Assessment of earthworms as an indicator of soil degradation: A case‐study on loess soils

Author(s):  
Yanpei Li ◽  
Jiao Wang ◽  
Ming'an Shao
Keyword(s):  



2012 ◽  
Vol 28 (4) ◽  
pp. 625-634
Author(s):  
B. G. J. S. Sonneveld ◽  
D. McGarry ◽  
D. Ndiaye
Keyword(s):  


2006 ◽  
Vol 11 (4) ◽  
pp. 477-492 ◽  
Author(s):  
JOHN M. ANTLE ◽  
JETSE J. STOORVOGEL ◽  
ROBERTO O. VALDIVIA

This paper provides a new explanation for the persistent land degradation in some parts of the world, despite the availability of seemingly effective soil conservation technologies. We demonstrate that soil conservation technologies may induce agricultural systems to exhibit equilibria characterized by both low and high levels of soil degradation. These two equilibria are separated by a threshold level of soil degradation beyond which a conservation investment will not yield a positive return. Once a parcel of land crosses this productivity threshold, soil degradation becomes economically irreversible (it is not profitable to invest in soil conservation) even though the degradation may be technically reversible. A case study of terracing investments in Peru is used to demonstrate the existence of multiple equilibria under conditions typical of many marginal agricultural areas. These findings help explain why attempts to encourage permanent adoption of soil conservation practices often fail, and how more successful policies could be designed.



2019 ◽  
Vol 38 (2) ◽  
pp. 221-229
Author(s):  
ANEESH M R ◽  
◽  
SURESH S ◽  
MANI K ◽  
◽  
...  
Keyword(s):  


2012 ◽  
Vol 16 (3) ◽  
pp. 953-966 ◽  
Author(s):  
G. Romanescu ◽  
V. Cotiuga ◽  
A. Asandulesei ◽  
C. Stoleriu

Abstract. The 3-D scanner, a rapid and precise means of monitoring the dynamics of erosive processes, was first used nationally (Romania) as a new technique of cartography and monitoring the dynamics of soil degradation processes in the Moldavian Plateau. Three sets of measurements took place: in 2008, in 2009 and in 2010, at intervals of exactly one year for the first and six months for the second part. Qualitative and quantitative differences were highlighted. The data obtained were corroborated with precipitation in the area studied. The 3-D scanner has a measurement accuracy of 6 mm. The map highlights the dynamics of gullies developed and may form the basis for the prediction of soil degradation phenomena. The dynamics of the gully and the type of land use show that the phenomenon of erosion of the Moldova Plateau will continue to accelerate. In this case, the gully attacked and destroyed an archaeological site of national importance. The rate of advance of the Cucuteni-Baiceni gully is extremely high (10 m/1.6 years). There are no measures at all to reduce or fight the process of the gully advance. Maximum erosion occurred at the beginning of spring after a winter rich in rainfall, which made the terrain subject to the process of subsidence.



2009 ◽  
Vol 20 (5) ◽  
pp. 551-561 ◽  
Author(s):  
I. Emadodin ◽  
S. Reiss ◽  
A. V. Mitusov ◽  
H. R. Bork
Keyword(s):  


Sign in / Sign up

Export Citation Format

Share Document