[1]LIU Jun,YANG Kaiqi,LIU Ke,et al.Characteristics of Soil Water and Nutrients in Different Types Area of Pisha Sandstone in Inner Mongolia[J].Research of Soil and Water Conservation,2023,30(04):47-52.[doi:10.13869/j.cnki.rswc.2023.04.049.]
Copy

Characteristics of Soil Water and Nutrients in Different Types Area of Pisha Sandstone in Inner Mongolia

References:
[1] 李婷,吕一河,任艳姣,等.黄土高原植被恢复成效及影响因素[J].生态学报,2020,40(23):8593-8605.
[2] Fu B J, Wang S, Liu Y, et al. Hydrogeomorphic ecosystem responses to natural and anthropogenic changes in the Loess Plateau of China[J]. Annual Review of Earth and Planetary Sciences, 2017,45(1):223-243.
[3] 李依璇.黄土高原植被覆盖度变化特征及其影响因素[D].北京:北京林业大学,2021.
[4] 白小芳,徐福利,王渭玲.我国落叶松人工林地力衰退与施肥研究综述[J].世界林业研究,2016,29(1):75-79.
[5] 汪晓.立地条件对吴起沙棘人工林衰退及更新的影响[D].北京:北京林业大学,2020.
[6] Chen Y X, Wei T X, Ren K, et al. The coupling interaction of soil organic carbon stock and water storage after vegetation restoration on the Loess Plateau, China[J]. Journal of Environment Management, 2022,306:114481.
[7] Wang Y Q, Shao M A, Zhu Y J, et al. Impacts of land use and plant characteristics on dried soil layers in different climatic regions on the Loess Plateau of China[J]. Agricultural and Forest Meteorology, 2011,151(4):437-448.
[8] 史君怡,王国梁,刘国彬.退耕还林(草)对黄土高原不同土地利用方式下土壤剖面水分含量的影响[J].水土保持研究,2018,25(2):81-86.
[9] 葛楠楠,石芸,杨宪龙,等.黄土高原不同土壤质地农田土壤碳、氮、磷及团聚体分布特征[J].应用生态学报,2017,28(5):1626-1632.
[10] 王愿昌,吴永红,寇权,等.砒砂岩分布范围界定与类型区划分[J].中国水土保持科学,2007,5(1):14-18.
[11] 张平仓,刘玉民,张仲子.皇甫川流域侵蚀产沙特征及成因分析[J].水土保持通报,1992,(2):15-24.
[12] 唐政洪,蔡强国,李忠武,等.内蒙古砒砂岩地区风蚀、水蚀及重力侵蚀交互作用研究[J].水土保持学报,2001,15(2):25-29.
[13] Liang Z S, Wu Z R, Yao W Y, et al. Pisha Sandstone: causes, processes and erosion options for its control and prospects[J]. International Soil and Water Conservation Research, 2018,7:1-8.
[14] Li Y, Xie Z, Qin Y, et al. Temporal-spatial variation characteristics of soil erosion in the Pisha Sandstone Area, Loess Plateau, China[J]. Polish Journal of Environmental Studies, 2019,28(4):2205-2214.
[15] 鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000.
[16] 高宇,樊军,彭小平,等.水蚀风蚀交错区典型植被土壤水分消耗和补充深度对比研究[J].生态学报,2014,34(23):7038-7046.
[17] 熊小玲,任寅榜,吕茂奎,等.武夷山不同海拔典型森林土壤有机碳和全氮储量分布特征[J].水土保持研究,2022,29(4):83-88.
[18] Albaladejo J, Ortiz R, Garcia-Franco N, et al. Land-use and climate change impacts on soil organic carbon stocks in semi-arid Spain[J]. Journal of Soils and Sediments, 2012,13:265-277.
[19] 卜繁靖,郭月峰,祁伟,等.砒砂岩区3种沙棘根系特征与固土能力[J].水土保持通报,2022,42(5):41-48. DOI:10.13961/j. cnki. stbctb.20220525.001.
[20] 王浩,黄晨璐,杨方社,等.砒砂岩区沙棘根系的生境适应性[J].应用生态学报,2019,30(1):157-164.
[21] 刘丙霞,任健,邵明安,等.黄土高原北部人工灌草植被土壤干燥化过程研究[J].生态学报,2020,40(11):3795-3803.
[22] 马俊梅,满多清,李得禄,等.干旱荒漠区退耕地植被演替及土壤水分变化[J].中国沙漠,2018,38(4):800-807.
[23] 张鹤,费洪岩,韩凤朋,等.植被恢复和覆土厚度对砒砂岩区土壤水分及养分的影响[J].水土保持通报,2022,42(2):98-106.
[24] 杨敏,赵西宁,高晓东,等.黄土高原人工林深层土壤水分利用研究[J].水土保持研究,2019,26(6):100-106.
[25] 李佩擎.林下植被去除和凋落物添加对杉木林土壤关键生态过程的影响[D].南昌:江西农业大学,2017.
[26] 息伟峰,徐新朋,赵士诚,等.长期施肥下3种旱作土壤有机碳含量及其矿化势比较研究[J].植物营养与肥料学报,2021,27(12):2094-2104.
[27] Chai Q L, Ma Z Y, An Q Q, et al. Does artificial Caragana korshinskii plantation increase soil carbon continuously in a water-limited landscape on the Loess Plateau[J]. Land Degradation & Development, 2019,30:1691-1698.
[28] 张爱梅,殷一然,孙坤.沙棘属植物弗兰克氏菌研究进展[J].微生物学通报,2020,47(11):3933-3944.
[29] 武昭.基于室内土柱模拟的稳定性氮肥无机氮转化及淋溶探究[D].呼和浩特:内蒙古农业大学,2018.
Similar References:

Memo

-

Last Update: 2023-06-10

Online:1502       Total Traffic Statistics:27350296

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100