波兰东南部卢布林高地由黄土发育而成的森林格洛斯特网状沉积物的物理特性研究

IF 1.4 Q4 SOIL SCIENCE Soil Science Annual Pub Date : 2023-11-08 DOI:10.37501/soilsa/174969
Maja Bryk
{"title":"波兰东南部卢布林高地由黄土发育而成的森林格洛斯特网状沉积物的物理特性研究","authors":"Maja Bryk","doi":"10.37501/soilsa/174969","DOIUrl":null,"url":null,"abstract":"Clay-illuvial soils with argic horizon and developed from loess or other silty deposits constitute high-quality arable land owing to favourable physical and chemical properties. There are thus numerous reports on such soils, considering their structure, compaction, erosion, water and air properties. However, there is still a lack of quantitative studies on structure and physical properties on analogous soils under forests. The aim of this research was therefore a comprehensive description of the physical state, including structure, water and air properties, of a forest Retisol developed from loess. Morphographic, morphological and morphometric parameters of structure, selected physicochemical and water and air properties and also relationships among the obtained parameters were analysed for genetic horizons O, Ah, AE, E, Bt/E, Bt, BtC and C. The fi eld survey and soil structure images indicated that the studied forest soil had an undisturbed sequence of genetic horizons. The soil structure was shaped by soil fl ora and fauna causing bioturbation. Qualitative and quantitative structure analysis revealed that the O horizon had a loose arrangement, the Ah horizon had an aggregate crumb structure, the AE horizon had zones of an aggregate crumb structure and non-aggregate structure ( fi ssured or with channels), while the remaining mineral horizons showed essentially a non-aggregate structure with varying proportions and sizes of planes and biogenic pores (i.e. cracked or fi ssured structure and structure with channels, respectively). The morphometric and physicochemical parameters facilitated a detailed analysis of the Retisol’s physical state. The Retisol’s structure type and degree of aggregate development directly in fl uenced its hydraulic conductivity and water retention capacity. Therefore, under simulated precipitation, the soil water content and effective saturation varied mainly in the topsoil (O–E horizons) and virtually no changes were observed in the subsoil (Bt–C horizons). The research resulted in a comprehensive analysis of the physicochemical and morphometric parameters, their relationships, and structure images that were previously unavailable in other studies, covering the physical state of the entire pedon of a forest Retisol. The results obtained may serve, for example, as a reference (control) for analogous soils located in non-forest ecosystems and become an element in space-for-time substitu-tion scenarios aimed at assessing the intensity of anthropogenic transformation","PeriodicalId":44772,"journal":{"name":"Soil Science Annual","volume":null,"pages":null},"PeriodicalIF":1.4000,"publicationDate":"2023-11-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Study on the physical properties of a forest Glossic Retisol developed from loess in the Lublin Upland, SE Poland\",\"authors\":\"Maja Bryk\",\"doi\":\"10.37501/soilsa/174969\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Clay-illuvial soils with argic horizon and developed from loess or other silty deposits constitute high-quality arable land owing to favourable physical and chemical properties. There are thus numerous reports on such soils, considering their structure, compaction, erosion, water and air properties. However, there is still a lack of quantitative studies on structure and physical properties on analogous soils under forests. The aim of this research was therefore a comprehensive description of the physical state, including structure, water and air properties, of a forest Retisol developed from loess. Morphographic, morphological and morphometric parameters of structure, selected physicochemical and water and air properties and also relationships among the obtained parameters were analysed for genetic horizons O, Ah, AE, E, Bt/E, Bt, BtC and C. The fi eld survey and soil structure images indicated that the studied forest soil had an undisturbed sequence of genetic horizons. The soil structure was shaped by soil fl ora and fauna causing bioturbation. Qualitative and quantitative structure analysis revealed that the O horizon had a loose arrangement, the Ah horizon had an aggregate crumb structure, the AE horizon had zones of an aggregate crumb structure and non-aggregate structure ( fi ssured or with channels), while the remaining mineral horizons showed essentially a non-aggregate structure with varying proportions and sizes of planes and biogenic pores (i.e. cracked or fi ssured structure and structure with channels, respectively). The morphometric and physicochemical parameters facilitated a detailed analysis of the Retisol’s physical state. The Retisol’s structure type and degree of aggregate development directly in fl uenced its hydraulic conductivity and water retention capacity. Therefore, under simulated precipitation, the soil water content and effective saturation varied mainly in the topsoil (O–E horizons) and virtually no changes were observed in the subsoil (Bt–C horizons). The research resulted in a comprehensive analysis of the physicochemical and morphometric parameters, their relationships, and structure images that were previously unavailable in other studies, covering the physical state of the entire pedon of a forest Retisol. The results obtained may serve, for example, as a reference (control) for analogous soils located in non-forest ecosystems and become an element in space-for-time substitu-tion scenarios aimed at assessing the intensity of anthropogenic transformation\",\"PeriodicalId\":44772,\"journal\":{\"name\":\"Soil Science Annual\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2023-11-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Soil Science Annual\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.37501/soilsa/174969\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil Science Annual","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.37501/soilsa/174969","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0

摘要

由黄土或其他淤泥沉积物发育而成的含阿尔卡地层的粘土-冲积土因其有利的物理和化学特性而成为优质耕地。因此,关于这类土壤的报告不胜枚举,其中考虑到了其结构、压实、侵蚀、水和空气特性。然而,对森林中类似土壤的结构和物理特性仍缺乏定量研究。因此,本研究的目的是全面描述由黄土发展而来的森林 Retisol 的物理状态,包括结构、水和空气特性。研究分析了 O、Ah、AE、E、Bt/E、Bt、BtC 和 C 基因层的形态学、形态和形态计量学参数、选定的物理化学和水气性质,以及所获参数之间的关系。土壤结构是由土壤层和动物群造成的生物扰动形成的。定性和定量的结构分析表明,O 层具有松散的排列,Ah 层具有聚集的碎屑结构,AE 层具有聚集的碎屑结构区和非聚集结构区(稳定的或有通道的),而其余矿物层基本上是非聚集结构,具有不同比例和大小的平面和生物孔隙(即裂缝或稳定的结构和有通道的结构)。形态计量和物理化学参数有助于对 Retisol 的物理状态进行详细分析。Retisol 的结构类型和骨料发育程度直接影响其导水率和保水能力。因此,在模拟降水条件下,土壤含水量和有效饱和度主要在表土(O-E 层)发生变化,而在底土(Bt-C 层)几乎没有变化。这项研究对物理化学和形态计量参数、它们之间的关系以及结构图像进行了全面分析,这是以前其他研究中无法获得的,它涵盖了森林网状土壤整个地层的物理状态。例如,研究结果可作为非森林生态系统中类似土壤的参考(对照),也可作为旨在评估人为改造强度的时空置换方案的一个要素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Study on the physical properties of a forest Glossic Retisol developed from loess in the Lublin Upland, SE Poland
Clay-illuvial soils with argic horizon and developed from loess or other silty deposits constitute high-quality arable land owing to favourable physical and chemical properties. There are thus numerous reports on such soils, considering their structure, compaction, erosion, water and air properties. However, there is still a lack of quantitative studies on structure and physical properties on analogous soils under forests. The aim of this research was therefore a comprehensive description of the physical state, including structure, water and air properties, of a forest Retisol developed from loess. Morphographic, morphological and morphometric parameters of structure, selected physicochemical and water and air properties and also relationships among the obtained parameters were analysed for genetic horizons O, Ah, AE, E, Bt/E, Bt, BtC and C. The fi eld survey and soil structure images indicated that the studied forest soil had an undisturbed sequence of genetic horizons. The soil structure was shaped by soil fl ora and fauna causing bioturbation. Qualitative and quantitative structure analysis revealed that the O horizon had a loose arrangement, the Ah horizon had an aggregate crumb structure, the AE horizon had zones of an aggregate crumb structure and non-aggregate structure ( fi ssured or with channels), while the remaining mineral horizons showed essentially a non-aggregate structure with varying proportions and sizes of planes and biogenic pores (i.e. cracked or fi ssured structure and structure with channels, respectively). The morphometric and physicochemical parameters facilitated a detailed analysis of the Retisol’s physical state. The Retisol’s structure type and degree of aggregate development directly in fl uenced its hydraulic conductivity and water retention capacity. Therefore, under simulated precipitation, the soil water content and effective saturation varied mainly in the topsoil (O–E horizons) and virtually no changes were observed in the subsoil (Bt–C horizons). The research resulted in a comprehensive analysis of the physicochemical and morphometric parameters, their relationships, and structure images that were previously unavailable in other studies, covering the physical state of the entire pedon of a forest Retisol. The results obtained may serve, for example, as a reference (control) for analogous soils located in non-forest ecosystems and become an element in space-for-time substitu-tion scenarios aimed at assessing the intensity of anthropogenic transformation
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Soil Science Annual
Soil Science Annual SOIL SCIENCE-
CiteScore
2.50
自引率
6.70%
发文量
0
审稿时长
29 weeks
期刊介绍: Soil Science Annual journal is a continuation of the “Roczniki Gleboznawcze” – the journal of the Polish Society of Soil Science first published in 1950. Soil Science Annual is a quarterly devoted to a broad spectrum of issues relating to the soil environment. From 2012, the journal is published in the open access system by the Sciendo (De Gruyter).
期刊最新文献
Assessment of soil erosion in the Beas Valley, Kullu, Himachal Pradesh: A study of Western Himalayan landscape, Northern India Characterization of the “Waru Waru” soils on the Peruvian high plateau Linking marginal soil to sugarcane productivity in Takalar, Indonesia Topsoil organic carbon and soil pH across different peatland use types in Co-Offaly, Ireland Influence of prolonged agrogenic transformation on soil structure and physicochemical properties of Ukrainian Albic Stagnic Luvisols: a case study from western Ukraine
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1