振芬.三江平原湿地不同土地利用方式对土壤养分及酶活性的影响[J].水土保持研究,2019,26(02):43.
　WANG Zhenfen.Characteristics of Soil Nutrients and Enzyme Activity Under Different Types of Land Use in Wetland of Sanjiang Plain[J].Research of Soil and Water Conservation,2019,26(02):43.
[10]鲁菁,张玉虎,高峰,等.近40年三江平原极端降水时空变化特征分析[J].水土保持研究,2019,26(02):272.
　LU Jing,ZHANG Yuhu,GAO Feng,et al.Temporal and Spatial Variation Characteristics of Extreme Precipitation in the Sanjiang Plain in Recent 40 Years[J].Research of Soil and Water Conservation,2019,26(02):272.
[11]刘东,张健,付强.基于连续小波变换与分形理论的三江平原井灌区地下水埋深序列复杂性研究[J].水土保持研究,2011,18(02):116.
　LIU Dong,ZHANG Jian,FU Qiang.Study on Complexity of Groundwater Depth Series in Well Irrigation Area of Sanjiang Plain Based on Continuous Wavelet Transform and Fractal Theory[J].Research of Soil and Water Conservation,2011,18(02):116.

备注/Memo

收稿日期:2011-7-18;改回日期:2011-9-30。
基金项目:国家自然科学基金(41071053);中国博士后科学基金特别资助(201003410);高等学校博士学科点专项科研基金(20102325120009);黑龙江省自然科学基金(C201026);黑龙江省教育厅科学技术研究项目(11541024);东北农业大学博士启动基金(2009RC37)
作者简介:刘东（1972- ）,男,黑龙江安达人,教授,博士,博士生导师,主要研究方向为农业水土资源系统分析与优化利用。E-mail:l

更新日期/Last Update: 1900-01-01