Soil Carbon-Nitrogen-Water Relations in Forests

A special issue of Land (ISSN 2073-445X). This special issue belongs to the section "Soil-Sediment-Water Systems".

Deadline for manuscript submissions: closed (28 February 2023) | Viewed by 1928

Special Issue Editors

Departament of Botany and Forest Habitats, Faculty of Forestry and Wood Technology, Poznań University of Life Sciences, Wojska Polskiego 71f, 60-625 Poznań, Poland
Interests: ekohydrology; forest floor hydrology; stemflow; throughfall; bark hydrology
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Guest Editor
Department of Sol Science, Environmental Chemistry and Hydrology, University of Rzeszow, ul. Zelwerowicza 8B, Budynek D7, 35-601 Rzeszów, Poland
Interests: impact of waste use in agriculture on soil properties and plant growth and development; soil contamination with trace elements; effect of the tillage system on soil organic matter properties
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Special Issue Information

Dear Colleagues,

In forest ecosystems, the primary water source is precipitation, which reaches the forest as rainfall, fog, or snow. When precipitation reaches the soil surface, it infiltrates the soil profile, is stored in the soil, or evaporates into the atmosphere. A crucial role in this process is played by soil organic matter (SOM), which is accumulated mainly in the top part of the soil profile. Forests of different species compositions have different impacts on the quantity and quality of the supplied aboveground and underground organic matter, as well as other properties, such as pH, the amount of N and C, and the circulation of nutrients. The decomposition of organic matter is the basic process regulating the nutrient cycle, primarily carbon, and in turn, the degree of decomposition and the quantity and quality of organic matter significantly affect soil water content. For nutrient-poor soils where water content is highly variable, nutrient availability is a frequent limiting factor for ecosystem development, and net primary production requires water and nutrient availability. Therefore, in this Special Issue, we argue that understanding the carbon, nitrogen, and water relations in forest areas is highly important in climate change projections as areas where warmer and drier conditions are predicted to have more severe and recurrent droughts.

We are interested in contributions that intimately link soil carbon–nitrogen–water to forest ecosystems while focusing on the social science aspects of improving carbon, nitrogen, and water resources in forest areas, use, and policy. Contributions can either be empirical research or conceptual works, examining any key processes, including but not limited to:

  • Influence of stand species' composition on carbon, nitrogen, and the water cycle ;
  • Influence of drought on carbon–nitrogen–water relations in forest;
  • Influence of decomposition of aboveground and underground organic matter on the carbon, nitrogen, and water relations;
  • New methods for examing carbon–nitrogen–water relations.

Dr. Anna Ilek
Dr. Małgorzata Szostek
Guest Editors

Manuscript Submission Information

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Keywords

  • climate change
  • forest ecosystems
  • soil organic matter
  • soil carbon-nitrogen-water interactions
  • water cycle
  • carbon and nitrogen cycles

Published Papers (1 paper)

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Research

18 pages, 1721 KiB  
Article
Nitrogenous and Phosphorus Soil Contents in Tierra del Fuego Forests: Relationships with Soil Organic Carbon, Climate, Vegetation and Landscape Metrics
by Guillermo Martínez Pastur, Marie-Claire Aravena Acuña, Jimena E. Chaves, Juan M. Cellini, Eduarda M. O. Silveira, Julián Rodriguez-Souilla, Axel von Müller, Ludmila La Manna, María V. Lencinas and Pablo L. Peri
Land 2023, 12(5), 983; https://doi.org/10.3390/land12050983 - 28 Apr 2023
Cited by 1 | Viewed by 1521
Abstract
Soil nitrogen (SN) and soil phosphorus (SP) contents support several ecosystem services and define the forest type distribution at local scale in Southern Patagonia. The quantification of nutrients during forest surveys requires soil samplings and estimations that are costly and difficult to measure. [...] Read more.
Soil nitrogen (SN) and soil phosphorus (SP) contents support several ecosystem services and define the forest type distribution at local scale in Southern Patagonia. The quantification of nutrients during forest surveys requires soil samplings and estimations that are costly and difficult to measure. For this, predictive models of soil nutrients are needed. The objective of this study was to quantify SN and SP contents (30 cm depth) using different modelling approaches based on climatic, topographic and vegetation variables. We used data from 728 stands of different forest types for linear regression models to map SN and SP. The fitted models captured the variability of forest types well (R²-adj. 92–98% for SN and 70–87% for SP). The means were 9.3 ton ha−1 for SN and 124.3 kg ha−1 for SP. Overall, SN values were higher in the deciduous forests than those in the mixed evergreen, while SP was the highest in the Nothofagus pumilio forests. SN and SP are relevant metrics for many applications, connecting major issues, such as forest management and conservation. With these models, the quantification of SN and SP stocks across forests of different protection status (National Law 26,331/07) and national/provincial reserve networks is possible, contributing to the determination of nutrient contents at landscape level. Full article
(This article belongs to the Special Issue Soil Carbon-Nitrogen-Water Relations in Forests)
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