1. 兰州城市学院地理与环境工程学院,兰州,730070
2. 中国地质大学(武汉)公共管理学院,武汉,430070
3. 甘肃农业大学人文学院,兰州,730070
4. 甘肃省耕地质量建设管理总站,兰州,730000
[ "李昂(1969-),男,甘肃兰州人,博士,副教授,主要从事退化环境的恢复与治理研究。E-mail:liang@lzcu.edu.cn" ]
纸质出版:2020
移动端阅览
李昂, 李昌明, 尹卓忻, 等. 甘肃秦王川灌区种植豆禾混播牧草的农田生态保育效应[J]. 水土保持学报, 2020,34(2):239-244.
LI Ang, LI Changmin, YIN Zhuoxin, et al. Ecological Conservation Effect of Mixed Planting Legume and Grass in Qinwangchuan Irrigation Area of Gansu Province[J]. 2020, 34(2): 239-244.
李昂, 李昌明, 尹卓忻, 等. 甘肃秦王川灌区种植豆禾混播牧草的农田生态保育效应[J]. 水土保持学报, 2020,34(2):239-244. DOI: 10.13870/j.cnki.stbcxb.2020.02.034.
LI Ang, LI Changmin, YIN Zhuoxin, et al. Ecological Conservation Effect of Mixed Planting Legume and Grass in Qinwangchuan Irrigation Area of Gansu Province[J]. 2020, 34(2): 239-244. DOI: 10.13870/j.cnki.stbcxb.2020.02.034.
以裸地(CK)、种植小麦(Triticum aestivum)和苜蓿/无芒雀麦(Medicago sativa/Bromus inermis)豆禾混播牧草地为研究对象,通过测定地表植被特征指标、土壤风蚀量及理化性质等指标,探究秦王川灌区农田风蚀规律及种植春小麦和牧草对土壤及养分流失的影响。结果表明:农田表土损失呈秋末冬初流失较多,冬季较少,春季又明显增强的"U"形曲线模式,从9月至翌年6月,出现2个风蚀高峰期(9—11月和3—5月);耕地裸露造成表土年均流失1.7 kg/m2,即每年被风吹蚀1.3 mm厚表土,土壤有机质损失236.2 kg/hm2,而种植小麦和牧草后在地表植被(根茬)覆盖作用下表土流失减少20.1%和52.3%,有机质损失减少12.2%和50.7%;由于风蚀季牧草植被(根茬)的盖度、高度和地表生物量均较小麦大,使得牧草地的地表粗糙度和湿度及表土(0—5 cm)含水率较小麦地高,从而造成土壤和有机质流失较小麦地少;相关和回归分析显示,地表植被特征指标与地表粗糙度和土壤含水率间呈显著正相关,而与地表土壤和有机质流失量呈极显著负相关;植被盖度每提高1%,将使表土和有机质流失减少4.1 g/m2和59.3 mg/m2,地表生物量每提高1 g/m2,将使表土和有机质流失减少2.3 g/m2和34.0 mg/m2;春季春播小麦地的表土流失量与裸地相同,而种植多年生豆禾混播牧草可显著减少表土流失和有机质损失。综合以上,甘肃灌区农田春季播种农作物易引起土壤退化,而种植多年生豆禾混播牧草可实现农田生态保育,从而提高耕地质量和区域环境质量。
To explore wind erosion law of farmland and effects of planting spring wheat and pasture on soil and nutrient loss
the experiment took bare land (CK)
planting Triticum aestivum and Medicago sativa/Bromus inermis farmland as research objects. We measured indexes of vegetation characteristics
soil wind erosion
and physical and chemical properties. The results showed that soil loss showed a 'U' curve pattern
with more loss in late autumn and early winter
less loss in winter
and significantly increased loss in spring. There were two peak periods of wind erosion (September to November and March to May) from September to June of the following year. The average annual soil loss of bare land was up to 1.7 kg/m2
that was
as 1.3 mm thick topsoil was blown away by wind
resulting in the loss of land organic matter up to 236.2 kg/hm2. When wheat and pasture were planted
the soil mass loss reduced by 20.1% and 52.3%
and the organic matter loss reduced by 12.2% and 50.7% under the influence of surface vegetation (stubble). Due to the higher coverage
height
and surface biomass of pasture vegetation (stubble) than those of wheat in wind erosion season
the surface roughness
humidity
and water content of topsoil (0-5 cm) of grassland were higher than those of wheat field
resulting in less soil and organic matter loss than that of wheat field. Correlation analysis showed that there were a significant positive correlation between vegetation characteristics and surface roughness and soil moisture content
while there were a significant negative correlation between vegetation characteristics and surface soil and organic matter loss. Regression analysis showed that every 1% increase of vegetation coverage would reduce topsoil and organic matter loss by 4.1 g/m2and 59.3 mg/m2. Every 1 g/m2 increase of surface biomass would reduce topsoil and organic matter loss by 2.3 g/m2 and 34.0 mg/m2. The amount of topsoil loss of wheat fields sowed in spring was the same as that of bare land
while planting perennial legume-grass mixtures could significantly reduce the loss of topsoil and organic matter. On the whole
crops sowed in spring in irrigated areas of Gansu would likely cause soil degradation
while planting perennial legume-grass mixtures could fulfill the farmland ecological conservation
improve quality of cultivated land and regional environment.
杨彩红,王军强,柴强,等.民勤绿洲区撂荒农耕地抗风蚀效果[J].水土保持学报,2019,33(1):57-61.
中国农业部.我国出现沙尘暴的尘源主要来自农田[EB/OL].(2008-07-30).http:www.chinanews.com/gn/news/2008/07-30/1329140.shtml.
李昂,高天鹏,张鸣,等.西北风蚀区植被覆盖对土壤风蚀动态的影响[J].水土保持学报,2014,28(6):120-123.
Xie Y, Lin H H, Ye Y, et al. Changes in soil erosion in cropland in northeastern China over the past 300 years[J].Catena,2019,176:410-418.
Yan Y C, Wang X, Guo Z J, et al. Influence of wind erosion on dry aggregate size distribution and nutrients in three steppe soils in northern China[J].Catena,2018,170:159-168.
Yan Y C, Xin X P, Xu X L, et al. Quantitative effects of wind erosion on the soil texture and soil nutrients under different vegetation coveragein a semiarid steppe of northern China[J].Plant and Soil,2013,369:585-598.
Li F R, Zhao W Z, Liu J L, et al. Degraded vegetation and wind erosion influence soil carbon, nitrogen and phosphorus accumulation in sandy grasslands[J].Plant and Soil,2009,317:79-92.
移小勇,赵哈林,李玉霖,等.科尔沁沙地不同风沙土的风蚀特征[J].水土保持学报,2006,20(2):10-13.
王仁德,邹学勇,赵婧研,等.北京市平原区农田土壤蚀积特征分析[J].水土保持学报,2011,25(1):20-24.
苑依笑,王仁德,常春平,等.风蚀作用下农田土壤细颗粒的粒度损失特征及其对土壤性质的影响[J].水土保持学报,2018,32(2):104-109.
李昂,张鸣,蔺海明,等.种植甘草预防土壤风蚀效应[J].草业科学,2014,31(5):839-843.
孙铁军,肖春利,滕文军.不同草地建植模式对荒坡地土壤风蚀及理化性质的影响[J].水土保持学报,2011,25(3):44-48.
李昂,吴应珍,陈伟,等.甘草植被覆盖对西北风蚀区农田土壤养分及风蚀的影响[J].生态与农村环境学报,2016,32(2):295-301.
李昂,张鸣,陈映全,等.西北风蚀区种植甘草对农田土壤质地及碳,氮含量的影响[J].水土保持学报,2016,30(5):286-290.
肖红浪.甘肃秦王川大规模农垦中土壤风蚀与养分、盐分变化[J].土壤通报,1998,29(4):148-150.
李昂,吴应珍,叶鹤琳,等.种植小麦与牧草对西北风蚀区秦王川灌区粉砂壤土风蚀的影响[J].生态与农村环境学报,2018,34(6):535-540.
缑倩倩,韩致文,屈建军,等.秦王川灌区农田土壤盐分离子特征分析[J].土壤,2014,46(1):100-106.
李昂,张鸣,张建,等.西北干旱灌溉区种植春小麦和牧草对耕地盐渍化的影响[J].水土保持通报,2018,38(3):32-37.
Li A, Niu K C, Du G Z. Resource availability, species composition and sown density effects on productivity of experimental plant communities[J].Plant and Soil,2011,344(1):177-186.
海春兴,刘宝元,赵烨.土壤湿度和植被盖度对土壤风蚀的影响[J].应用生态学报,2002,13(8):1057-1058.
赵彩霞,郑大玮,何文清.植被覆盖度的时间变化与其防风蚀效应[J].植物生态学报,2005,29(1):68-73.
彭佳佳,胡玉福,肖海华,等.生态修复对川西北草地土壤有机质和氮素的影响[J].干旱区资源与环境,2015,29(5):149-153.
陈林,杨新国,宋乃平,等.荒漠草原区不同粒径土壤理化性质对苜蓿种植年限的响应[J].水土保持学报,2014,28(2):105-111.
0
浏览量
900
下载量
6
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621