The Determination of pH at Soil Moisture Contents Approximating Field Conditions

1941 ◽  
Vol 5 (C) ◽  
pp. 191-200 ◽  
Author(s):  
H. D. Chapman ◽  
John H. Axley ◽  
Denzel S. Curtis
Soil Research ◽  
1977 ◽  
Vol 15 (3) ◽  
pp. 205 ◽  
Author(s):  
AR Aston ◽  
FX Dunin

An empirical relationship was derived for drainage from a podzolic sandy loam using a weighing lysimeter at Krawarree, N.S.W. The form of the equation was similar to those used to describe drainage following irrigation. The agreement between computed and measured soil moisture contents over a period of five years was good, and indicated the usefulness of such an approach to characterize drainage of soil water under natural field conditions.


1956 ◽  
Vol 4 (1) ◽  
pp. 111-113
Author(s):  
P. Mortier ◽  
M. De Boodt

Curves of counting rate versus moisture content are presented, for sand, loam and clay soils, using (i) a 1000 me Ra-Be source surrounded by a small rigid indium cylinder acting as detector of slow neutrons and (ii) two co-axial Cd cylinders protecting the indium detector. Improved accuracy in the region of low moisture contents was obtained with (ii). (Abstract retrieved from CAB Abstracts by CABI’s permission)


1960 ◽  
Vol 6 (4) ◽  
pp. 439-452 ◽  
Author(s):  
G. Stotzky

A simple method for the determination of the respiratory quotient of soils is described. The advantages of this method over those previously described are: (1) Variability between identical treatments is minimized. (2) Errors arising from non-uniform respiration of replicated treatments are eliminated. (3) Soil moisture contents are maintained at a constant level. (4) R.Q.'s can be correlated directly with microbial activity as indicated by CO2evolution and both parameters are collected from a single soil sample for extended periods of time. (5) C14-enriched substrates may be used. (6) The composition of the ambient atmosphere can be easily controlled. A brief comparison of different methods is presented.


HortScience ◽  
1995 ◽  
Vol 30 (4) ◽  
pp. 868D-868
Author(s):  
Lurline E. Marsh ◽  
Dyremple B. Marsh

Increasing seed moisture has been beneficial in improving seedling emergence of some crops. Seed moisture contents of three cowpea (Vigna unguiculata) genotypes (MN13, Pinkeye Purple Hull, and IT 82E-16) and two pigeonpea (Cajanus cajan) (ICPL 85024 and ICPL 8304) were modified by incubating a 10 seed: 4 celite: 13 water (by weight) mixture at 15C. Conditioned seeds had moisture contents ranging from 46% to 64%, while nontreated seeds ranged from 4% to 8%. Matriconditioned and nontreated seeds had <15% emergence at 28 days after planting (DAP) in dry field conditions, where precipitation was <41 mm. In greenhouse tests at 14 DAP, matriconditioning had a negative effect on seeds in flooded, moist, and dry soils. The percent emergence for these seeds was 40% when compared to 60% for nontreated ones. Conditioning did not affect percent emergence at 7 DAP, days to first emergence, and percentage of germinated, unemerged seeds at 14 DAP. In the dry soil, emergence was less and later, and more germinated, unemerged seeds were present at 14 DAP. Cowpeas averaged 56% germination and pigeonpeas were 27%.


2013 ◽  
Vol 807-809 ◽  
pp. 1648-1652
Author(s):  
Tie Jun Sun ◽  
Baderihu Tajilake

Experiment was executed to plant eco-grass of Bromus inermis Leyss on 15°bare slopes, and study effect of biological characters on dynamics of soil moisture contents. The results indicated that vegetation restored quickly on the bare slope after the eco-grass planted. There were 2473.4 kg/hm2 of overground biomass and 1744.1kg/hm2 of underground biomass, and 70% of underground biomass was in 0-10cm layer of soil. Meanwhile, there was a regulatory mechanism of soil moisture content for Bromus inermis Leyss. When rainfall was enough, soil moisture content in 0-80 cm layer could reach to the most of 26.83% quickly this year. Next it could decline near to the first value of 19.81% after rainfall stopped, and keep a dynamic balance between 19.48% and 19.96%. Moreover, the regulatory mechanism realized though underground biomass, and was clearer with underground biomass increasing, especially in the 0-40cm layer of soil.


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