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1. 西北农林科技大学 资源环境学院, 陕西 杨凌,712100
2. 中科院水利部 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌,712100
3. 中科院水利部 水土保持研究所, 陕西 杨凌,712100
4. 中科院水利部 水土保持生态工程技术研究中心, 陕西 杨凌,712100
Published:2022
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Zhang He, Fei Hongyan, Han Fengpeng, et al. Effects of Vegetation Restoration and Soil Thickness on Soil Moisture and Nutrient in Feldspathic Sandstone Area[J]. Bulletin of Soiland Water Conservation, 2022, 42(2): 98-106.
Zhang He, Fei Hongyan, Han Fengpeng, et al. Effects of Vegetation Restoration and Soil Thickness on Soil Moisture and Nutrient in Feldspathic Sandstone Area[J]. Bulletin of Soiland Water Conservation, 2022, 42(2): 98-106. DOI: 10.13961/j.cnki.stbctb.2022.02.014.
[目的] 研究植被恢复对砒砂岩区土壤水分和养分的影响状况,明确对于砒砂岩地区土壤保水保肥效果最佳的植被恢复类型,为砒砂岩区的生态修复和区域水土流失治理提供理论依据。[方法] 选取准格尔旗暖水乡裸露砒砂岩向覆土砒砂岩过渡区域,以黄土—砒砂岩交界带不同人工恢复植被和自然恢复草地的土壤为研究对象,测定土壤水分和养分含量,分析不同植被恢复和覆土厚度对砒砂岩区土壤水分和养分特征的影响(其中天然草地作为对照)。[结果] ①裸露砒砂岩向覆土砒砂岩过渡区域土壤水分含量主要受黄土厚度影响,黄土的持水性能优于砒砂岩土壤,养分含量主要受植被恢复类型影响; ②研究区土壤各指标均属于中等变异程度,其中土壤水分、碳、氮含量自北向南随覆土厚度增加逐渐增加,磷素分布则相反; ③对比天然草地,沙棘和油松恢复对砒砂岩区土壤碳、氮含量的提升效果最好,土壤有机质含量分别提高了43.12%和34.27%,全氮提高了78.95%和42.11%,铵态氮提高25.64%和46.15%,硝态氮提高69.44%和42.22%。其中油松恢复下土壤水分含量高于天然草地54.55%,但人工植被恢复后的土壤磷素水平并没有提升。[结论] 黄土较砒砂岩土壤持水能力更好,二者界面对水分下渗以及下层水分向上损失起到一定阻挡作用,因此砒砂岩区土壤水分改善方面可以考虑覆土层的蓄水保水能力。在进行人工植被恢复时
推荐种植沙棘和油松
可提升区域土壤水分、碳、氮含量
保水保肥能力较好。
[Objective] The effects of vegetation restoration on soil moisture and nutrients were studied
and the type of vegetation restoration that has the best effect on soil water and fertilizer conservation was clarified
in order to provide theoretical basis for the ecological restoration and regional soil erosion control of the feldspathic sandstone area. [Methods] The transition area between exposed feldspathic sandstone and soil-covered feldspathic sandstone in Nuanshui Township
Jungar Banner of Inner Mongolia was selected as the study area
and soils of different artificially restored vegetation and naturally restored grassland in loess-feldspathic sandstone boundary area were taken as the research object. The content of soil water and nutrients were measured
and the effects of different vegetation restoration and soil thickness on the characteristics of moisture and nutrient in the feldspathic sandstone area were analyzed with natural grassland as control. [Results] ① The soil moisture content in the transition zone from exposed feldspathic sandstone to soil-covered feldspathic sandstone was mainly affected by the thickness of loess. The water holding capacity of loess soil was better than that of feldspathic sandstone soil
and nutrient contents were mainly affected by vegetation restoration types. ② The soil indexes in the study area were of medium variation
in which the contents of soil moisture
carbon and nitrogen increased gradually with the increase of soil thickness from north to south
while the distribution of phosphorus was opposite. ③ Compared with natural grassland
the restoration of Hippophae rhamnoides and Pinus tabuliformis has the best effect on improving the content of soil carbon and nitrogen in feldspathic sandstone area. The content of soil organic matter increased by 43.12% and 34.27%
total nitrogen increased by 78.95% and 42.11%
ammonium nitrogen increased by 25.64% and 46.15%
and nitrate nitrogen increased by 69.44% and 42.22%
respectively. Among them
the content of soil moisture under the restoration of Pinus tabuliformis was higher than that of natural grassland by 54.55%
but the soil phosphorus level did not increase after artificial vegetation restoration. [Conclusion] Loess has better water-holding capacity than feldspathic sandstone soil
and the interface between the two has a certain barrier effect on the infiltration of water and the upward loss of water in the lower layer. Therefore
the water-storage and water-retention capacity of the overlying soil can be considered in the improvement of soil moisture in feldspathic sandstone area. During the restoration of artificial vegetation
it is recommended to plant Hippophae rhamnoides and Pinus tabuliformis
which can improve the soil moisture
carbon
and nitrogen content
as they have better water and fertilizer retention capacity.
伍艳,杨忠芳,刘慧,等.砒砂岩物质组成及其对养分含量的影响[J].人民黄河,2016,38(6):18-21,25.
史志华,刘前进,张含玉,等.近十年土壤侵蚀与水土保持研究进展与展望[J].土壤学报,2020,57(5):1117-1127.
陈同德,焦菊英,王颢霖,等.青藏高原土壤侵蚀研究进展[J].土壤学报,2020,57(3):547-564.
卢立娜,赵雨兴,胡莉芳,等.沙棘(
Hippophae rhamnoides
)种植对鄂尔多斯砒砂岩地区土壤容重、孔隙度与贮水能力的影响[J].中国沙漠,2015,35(5):1171-1176.
白杭改,明晓冉,刘立,等.暖水乡砒砂岩地球化学分类类型与物源区特征[J].人民黄河,2017,39(9):79-85,89.
李长明,宋丽莎,王立久.砒砂岩的矿物成分及其抗蚀性[J].中国水土保持科学,2015,13(2):11-16.
Yang Fangshe, Bi Cifen, Cao Mingming, et al. Simulation of sediment retention effects of the double seabuckthorn plant flexible dams in the Pisha Sandstone area of China [J]. Ecological Engineering, 2014,71(07):21-31.
李传福,刘阳,党晓宏,等.鄂尔多斯砒砂岩区生态恢复研究进展[J].内蒙古林业科技,2019,45(1):49-52.
郭雒敏,李晓丽,王文,等.坡度对紫红色砒砂岩击溅侵蚀的影响[J].中国水土保持科学,2019,17(1):1-9.
王丽丽,甄庆,王颖,等.晋陕蒙矿区排土场不同改良模式下土壤养分效应研究[J].土壤学报,2018,55(6):1525-1533.
Wang Ruijie, Yan Feng, Wang Yanjiao. Vegetation growth status and topographic effects in the Pisha sandstone area of China [J]. Remote Sensing, 2020,12(17):1-21.
杨振奇,郭建英,秦富仓,等.裸露砒砂岩区不同植被类型土壤团聚体稳定性与抗蚀性能[J].水土保持通报,2021,41(3):8-14.
邢启鑫,饶良懿,王志臻,等.内蒙古砒砂岩不同类型区土壤有机质与速效钾特征[J].水土保持学报,2019,33(6):257-264,272.
李洪杰,郭月峰,姚云峰,等.砒砂岩区沙棘液流及细根变化对土壤水分变化的响应[J].水土保持通报,2021,41(5):1-7.
杨振奇,秦富仓,李龙,等.砒砂岩区小流域土壤有机质的空间分布及其环境影响因素研究[J].土壤,2020,52(3):625-632.
郭曼,郑粉莉,和文祥,等.黄土丘陵区不同退耕年限植被多样性变化及其与土壤养分和酶活性的关系[J].土壤学报,2010,47(5):979-986.
王彦武,罗玲,张峰,等.河西绿洲荒漠过渡带梭梭林土壤保育效应[J].土壤学报,2019,56(3):749-762.
张凯,郑华,陈法霖,等.桉树取代马尾松对土壤养分和酶活性的影响[J].土壤学报,2015,52(3):646-653.
薛立,邝立刚,陈红跃,等.不同林分土壤养分、微生物与酶活性的研究[J].土壤学报,2003,40(2):280-285.
卢同平,张文翔,牛洁,等.典型自然带土壤氮磷化学计量空间分异特征及其驱动因素研究[J].土壤学报,2017,54(3):682-692.
罗红,吴建普,边巴多吉,等.西藏人工造林作业区土壤养分特征研究[J].土壤学报,2017,54(2):421-433.
张勇强,李智超,厚凌宇,等.林分密度对杉木人工林下物种多样性和土壤养分的影响[J].土壤学报,2020,57(1):239-250.
王昭艳,左长清,曹文洪,等.红壤丘陵区不同植被恢复模式土壤理化性质相关分析[J].土壤学报,2011,48(4):715-724.
张祎,李鹏,肖列,等.黄土高原丘陵区地形和土地利用对土壤有机碳的影响[J].土壤学报,2019,56(5):1140-1150.
Wang Kaibo, Deng Lei, Zhou Zhengchao, et al. Profile distributions and controls of soil inorganic carbon along a 150-year natural vegetation restoration chronosequence [J]. Soil Science Society of America Journal, 2016,80(1):193-202.
何群,席欢,万婷.不同植被恢复模式对红原沙化草地土壤理化性质的影响[J].四川环境,2017,36(1):35-40.
闫丽娟,王海燕,李广,等.黄土丘陵区4种典型植被对土壤养分及酶活性的影响[J].水土保持学报,2019,33(5):190-196,204.
谭学进,穆兴民,高鹏,等.黄土区植被恢复对土壤物理性质的影响[J].中国环境科学,2019,39(2):713-722.
刘文祥,李勇,于寒青.草灌植被恢复提高坡地土壤水稳性团聚体和碳、氮含量的有效性:退耕年限的影响[J].植物营养与肥料学报,2016,22(1):164-170.
翁伯琦,郑祥洲,丁洪,等.植被恢复对土壤碳氮循环的影响研究进展[J].应用生态学报,2013,24(12):3610-3616.
饶良懿,徐也钦,胡剑汝,等.砒砂岩覆土区小流域土壤可蚀性
K
值研究[J].应用基础与工程科学学报,2020,28(4):763-773.
朱雅娟,党宏忠,杜娟,等.覆土砒砂岩区沙棘耗水量及其影响因子[J].水土保持研究,2020,27(4):171-177,183.
Jian Shengqi, Zhao Chuanyan, Fang Shumin, et al. Evaluation of water use of
Caragana korshinskii
Kom. and
Hippophae rhamnoides
Linns. in the Chinese Loess Plateau [J]. Canadian Journal of Forestresearch, 2014,45(1):15-25.
何京丽,殷丽强,郭建英,等.砒砂岩地区沙棘生态工程的土壤修复效果分析[J].国际沙棘研究与开发,2013,11(3):19-23.
梁月,殷丽强.砒砂岩区沙棘人工林对土壤化学性质的影响分析[J].国际沙棘研究与开发,2014,12(2):15-17.
吴晓光,刘龙,张宏飞,等.砒砂岩区主要造林树种枯落物持水性能及土壤物理性质[J].水土保持学报,2020,34(4):137-144.
鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000.
Zhang Pan, Xiao Peiqing, Yao Wenyi, et al. Profile distribution of soil moisture response to precipitation on the Pisha sandstone hillslopes of China [J]. Scientific Reports, 2020,10(1):1-10.
Li Jing, Li Zhanbin, Guo Mengjing, et al. Effects of vegetation restoration on soil physical properties of abandoned farmland on the Loess Plateau, China [J]. Environmental Earth Sciences, 2018,77(5):1-9.
沈晗悦,信忠保,王志杰.北京山区侧柏林坡面土壤水分时空动态及其影响因素[J].生态学报,2021,41(7):2676-2686.
李晓丽,苏雅,齐晓华,等.高原丘陵区砒砂岩土壤特性的试验分析研究[J].内蒙古农业大学学报(自然科学版),2011,32(1):315-318.
马章怀.覆土砒砂岩区典型退化植被下土壤水分特征及调控[D].陕西 杨凌:西北农林科技大学,2020.
杨振奇.裸露砒砂岩区人工植被对水力侵蚀的调控机制研究[D].内蒙古 呼和浩特:内蒙古农业大学,2020.
Yang Lei, Chen Liding, Wei Wei, et al. Comparison of deep soil moisture in two re-vegetation watersheds in semi-arid regions [J]. Journal of Hydrology, 2014,513(1):314-321.
苏荣瑞,金卫斌,艾天成,等.基于GIS的湖北省江陵县土壤养分空间变异研究[J].长江大学学报(自科版):农学卷,2007,4(3):13-17.
刘晓林,李文峰,杨林楠,等.基于ArcGIS地统计分析模块的土壤养分空间变异分析:以云南省建水县为例[J].土壤通报,2012,43(6):1432-1437.
李龙,姚云峰,秦富仓,等.黄花甸子流域土壤全氮含量空间分布及其影响因素[J].应用生态学报,2015,26(5):1306-1312.
王国梁,刘国彬,许明祥.黄土丘陵区纸坊沟流域植被恢复的土壤养分效应[J].水土保持通报,2002,22(1):1-5.
袁媛,张鹤,武杼华,等.植被恢复对毛乌素沙地土壤pH和养分含量的影响[J].土壤通报,2021,52(1):148-156.
何高迅,王越,彭淑娴,等.滇中退化山地不同植被恢复下土壤碳氮磷储量与生态化学计量特征[J].生态学报,2020,40(13):4425-4435.
王利彦,周国娜,朱新玉,等.凋落物对土壤有机碳与微生物功能多样性的影响[J].生态学报,2021,41(7):2709-2718.
Zhang Yongwang, Shangguan Zhouping. The coupling interaction of soil water and organic carbon storage in the long vegetation restoration on the Loess Plateau [J]. Ecological Engineering, 2016,91(3):574-581.
陈彦,吕新.基于GIS和地统计学的土壤养分空间变异特征研究:以新疆农七师125团为例[J].中国农学通报,2005,21(7):389-391,405.
李丹维,王紫泉,田海霞,等.太白山不同海拔土壤碳、氮、磷含量及生态化学计量特征[J].土壤学报,2017,54(1):160-170.
姜沛沛,曹扬,陈云明,等.不同林龄油松(
Pinus tabulaeformis
)人工林植物、凋落物与土壤C, N, P化学计量特征[J].生态学报,2016,36(19):6188-6197.
Cheng Yuting, Li Peng, Xu Guoce, et al. Effects of soil erosion and land use on spatial distribution of soil total phosphorus in a small watershed on the Loess Plateau, China [J]. Soil & Tillage Research, 2018,184(7):142-152.
陈健,刘顺,史作民,等.川西亚高山3种森林恢复途径对土壤生物有效磷的影响[J].生态学报,2021,41(7):2698-2708.
岑龙沛,严友进,戴全厚,等.喀斯特不同土地利用类型裂隙土壤有机碳及磷素赋存特征[J].生态学报,2020,40(21):7567-7575.
程立平,赵玉明,刘沛松.豫西低山丘陵区不同植被修复模式下土壤养分评价[J].江苏农业科学,2015,43(10):423-426.
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