CHARACTERIZATION OF SOIL-WATER RETENTION OF A VERY GRAVELLY LOAM SOIL VARIED WITH DETERMINATION METHOD

Soil Science ◽  
2006 ◽  
Vol 171 (2) ◽  
pp. 85-93 ◽  
Author(s):  
Rashid Al-Yahyai ◽  
Bruce Schaffer ◽  
Frederick S. Davies ◽  
Rafael Mu??oz-Carpena
Land ◽  
2021 ◽  
Vol 10 (2) ◽  
pp. 195 ◽  
Author(s):  
Mirko Castellini ◽  
Anna Maria Stellacci ◽  
Danilo Sisto ◽  
Massimo Iovino

The multi-height (low, L = 3 cm; intermediate, M = 100 cm; high, H = 200 cm) Beerkan run methodology was applied on both a minimum tilled (MT) (i.e., up to a depth of 30 cm) and a no-tilled (NT) bare loam soil, and the soil water retention curve was estimated by the BEST-steady algorithm. Three indicators of soil physical quality (SPQ), i.e., macroporosity (Pmac), air capacity (AC) and relative field capacity (RFC) were calculated to assess the impact of water pouring height under alternative soil management practices. Results showed that, compared to the reference low run, M and H runs affected both the estimated soil water retention curves and derived SPQ indicators. Generally, M–H runs significantly reduced the mean values of Pmac and AC and increased RFC for both MT and NT soil management practices. According to the guidelines for assessment of SPQ, the M and H runs: (i) worsened Pmac classification of both MT and NT soils; (ii) did not worsen AC classification, regardless of soil management parameters; (iii) worsened RFC classification of only NT soil, as a consequence of insufficient soil aeration. For both soil management techniques, a strong negative correlation was found between the Pmac and AC values and the gravitational potential energy, Ep, of the water used for the infiltration runs. A positive correlation was detected between RFC and Ep. The relationships were plausible from a soil physics point of view. NT soil has proven to be more resilient than MT. This study contributes toward testing simple and robust methods capable of quantifying soil degradation effects, due to intense rainfall events, under different soil management practices in the Mediterranean environment.


2019 ◽  
Vol 14 (No. 2) ◽  
pp. 67-75
Author(s):  
Hana Hlaváčiková ◽  
Viliam Novák ◽  
Koji Kameyama ◽  
Katarína Brezianska ◽  
Marek Rodný ◽  
...  

Biochar (BC) is used as a soil amendment to enhance plant growth by improving mainly soil chemical and hydrophysical properties. In this work the effects of two types of BCs on soil water retention properties were analysed. The first type of BC was made from sugarcane bagasse. It was added to a clay “Shimajiri Maji” soil at an application rate of 3 w%. The second type of BC was made from paper fiber sludge and grain husks. It was added into a loam soil at rates of 3.6, and 7.3 w%. It was assumed that the effect of BC amendment will be more pronounced in coarse-grained soil than in fine-grained one. Therefore, the second type of BC was applied additionally in the silica sand, in a textured contrast material compared with the loam soil. The BC amendment caused statistically significant increase of water content in the transmission pores of the clay soil, in the storage pores of the loam soil, and in the macropores and the storage pores in the silica sand. Despite of the positive effect on soil water retention, statistically significant increase of available water capacity (AWC) was identified only in the loam soil with the larger BC amendment rate. Possible reasons are discussed.


Soil Science ◽  
1995 ◽  
Vol 159 (1) ◽  
pp. 1-12 ◽  
Author(s):  
P. J. SHOUSE ◽  
W. B. RUSSELL ◽  
D. S. BURDEN ◽  
H. M. SELIM ◽  
J. B. SISSON ◽  
...  

2009 ◽  
Author(s):  
Luis P Barquin ◽  
Kati W Migliaccio ◽  
Rafael Muñoz-Carpena ◽  
Bruce Schaffer ◽  
Jonathan Crane ◽  
...  

1987 ◽  
Vol 67 (2) ◽  
pp. 395-397 ◽  
Author(s):  
D. S. STEVENSON

Soil water contents of a sandy loam and a silt loam soil were measured at −1500, −100, and either −20 or −30 kPa (the finer texture at −30 kPa) on pressure plate equipment, after samples of each soil had been treated with one of three soil conditioners or with water as a control treatment. One of the soil conditioners increased the soil water retention of both soils at all matric potentials while the other two increased soil water retention at −1500 kPa in the silt loam. The implications in terms of water availability to plants are discussed briefly. Key words: Matric potentials, soil water retention, soil conditioners, laboratory


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