The contribution of agrotechnical works following a fire to the protection of forest soils and the regeneration of natural forest

Author(s):  
M.A. Sapountzis ◽  
G.S. Efthimiou ◽  
P.S. Stefanidis
Keyword(s):  

Geoderma ◽  
1998 ◽  
Vol 84 (4) ◽  
pp. 345-362 ◽  
Author(s):  
D Martin ◽  
P.C Srivastava ◽  
D Ghosh ◽  
W Zech


2008 ◽  
Vol 40 (9) ◽  
pp. 2079-2087 ◽  
Author(s):  
R. Zornoza ◽  
J. Mataix-Solera ◽  
C. Guerrero ◽  
V. Arcenegui ◽  
J. Mataix-Beneyto ◽  
...  


2004 ◽  
Vol 57 (3) ◽  
pp. 363-374 ◽  
Author(s):  
Nadia Ait Ali ◽  
Mohammed Ater ◽  
Geoffrey I. Sunahara ◽  
Pierre Yves Robidoux


2003 ◽  
Vol 44 (2) ◽  
pp. 198-209 ◽  
Author(s):  
P. Y. Robidoux ◽  
G. Bardai ◽  
L. Paquet ◽  
G. Ampleman ◽  
S. Thiboutot ◽  
...  
Keyword(s):  


2020 ◽  
Vol 100 (1) ◽  
pp. 69-80 ◽  
Author(s):  
Justine Lejoly ◽  
Sylvie A. Quideau ◽  
Frédéric Rees

Two types of organic-matter-rich coversoils are used during reclamation in the oil sands region of Alberta: forest floor material (FFM) salvaged from upland forests, and peat material (PM) salvaged from boreal wetlands. In this study, we tested the hypothesis that carbon (C) and nutrient availability may limit microbial activity in these reclamation materials by measuring their response to either 13C-labeled glucose or NPKS addition. Coversoil materials were compared with two natural forest soils corresponding to target sites for reclamation. A shift in microbial community structure (determined using phospholipid fatty acid analysis) was detected after both additions, but it was stronger with glucose than NPKS, especially for the two reclamation materials. For all soils, the increase in microbial respiration was stronger after glucose than after NPKS addition. The majority of CO2 originated from soil organic matter (SOM) for the natural forest soils but from glucose for the reclamation materials. In PM, glucose addition triggered SOM mineralization, as shown by a positive priming effect. Despite the absence of a priming effect for FFM, microbial communities incorporated higher rates of glucose into their biomass and respired double the amount of glucose compared with the other materials. Furthermore, the overall microbial community structure in the FFM became more similar to that of the natural forest soil materials following glucose addition. These findings indicate that C and NPKS limitations were stronger for the two reclamation materials than for the two natural forest soils. Furthermore, microbial communities in the two reclamation materials responded more readily to labile C than to NPKS addition.



2020 ◽  
Vol 2020 ◽  
pp. 1-8 ◽  
Author(s):  
Ricksy Prematuri ◽  
Maman Turjaman ◽  
Takumi Sato ◽  
Keitaro Tawaraya

The remediation of opencast bauxite mines in the natural forests of Indonesia is difficult. We have investigated and contrasted the chemical characteristics of soils from natural forests and mining sites and their effects on plant growth. The soil pH, total carbon (C), nitrogen (N) and available phosphorus (P) concentrations, cation exchange capacity, C/N ratio, and exchangeable K, Na, Mg, Ca, Fe, and Ni concentrations were determined. Falcataria moluccana and Albizia saman were then grown in these soils for 15 weeks, and their shoot heights, shoot dry weights, and root dry weights determined. The post bauxite mining soils’ N, C, and available P concentrations and exchangeable Ca, Mg, and Na concentrations decreased by 75, 75.7, 15.7, 92, 100, and 52%, respectively, in comparison with the natural forest soils. The shoot and root dry weights of F. moluccana when grown in the post bauxite mining soils were also lower than those from the natural forest soils. However, there was no difference in the shoot and root dry weights of A. saman when grown in the two soil types. The results suggest that opencast mining decreases the soil fertility, which in turn inhibits the initial growth of tree seedlings, and reduces the carbon stock in the land.



Geoderma ◽  
2016 ◽  
Vol 282 ◽  
pp. 139-146 ◽  
Author(s):  
Lefang Cui ◽  
Chao Liang ◽  
David S. Duncan ◽  
Xuelian Bao ◽  
Hongtu Xie ◽  
...  




Forests ◽  
2019 ◽  
Vol 10 (6) ◽  
pp. 492
Author(s):  
Peng-Dong Chen ◽  
Yu-Ping Hou ◽  
Yan-Hui Zhuge ◽  
Wei Wei ◽  
Qiao-Qiao Huang

Due to increasing globalization and human disturbance, plant invasion has become a worldwide concern. Soil characteristics associated with the vegetation of recipient communities affect plant invasion success to a great extent. However, the relative importance of soil biotic and abiotic factors of different recipient communities in resisting plant invasion is not fully understood. We hypothesized that natural forest soils can better resist plant invasion than can plantation soils, that the allelopathic legacy of resident trees in soil plays a role in resisting invasive plants, and that late-successional soils have a strong effect. We examined the effects of soil and litter collected from four natural forests at successional stages and one Robinia pseudoacacia Linn. plantation in eastern China on the growth of Phytolacca americana L., which is a highly invasive species across China, and explored the individual effects of soil nutrients, allelochemicals, and soil microbes. We found that allelopathic activity of natural forest soils can effectively resist P. americana invasion, and that low level of nutrients, especially of phosphorus, in the soils might be potential limiting factors for the plant growth. The profound conditioning of soil resources by exotic R. pseudoacacia based on tree traits (including allelopathy) facilitated further P. americana invasion. Allelochemicals from forest litter inhibited the germination of P. americana seeds, but pH played a major role in P. americana growth when these substances entered the soil. However, we have no evidence that late-successional forest soils exhibit strong allelopathy toward P. americana. The present study will help to further our understanding of the mechanism of community resistance to invasion.





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