|Table of Contents|

Variation of Soil Physicochemical Properties in the Root System of Forsythia at Different Altitudes

《北方园艺》[ISSN:1001-0009/CN:23-1247/S]

Issue:
2023年13
Page:
69-76
Research Field:
Publishing date:

Info

Title:
Variation of Soil Physicochemical Properties in the Root System of Forsythia at Different Altitudes
Author(s):
CHEN Hongyu1; CHEN Yunteng1; HUANG Bingxu1; REN Shifu1; REN Zibei2
(1.College of Forestry，Hebei Agricultural University，Baoding，Hebei 071000；2.Shijiazhuang Post & Telecommunication Technical College，Shijiazhuang，Hebei 050020)
Keywords:
:altitude; soil physical and chemical properties; principal component analysis
PACS:
-
DOI:
10.11937/bfyy.20224401
Abstract:
The root soil of Forsythia suspensa from two producing areas were used as the test material.The contents of organic matter，organic carbon,alkali hydrolyzable N，available phosphorus and available potassium in the root soil of Forsythia suspensa at different altitudes were determined by random sampling method，and the soil fertility was comprehensively evaluated，in order to provide reference for largEscale cultivation and artificial nurturing management of Forsythia suspensa，and promote scientific production.The results showed that both soils hadvery high levels of organic matter，organic carbon and alkali hydrolyzable N，but the contents of available phosphorus and available potassium were moderate and below，and the soil pH was relatively high，it was neutral and weakly alkaline soil.There was a significant positive correlation between soil organic matter，organic carbon，and alkali hydrolyzable N，all of which were positively correlated with altitude and negatively correlated with pH.There was a high correlation between available phosphorus，organic matter，and pH，while available potassium mainly came from soil parent materials，and its content changes were related to mountain environments at different altitudes.The highest soil fertility in both areas ranges from 900 m to 1 000 m，with abovEaverage soil fertility concentrated in the range of 700 m to 1 000 m in Jingxing county and 900 m to 1 100 m in She county.This characteristic had scientific significance for the cultivation and production of Forsythia suspensa.

References:

[1]常耀文,张瑞强,姜洪涛,等.内蒙古荒漠草原南缘春季消融期土壤水热变化特征及其对气象因子的响应[J].草原与草坪,2021,41(4):111-119.[2]JIANG F，WU X H，XIANG W H，et al.Spatial variations in soil organic carbon，nitrogen and phosphorus concentrations related to stand characteristics in subtropical areas[J].Plant and Soil，2017，413(1/2):289-301.[3]马国飞,满苏尔?沙比提,张雪琪.托木尔峰自然保护区台兰河上游不同海拔灌木土壤理化性质研究[J].土壤通报,2017,48(6):1288-1295.[4]张广杰,巢林,张伟东,等.亚热带森林土壤理化性质的异质性和最佳取样量[J].应用生态学报,2018,29(7):2139-2148.[5]黄婷,周冀衡,李强,等.不同海拔高度植烟土壤pH分布情况及其与土壤养分的关系:以云南省曲靖市为例[J].土壤通报,2015,46(1):105-110.[6]李相楹,张维勇,刘峰,等.不同海拔高度下梵净山土壤碳、氮、磷分布特征[J].水土保持研究,2016,23(3):19-24.[7]程浩,张厚喜,黄智军,等.武夷山不同海拔高度土壤有机碳含量变化特征[J].森林与环境学报,2018,38(2):135-141.[8]徐胜涛,何翔,杨佩文,等.不同海拔高度下香蕉园土壤理化性质及果实品质的变化[J].西南农业学报,2020,33(6):1215-1220.[9]沈霞,徐蓉蓉,裴丽珊,等.基于网络药理学连翘清热解毒功效的分子机制研究[J].药学学报,2018,53(11):1834-1842.[10]牛芳芳.河北太行山连翘药用林栽培关键技术调查研究[D].石家庄：河北农业大学,2013.[11]周颖,周鑫伟,郑听,等.生物炭对药用植物生长影响的研究进展[J].河南农业科学,2022,51(1):11-20.[12]吴娟娟,朱斌,史娟,等.药用植物种植与生产地重金属污染分析与评价[J].西北农林科技大学学报(自然科学版),2022,50(2):103-114.[13]葛阳,万修福,王升,等.氮肥对药用植物生态系统中土壤及三级营养关系的影响及机制[J].中国中药杂志,2021,46(8):1893-1900.[14]吴红淼,林文雄.药用植物连作障碍研究评述和发展透视[J].中国生态农业学报(中英文),2020,28(6):775-793.[15]刘引,戴蒙,鲍五洲,等.麻城不同产地菊花中矿质元素含量特征及其与土壤养分和有效成分的相关性研究[J].中国中药杂志,2021,46(2):281-289.[16]张姣,张晓虎,阎佩云.洛南县连翘种植区土壤养分状况及空间分布特征初步研究[J].中国农学通报,2020,36(10):95-101.[17]雷立,任宏力,李惠民,等.商洛不同产地连翘有效成分含量与土壤因子的相关性研究[J].山东农业科学,2016,48(5):55-57，61.[18]张建军.生态因子及抚育对野生连翘生长和产量的影响[J].山西农业大学学报(自然科学版),2013,33(1):10-15.[19]尹鑫,许利平,薛乾鑫,等.承德地区柴胡根际土壤因子与药材质量的关系[J].北方园艺,2022(8):95-101.[20]刘大会,郭兰萍,黄璐琦,等.矿质营养对药用植物黄酮类成分合成的影响[J].中国中药杂志,2010,35(18):2367-2371.[21]罗林,周应书,毕宁,等.喀斯特山区药用植物栽培环境变化与土壤化学性质的相关性[J].西部林业科学,2018,47(3):35-40.[22]SHEN C C，NI Y Y，LIANG W J，et al.Distinct soil bacterial communities along a smallscale elevational gradient in alpine tundra[J].Frontiers in Microbiology,2015（6）:582.[23]COTRUFO M F,SOONG J L,HORTON A J.Formation of soil organic matter via biochemical and physical pathways of litter mass loss[J].Nature Geoscience，2015,8(7):776-779.[24]李学斌,李月飞,陈林,等.宁夏荒漠草原不同土地利用方式对土壤活性有机碳的影响[J].北方园艺,2021(1):91-99.[25]董廷发.不同海拔云南松林土壤养分及其生态化学计量特征[J].生态学杂志,2021,40(3):672-679.[26]王镇,荆永锋,白刚,等.巴东烟区不同海拔和类型土壤养分差异分析[J].中国农学通报,2011,27(29):251-256.[27]颜秋晓,张维勇,石磊,等.梵净山自然保护区不同海拔林下土壤养分特征[J].贵州农业科学,2015,43(8):146-150.[28]李春雨,加鹏华,王树涛,等.阜平县不同海拔梯度下耕地土壤养分现状与分布特征[J].水土保持研究,2022,29(1):197-204.[29]CAO Y E，WANG Y，XU Z L.Soil C:P ratio along elevational gradients in picea schrenkiana forest of Tianshan Mountains[J].Polish Journal of Ecology，2019，66(4)：325-336.[30]任启文,王鑫,李联地,等.小五台山不同海拔土壤理化性质垂直变化规律[J].水土保持学报,2019,33(1):241-247.[31]OLANDER L P，VITOUSEK，P M.Regulation of soil phosphatase and chitinase activity by N and P availability[J].Biogeochemistry,2000，49(2)，175-190.[32]林巧玉,曾泉鑫,元晓春,等.氮添加对亚热带黄山松林土壤磷组分的影响[J].林业科学研究,2022,35(4):170-178.[33]谢欢,张秋芳,陈廷廷,等.氮添加促进丛枝菌根真菌和根系协作维持土壤磷有效性[J].植物生态学报,2022,46(7):811-822.[34]CHEN S，YAN Z J，ZHANG S，et al.Nitrogen application favors soil organic phosphorus accumulation in calcareous vegetable fields[J].Biology and Fertility of Soils，2019,55(5):481-496.[35]GEORGE T S，TURNER B L，GREGORY P J，et al.Depletion of organic phosphorus from Oxisols in relation to phosphatase activities in the rhizosphere[J].European Journal of Soil Science，2006,57(1):47-57.[36]LI L，MCCORMACK M L，CHEN F S.Different responses of absorptive roots and arbuscular mycorrhizal fungi to fertilization provide diverse nutrient acquisition strategies in Chinese fir[J].Forest Ecology and Management，2019,433:64-72.[37]李娟,王文丽,赵旭.生物肥料HZ-24对黄芪生长及土壤微生物数量和酶活性的影响[J].土壤与作物,2022,11(2):200-208.[38]曹婧,陈怡平,江瑶,等.陕西省农田土壤速效钾时空变化及其影响因素[J].水土保持学报,2021,35(5):296-302,311.[39]董艳红,王火焰,周健民,等.不同土壤钾素淋溶特性的初步研究[J].土壤,2014,46(2):225-231.[40]李兴民,车克钧,杨永红,等.白龙江上游不同海拔森林土壤养分变化规律研究[J].甘肃农业大学学报,2014,49(6):131-137.[41]王瑞永,刘莎莎,王成章,等.不同海拔高度高寒草地土壤理化指标分析[J].草地学报,2009,17(5):621-628.[42]孙彩丽,王艺伟,王从军,等.喀斯特山区土地利用方式转变对土壤酶活性及其化学计量特征的影响[J].生态学报,2021,41(10):4140-4149.[43]宋涛,朴世领,陈旸,等.苹果梨园土壤pH值与速效磷的变化规律研究[J].延边大学农学学报,2018,40(3):9-15.

Memo

Memo:
-
Last Update: 2023-08-21