|Table of Contents|

Soil Nutrient Distribution Characteristics of Baotou Nanhai Wetland in Different Seasons

《北方园艺》[ISSN:1001-0009/CN:23-1247/S]

Issue:
2023年20
Page:
69-76
Research Field:
Publishing date:

Info

Title:
Soil Nutrient Distribution Characteristics of Baotou Nanhai Wetland in Different Seasons
Author(s):
ZHOU Shifeng1WEI Yajuan2HE Lei3WANG Xiangfei4LIU Meiping2LIU Lanbo5
(1.Henan Vocational College of Agriculture,Zhengzhou,Henan 451450;2.Department of Resource and Environment,Baotou Teachers′ College,Baotou,Inner Mongolia 014030;3.College of Resources and Environmental Sciences,China Agricultural University,Beijing 100193;4.Urumqi Forestry and Grassland Bureau,Urumqi,Xinjiang 830000;5.Baotou Meteorological Bureau in Inner Mongolia Autonomous Region,Baotou,Inner Mongolia 014030)
Keywords:
soil nutrientsseasonspatial and temporal distributionBaotou Nanhai wetland
PACS:
S 714.2
DOI:
10.11937/bfyy.20230175
Abstract:
Soil physical and chemical properties of Nanhai Wetland in Baotou City,Inner Mongolia was used as test material,soil nutrient nutrient distribution characteristics and their influencing factors in different seasons (spring,summer and autumn) of Nanhai Wetland in Baotou City,Inner Mongolia were analyzed based on field sampling and lab analysis methods,in order to provide reference for the evaluation of soil quality in the region.The results showed that,1)the soil physicochemical indexes in Baotou Nanhai Wetland all conformed to normal distribution.Among them,total salinity,organic matter,total nitrogen and total phosphorus all had strong variability,indicating a large degree of variation in these four indicators in different seasons.2) The average soil organic matter,total nitrogen,total phosphorus and total potassium contents in different seasons ranged from 9.59 to 18.80 g·kg-1,0.36 to 0.70 g·kg-1,0.67 to 1.07 g·kg-1 and 16.21 to 22.39 g·kg-1,respectively.3) Total salinity,organic matter,total nitrogen and total phosphorus of each soil layer showed a trend of increasing and then decreasing with season,and soil pH and total potassium showed a decreasing trend with the season.4) Soil bulk density,soil moisture,total soil porosity,soil capillary porosity and soil non-capillary porosity varied with increasing soil depth within the same season.Soil total salinity,organic matter,total nitrogen and total phosphorus showed an accumulative decrease with soil depth.5) Redundancy analysis (RDA) revealed that pH and season were the potential drivers affecting soil nutrients in Nanhai Wetland.pH had dominant effect on soil nutrients amounting to 37.90% in Nanhai Wetland.The results will provide reference for the revegetation,ecological restoration and scientific management of the Yellow River wetland in Baotou.

References:

[1]崔乾,苗雨青,周光,等.鄱阳湖湿地典型植被群落土壤养分有效性特征[J].安徽师范大学学报(自然科学版),2020,43(1):80-85.[2]纪昌品,王华.鄱阳湖湿地植物群落分布特征及其对土壤环境因子的响应[J].生态环境学报,2018,27(8):1424-1431.[3]孙志高,刘景双,王金达,等.湿地生态系统土壤氮素矿化过程研究动态[J].土壤通报,2015,38(1):157-163.[4]吕铭志,盛连喜,张立.中国典型湿地生态系统碳汇功能比较[J].湿地科学,2013,11(1):114-120.[5]斯南雍茜,葛继稳,李愈,等.神农架大九湖亚高山典型泥炭湿地土壤养分特征分析[J].水土保持学报,2020,34(5):321-326.[6]孙飞达,李飞,陈文业,等.若尔盖退化高寒湿地土壤理化性质、酶活性及微生物群落的季节动态[J].生态学报,2020,40(7):2396-2406.[7]刘伟成,陈少波,郑春芳,等.乐清湾滨海湿地不同植被带土壤养分时空分布特征[J].土壤通报,2014,45(1):91-99.[8]胡维,葛刚,熊勇,等.鄱阳湖南矶山湿地土壤养分的时空分布规律研究[J].农业环境科学学报,2012,31(9):1785-1790.[9]周永维,葛瑶,艾宁,等.南泥湾湿地不同植被类型土壤养分变化规律与肥力评价[J].水土保持研究,2021,28(5):76-80,87.[10]乐易迅,胡敏杰,肖琳,等.河口湿地红树林植被恢复对土壤养分动态的影响[J].水土保持学报,2022,36(3):333-337.[11]纪昌品,张晓平.鄱阳湖不同湿地植物群落光合碳储量及分配[J].水土保持研究,2022,29(3):121-127.[12]郭舜,黄启堂.闽江河口湿地植物多样性与土壤养分和微生物因子关联分析[J].水土保持研究,2021,28(3):30-37.[13]杨文焕,王铭浩,李卫平,等.黄河湿地包头段不同地被类型对土壤有机碳的影响[J].生态环境学报,2018,27(6):1034-1043.[14]姜庆宏,王佳宁,李卫平,等.南海湖春季浮游植物群落结构及其与水质因子的关系[J].干旱区资源与环境,2018,32(8):166-171.[15]潘彤.南海湖浮游植物功能群季节演替特征及其影响因子分析[D].包头:内蒙古科技大学,2019.[16]于玲红,王铭浩,李卫平,等.包头南海湖沉积物有机碳空间分布特征[J].农业环境科学学报,2018,37(3):538-545.[17]王智超.4种植物混合浮床对南海湿地富营养化水体修复的研究[D].包头:内蒙古科技大学,2019.[18]王志超,王智超,缪晨霄,等.混合浮床对南海湖湿地富营养化水体修复的作用[J].水土保持通报,2019,39(4):120-126,133.[19]王越,于玲红,李卫平,等.基于PSR模型的包头黄河湿地分区生态健康评价[J].内蒙古大学学报(自然科学版),2016,47(3):328-336.[20]蔡楠,孙旭,刘永宏.包头黄河湿地不同植物群落土壤养分分布特征[J].北方园艺,2021(10):80-87.[21]杨荣,塞那,苏亮,等.内蒙古包头黄河湿地土壤碳氮磷含量及其生态化学计量学特征[J].生态学报,2020,40(7):2205-2214.[22]张天举,陈永金,刘加珍.黄河口湿地不同植物群落土壤盐分与养分分布特征[J].土壤,2020,52(1):180-187.[23]王高敏.晋西黄土区退耕16—20年间不同林地土壤理化性质和水文功能研究[D].北京:北京林业大学,2015.[24]鲍士旦.土壤农化分析[M].3版.北京:中国农业出版社,2000.[25]吴鹏,崔迎春,赵文君,等.喀斯特森林植被自然恢复过程中土壤化学计量特征[J].北京林业大学学报,2019,41(3):80-92.[26]杨再梅,谭伟,戚玉娇,等.茂兰喀斯特常绿落叶阔叶林土壤养分空间分布特征[J].福建农林大学学报(自然科学版),2021,50(3):404-412.[27]李恩宇,何贵永.青藏高原高寒草甸不同季节土壤理化性质及酶活性对施肥处理的响应[J].广西植物,2014,34(4):467-472,449.[28]陈永金,靖淑慧,杜婷婷,等.滨海湿地原生灌草群落土壤养分与盐分关系[J].南水北调与水利科技,2015,13(5):895-900.[29]王大伟,白军红,赵庆庆,等.黄河三角洲不同类型湿地土壤盐分的剖面分异特征[J].自然资源学报,2020,35(2):438-448.[30]肖烨,黄志刚,武海涛,等.三江平原典型湿地类型土壤微生物特征与土壤养分的研究[J].环境科学,2015,36(5):1842-1848.[31]王勇辉,董玉洁,艾尤尔·亥热提.艾比湖湿地泥炭土壤养分特征分析[J].干旱地区农业研究,2015,33(5):186-192.[32]高丽娟,吕光辉,王芸,等.艾比湖地区盐生植物群落土壤氮素的垂直分布特征[J].干旱区研究,2014,31(1):51-56.[33]CONG J,WANG X L,LIU X,et al.The distribution variation and key influencing factors of soil organic carbon of natural deciduous broadleaf forests along the latitudinal gradient[J].Acta Ecologica Sinica,2016,36(5):333-339.[34]刘学东,陈林,杨新国,等.白刺沙堆周围土壤理化性状的空间分布特征[J].北方园艺,2016(10):158-163.[35]SPARKS D L,LIEBHARDT W C.Temperature effects on potassium exchange and selectivity in Delaware soils[J].Soil Science,1982,133(1):10-17.[36]赵淑芳,胡尧.黄河流域不同湿地生态系统土壤呼吸和碳储量[J].北方园艺,2021(16):94-101.

Memo

Memo:
-
Last Update: 2023-11-30