1. 西南林业大学生态与环境学院,昆明,650224
2. 云南省昆明市晋宁区水务局,昆明,650607
[ "杨翠萍(1995-),女,硕士研究生,主要从事土壤侵蚀与控制研究。E-mail:17853482159@163.com" ]
纸质出版:2019
移动端阅览
杨翠萍, 脱云飞, 张岛, 等. 降雨对不同土地利用类型土壤水氮变化特征的影响[J]. 水土保持学报, 2019,33(6):220-226.
YANG Cuiping, TUO Yunfei, ZHANG Dao, et al. Effects of Rainfall on Soil Water and Nitrogen Change Characteristics Under Different Land Uses[J]. 2019, 33(6): 220-226.
杨翠萍, 脱云飞, 张岛, 等. 降雨对不同土地利用类型土壤水氮变化特征的影响[J]. 水土保持学报, 2019,33(6):220-226. DOI: 10.13870/j.cnki.stbcxb.2019.06.031.
YANG Cuiping, TUO Yunfei, ZHANG Dao, et al. Effects of Rainfall on Soil Water and Nitrogen Change Characteristics Under Different Land Uses[J]. 2019, 33(6): 220-226. DOI: 10.13870/j.cnki.stbcxb.2019.06.031.
以2018年6-10月降雨条件下园地、林地、荒草地、坡耕地和裸地的标准径流小区为研究对象,裸地为对照,通过研究降雨对园地、林地、荒草地、坡耕地和裸地的土壤含水率、总氮、硝态氮和铵态氮含量与土层深度和时间的变化特征,经野外试验数据统计分析,提出降雨对园地、林地、荒草地、坡耕地和裸地土壤含水率、总氮、硝态氮和铵态氮含量与土层深度和时间变化特征的影响。结果表明:降雨增加园地、林地、荒草地、坡耕地和裸地土壤含水率,加速土壤总氮、硝态氮和铵态氮水解转化硝化和反硝化速度,影响土壤含水率、总氮、硝态氮和铵态氮含量,降雨与土壤含水率、总氮、硝态氮、铵态氮呈显著相关性(P<0.05)。降雨条件下园地、林地、荒草地、坡耕地和裸地的土壤含水率随土层深度增大而增大,土层深度100 cm处土壤含水率最大,分别为30.34%,27.67%,24.98%,24.03%和21.95%,总氮随土层深度增大呈先增大后减小,在土层深度为60 cm土壤总氮含量最大,分别为1.02,0.99,0.90,0.86,0.75 g/kg,硝态氮和铵态氮含量随土层深度增大而减小,在土层深度为100 cm硝态氮和铵态氮含量均最小,其中硝态氮含量分别为9.01,7.89,7.25,6.10,5.22 mg/kg,铵态氮含量分别为9.41,9.14,6.40,5.38,4.37 mg/kg。土壤含水率随时间的延长先减小后增大又减小,呈正余弦变化趋势,8月土壤含水率最大,分别为22.97%,22.01%,19.87%,19.03%和17.98%,总氮随时间的延长先增大后减小,8月总氮最大,分别为1.09,1.01,0.94,0.84,0.76 g/kg,硝态氮和铵态氮含量随时间的延长而逐渐减少,6月硝态氮和铵态氮含量均最大,其中硝态氮含量分别为13.40,12.37,11.20,10.39,8.67 mg/kg,铵态氮含量分别为18.89,17.02,14.54,12.02,8.36 mg/kg。不同土地利用类型土壤含水率、总氮、硝态氮和铵态氮平均值与土层深度和时间关系由大到小依次为园地、林地、荒草地、坡耕地和裸地,研究结果为农田土壤水肥流失控制和养分利用提供理论技术支持。
Under the rainfall from June to October
2018
the standard runoff plots in garden land
forest land
grassland
farmland and bare land were taken as research object
with the bare land as the control. The soil moisture contents
total nitrogen
nitrate nitrogen and ammonium nitrogen contents in different soil depth and time were studied in garden land
forest land
grass land
farmland and bare land. Through statistical analysis of field test data
the effects of rainfall on soil water and nitrogen change characteristics under different land uses were proposed. The results showed that the rainfall increased soil moisture content in garden land
forest land
grassland
farmland and bare land and accelerated soil total nitrogen
nitrate nitrogen and ammonium nitrogen hydrolysis conversion of nitrification and denitrification rate
affected the soil moisture contents
total nitrogen
nitrate nitrogen and ammonium nitrogen contents. The rainfall had significant correlations (P<0.05) with soil moisture contents
total nitrogen
nitrate nitrogen
ammonium nitrogen. Under rainfall
soil moisture content increased with the soil depth in garden land
forest land
grassland
farmland and bare land. At soil depth of 100 cm
soil moisture content was the largest
which were 30.34%
27.67%
24.98%
24.03% and 21.95%
respectively. Total nitrogen contents increased first and decreased then with the increasing soil depth
and at the soil depth of 60 cm
soil total nitrogen was the largest
which were 1.02
0.99
0.90
0.86 and 0.75 g/kg
respectively. Nitrate nitrogen and ammonium nitrogen contents decreased with the increasing soil depth. The nitrate nitrogen and ammonium nitrogen contents at soil depth of 100 cm were the smallest
among which the nitrate nitrogen was 9.01
7.89
7.25
6.10
5.22 mg/kg
and the ammonium nitrogen was 9.41
9.14
6.40
5.38
4.37 mg/kg
respectively. With the time
soil moisture contents decreased first
then increased
and then decreased at last
showing a positively cosine changing trend. Soil moisture contents was the largest in August
which were 22.97%
22.01%
19.87%
19.03% and 17.98% respectively. Total nitrogen first increased and then decreased with time
with the largest in August
which were 1.09
1.01
0.94
0.84 and 0.76 g/kg
respectively. Nitrate nitrogen and ammonium nitrogen contents reduced gradually with time. Soil nitrate nitrogen and ammonium nitrogen contents were larger in June. Soil nitrate contents were 13.40
12.37
11.20
10.39
8.67 mg/kg
ammonium nitrogen 18.89
17.02
14.54
12.02
8.36 mg/kg
respectively. The relationships between average soil moisture contents
total nitrogen
nitrate nitrogen and ammonium nitrogen contents and soil depth and time in different land uses were following as:garden > woodland > grassland > sloping land > bare land. This study could provide theoretical and technical support for soil water and fertilizer loss control and nutrient utilization in farmland.
徐国策,李占斌,李鹏,等.丹江中游典型小流域土壤总氮的空间分布[J].地理学报,2012,67(11):1547-1555.
杨林章,徐琪.土壤生态系统[M].北京:科学出版社,2005.
刘沛松,王健胜,楚纯洁,等.豫西低山丘陵区不同土地利用方式对陡坡地土壤理化性状的影响[J].干旱地区农业研究,2014,32(1):208-212.
范夫静,宋同清,黄国勤,等.西南峡谷型喀斯特坡地土壤养分的空间变异特征[J].应用生态学报,2014,25(1):92-98.
徐志超,宋彦涛,乌云娜,等.放牧影响下克氏针茅草原不同物候期土壤酶活性与微生物生物量的变化[J].生态学杂志,2016,35(8):2022-2028.
白军红,丁秋档,高海峰,等.向海湿地不同植被群落下土壤氮素的分布特征[J].地理科学,2009,29(3):381-384.
宋成军,张玉华,刘东生,等.土地利用/覆被变化(LUCC)与土壤重金属积累的关系研究进展[J].生态毒理学报,2009,4(5):617-624.
朱燕琴,赵志斌,齐广平.黄土丘陵区植被类型和降雨对坡面侵蚀产沙的影响[J].水土保持学报,2019,33(2):9-16.
林锦阔,李子君,许海超,等.降雨因子对沂蒙山区不同土地利用方式径流小区产流产沙的影响[J].水土保持通报,2016,36(5):7-12.
艾宁,魏天兴,朱清科.陕北黄土高原不同植被类型下降雨对坡面径流侵蚀产沙的影响[J].水土保持学报,2013,27(2):26-30.
Foroughifar H, Jafarzadeh A A, Torabi H, et al. Using geostatistics and geographic information system techniques to characterize spatial variability of soil properties, includingmicronutrients[J].Communications in Soil Science and Plant Analysis,2013,44(8):1273-1281.
Joseph G, Henry H. Soil nitrogen leaching losses in response to freeze-thaw cycles and pulsed warming in a temperate old field[J].Soil Biology and Biochemistry,2008,40(7):1947-1953.
Varma V, Iyengar S B, Sankaran M. Effects of nutrient addition and soil drainage on germination of N-fixing and non-N-fixing tropical dry forest tree species[J].Plant Ecology,2016,217(8):1043-1054.
Usowicz B, Lipiec J.Spatial variability of soil properties and cereal yield in a cultivated field on sandy soil[J].Soil and Tillage Research,2017,174:241-250.
Leip A, Britz W, Weiss F, et al. Farm, land, and soil nitrogen budgets for agriculture in Europe calculated with CAPRI[J].Environmental Pollution,2011,159(11):3243-3253.
赵勇,王鹏飞,樊巍,等.太行山丘陵区不同龄级栓皮栎人工林养分循环特征[J].中国水土保持科学,2009,7(4):66-71.
赵明松,张甘霖,李德成,等.苏中平原南部土壤有机质空间变异特征研究[J].地理科学,2013,33(1):83-89.
高雪松,邓良基,张世熔.不同利用方式与坡位土壤物理性质及养分特征分析[J].水土保持学报,2005,19(2):53-56.
王艳萍,王力,韩雪,等.黄土塬区不同土地利用方式土壤水分消耗与补给变化特征[J].生态学报,2015,35(22):7571-7579.
柴锦隆,徐长林,张德罡,等.模拟践踏和降水对高寒草甸土壤养分和酶活性的影响[J].生态学报,2019,39(1):333-344.
杨民英,李玉辉,庞丹波,等.基于GIS和RS的喀斯特水源地景观格局动态变化研究:以大春河小流域为例[J].四川农业大学学报,2016,34(2):227-233.
Chen F S, Zeng D H, XingY H E. Small-scale spatial variability of soil nutrients and vegetation properties in semi-arid northern China[J].Pedosphere,2006,16(6):778-787.
黄鹏.黄土丘陵区不同土地利用类型下土壤水分运移模拟研究[D].西安:西安理工大学,2018.
曾伟斌,邓琦,张全发.丹江口库区不同土地利用土壤碳氮含量的变化[J].土壤,2013,45(3):385-391.
舒晓,门杰.减氮配施有机物质对土壤氮素淋失的调控作用[J].水土保持学报,2019,33(1):186-191.
张亚娟,叶雪均,杨勇.贵州安顺市不同土地利用类型土壤养分特征研究[J].广东农业科学,2015,42(18):56-62.
Cao C Y, Jiang S Y, Ying Z. Spatial variability of soil nutrients and microbiological properties after the establishment of leguminous shrub
Caragana microphylla
Lam. plantation on sand dune in the Horqin Sandy Land of Northeast China[J].Ecological Engineering,2011,37(10):1467-1475.
Tesfahunegn G B, Tamene L, Vlek P L G. Catchment-scale spatial variability of soil properties and implications on site-specific soil management in northen Ethiopia[J].Soil and Tillage Research,2011,117:124-139.
Dubuis A, Giovanettina S, Loïc P. Improving the prediction of plant species distribution and community composition by adding edaphic to topo-climatic variables[J].Journal of Vegetation Science,2013,24(4):593-606.
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