[1]盖浩琪,石培君,李 志.黄土区长武塬土地利用变化对土壤水平衡的影响[J].水土保持研究,2023,30(04):154-159.[doi:10.13869/j.cnki.rswc.2023.04.032.]
 GAI Haoqi,SHI Peijun,LI Zhi.Impact of Land Use Change on Soil Water Balance in Changwu Tableland of Loess Region[J].Research of Soil and Water Conservation,2023,30(04):154-159.[doi:10.13869/j.cnki.rswc.2023.04.032.]
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黄土区长武塬土地利用变化对土壤水平衡的影响

参考文献/References:

[1] 裴艳武,黄来明,邵明安,等.毛乌素沙地不同地下水位埋深下土壤水补给特征及影响因素[J].农业工程学报,2021,37(12):108-116.
[2] Li B B, Biswas A, Wang Y Q, et al. Identifying the dominant effects of climate and land use change on soil water balance in deep loessial vadose zone[J]. Agricultural Water Management, 2021, 245:106637.
[3] 张瑞,李鹏展,王力.黄土旱塬区土壤水分状况与作物生长、降水的关系[J].应用生态学报,2019,30(2):359-369.
[4] 穆兴民,徐学选,王文龙,等.黄土高原人工林对区域深层土壤水环境的影响[J].土壤学报,2003,40(2):210-217.
[5] 刘锦月,韩晓阳,朱元骏.长武塬区苹果园和农田相互转换的深层土壤水环境效应[J].干旱地区农业研究,2020,38(5):130-135.
[6] 白晓,贾小旭,邵明安,等.黄土高原北部土地利用变化对长期土壤水分平衡影响模拟[J].水科学进展,2021,32(1):109-119.
[7] 程立平,刘文兆,李志.黄土塬区不同土地利用方式下深层土壤水分变化特征[J].生态学报,2014,34(8):1975-1983.
[8] Shi P J, Huang Y N, Ji W J, et al. Impacts of deep-rooted fruit trees on recharge of deep soil water using stable and radioactive isotopes[J]. Agricultural and Forest Meteorology, 2021, 300:108325.
[9] Li B B, Wang Y Q, Hill R L, et al. Effects of apple orchards converted from farmlands on soil water balance in the deep loess deposits based on HYDRUS-1D model[J]. Agriculture, Ecosystems & Environment, 2019, 285:106645.
[10] 刘增进,柴红敏,李宝萍.豫西黄土丘陵区林草植被蒸散量估算研究[J].灌溉排水学报,2012,31(3):99-102,138.
[11] 张建军,李慧敏,徐佳佳.黄土高原水土保持林对土壤水分的影响[J].生态学报,2011,31(23):71-81.
[12] 陶泽,司炳成,靳静静.矮化枣树冠层改变降雨截留历时过程同位素和化学特征[J].水土保持学报,2017,31(5):189-195.
[13] 穆艳,王延平.黄土长武塬区苹果林地水量平衡研究[J].农业现代化研究,2017,38(1):161-167.
[14] Li H, Si B C, Li M. Rooting depth controls potential groundwater recharge on hillslopes[J]. Journal of Hydrology, 2018, 564:164-174.
[15] 李杰彪,苏锐,田霄,等.干旱-半干旱地区地下水补给方法研究综述[J].世界核地质科学,2013,30(3):168-173.
[16] Shi P J, Huang Y N, Yang C Y, et al. Quantitative estimation of groundwater recharge in the thick loess deposits using multiple environmental tracers and methods[J]. Journal of Hydrology, 2021, 603:126895.
[17] Xiang W, Evaristo J, Li Z. Recharge mechanisms of deep soil water revealed by water isotopes in deep loess deposits[J]. Geoderma, 2020, 369:114321.
[18] Li Z, Jasechko S, Si B C. Uncertainties in tritium mass balance models for groundwater recharge estimation[J]. Journal of Hydrology, 2019,571:150-158.
[19] Li Z, Chen X, Liu W Z, et al. Determination of groundwater recharge mechanism in the deep loessial unsaturated zone by environmental tracers[J]. Science of the Total Environment, 2017,586:827-835.
[20] Zhang Z Q, Evaristo J, Li Z, et al. Tritium analysis shows apple trees may be transpiring water several decades old[J]. Hydrological Processes, 2017,31(5):1196-1201.
[21] Huang T M, Pang Z H. Estimating groundwater recharge following land-use change using chloride mass balance of soil profiles: a case study at Guyuan and Xifeng in the Loess Plateau of China[J]. Hydrogeology Journal, 2011,19(1):177-186.
[22] Huang Y N, Li B B, Li Z. Conversion of degraded farmlands to orchards decreases groundwater recharge rates and nitrate gains in the thick loess deposits[J]. Agriculture, Ecosystems & Environment, 2021, 314: 107410.
[23] Ji W J, Huang Y N, Shi P J, et al. Recharge mechanism of deep soil water and the response to land use change in the loess deposits[J]. Journal of hydrology, 2021, 592:125817.
[24] Li H J, Si B C, Wu P T, et al. Water mining from the deep critical zone by apple trees growing on loess[J]. Hydrological Processes, 2019,33(2):320-327.
[25] Lu Y W, Si B C, Li H J, et al. Elucidating controls of the variability of deep soil bulk density[J]. Geoderma, 2019,348:146-157.
[26] Zhang Z Q, Li M, Si B C, et al. Deep rooted apple trees decrease groundwater recharge in the highland region of the Loess Plateau, China[J]. Science of the Total Environment, 2018, 622:584-593.
[27] De Medeiros G A, Arruda F B, Sakai E, et al. The influence of crop canopy on evapotranspiration and crop coefficient of beans(Phaseolus vulgaris L.)[J]. Agricultural Water Management, 2001,49(3):211-224.
[28] 胡良军,邵明安.黄土高原植被恢复的水分生态环境研究[J].应用生态学报,2002,13(8):1045-1048.
[29] Huang Y N, Chang Q R, Li Z. Land use change impacts on the amount and quality of recharge water in the loess tablelands of China[J]. Science of the Total Environment, 2018,628:443-452.
[30] 李晨曦.基于环境同位素的洛川塬区地下水补给机制研究[D].陕西杨凌:西北农林科技大学,2017.
[31] 程立平,刘文兆,李志,等.长武黄土塬区土地利用变化对潜水补给的影响[J].水科学进展,2016,27(5):670-678.

备注/Memo

收稿日期:2022-04-21 修回日期:2022-05-30
资助项目:国家自然科学基金“黄土区潜水补给的方式、速率与控制因素”(42071043)
第一作者:盖浩琪(1998—),女,山西长治人,硕士研究生,研究方向为旱区植被变化生态水文效应。E-mail:2020050718@nwafu.edu.cn
通信作者:李志(1978—),男,山东沂水人,博士,教授,主要从事旱区水循环与水环境演变机理与调控研究。E-mail:lizhibox@nwafu.edu.cn

更新日期/Last Update: 2023-06-10