scholarly journals Surface soil sampling plan for the 200-UP-2 operable unit

1994 ◽  
Author(s):  
R.M. Mitchell
1967 ◽  
Author(s):  
Sterling J. Knight ◽  
Claude A. Blackmon
Keyword(s):  

2016 ◽  
Vol 25 (3) ◽  
pp. e070 ◽  
Author(s):  
Mustafa-Nawaz Shafqat ◽  
Salina Shahid ◽  
Syed-Ali-Musstjab-Akber-Shah Eqani ◽  
Syed-Haider Shah ◽  
Amir Waseem

Aims of the study: This study aims (i) to monitor the amount of dust deposition during dry season in the moist temperate forest; (ii) to study nature of P fractions in the dust samples falling on the trees in the region; (iii) to study soil P fractions as influenced by the processes of throughfall and stemflow of a Blue Pine (Pinus wallichiana) canopy and to finger print the contribution of dust towards P input in the temperate forest ecosystem.Area of study: The site used for the collection of soil samples was situated at an elevation of 6900 feet above sea levels (temperate forest in Himalaya region) in the Thandani area national forest located in the north west of Pakistan.Material and methods:  For soil sampling and processing, three forest sites with three old tree plants per site were selected at approximately leveled plain for surface soil sampling. Two dust samples were collected and analyzed for different physicochemical properties along with different P fractions. First dust sample was collected from a site situated at an elevation of 4000 feet and second one was collected from an elevation of 6500 feet above sea levels. Modified Hedley procedure for the fractionation of P in the dust and soil samples were used.Main results: The input of dust was 43 and 20 kg ha-1 during drier months of the year (September-June) at lower and higher elevation sites respectively, and the dust from lower elevation site had relative more all P fractions than the other dust sample. However, HCl-Pi fraction was dominant in both samples. Both labile (water plus NaHCO3) and non-labile (NaOH plus HCl) inorganic P (Pi) fractions were significantly increased in the surface soil by both stemflow and throughfall compared to the open field soil. The buildup of NaOH and HCl-Pi pools in soils underneath the canopy might prove useful in fingerprinting the contribution of atmospheric dust towards P cycling in this temperate forest.Research highlights: The role of dust in the cycling of P in temperate forest in Himalaya region.Keywords: soil phosphorus fractions; atmospheric dust; stemflow, throughfall; temperate forest.


1963 ◽  
Vol 3 (9) ◽  
pp. 105 ◽  
Author(s):  
DP Drover

The results of an eight year lysimeter study conducted at Muresk, Western Australia, are presented. The lysimeters contained two soils, a lateritic sandplain and a noncalcic brown soil, upon which various agronomic treatments were imposed. Mean annual leaching losses of nitrate-nitrogen from the sandplain soil were 4 to 7 lb N per acre under fallow and 6 lb N per acre from subterranean clover pasture. Losses of nitrate-nitrogen from wheat, either with added urea or clover residues (equivalent to 60 lb N per acre) were much higher, viz, 14 to 21 lb N per acre. From the noncalcic brown soil, losses under fallow were 3 to 6 lb N per acre, under clover pasture 2 lb N per acre, and under wheat, either with urea or clover residue added, 4 to 19 lb N per acre. For the sandplain soil, mean annual losses per acre of constituents other than nitrogen were 6 lb K ; 13 lb Ca ; 5 lb Mg ; less than 0.2 lb P ; and 2 to 7 lb S. For the noncalcic brown soil the losses were much lower, viz., 1 lIb K ; 7 lb Ca ; 3 lb Mg; less than 0.2 lb P ; and 0 to 7 lb S. The leaching losses of K, Ca and Mg were related to plant cover, being higher under wheat than under fallow, particularly with the sandplain soil. A n attempt was made to relate changes in nitrogen content of the surface soil at the end of the experiment to the net gain (input minus output) of nitrogen over the same period. This approach was unsatisfactory due largely to the statistical errors associated with soil sampling.


2007 ◽  
Vol 47 (2) ◽  
pp. 208 ◽  
Author(s):  
B. W. Dunn ◽  
H. G. Beecher

Irrigated agriculture has contributed to increasing topsoil acidity, which in turn can increase acidification of the subsoil. Lime is typically applied at a uniform rate to raise the pH of the soil, with no accounting for the variation in soil acidity that may exist within a field. Current commercial sampling protocols use surface soil composites taken across the whole field or in parts of fields where visual soil differences are apparent. Current liming recommendations may not account for in-field soil pH spatial variability, especially if the variability is not related to visual differences. Three studies were undertaken over 10 fields, to investigate the potential of using electro-magnetic induction instruments (Geonics EM38 and EM31) to target soil sampling in order to identify differences in soil acidity within flood-irrigated fields in southern New South Wales (NSW), Australia. Within individual fields, large differences in surface soil acidity were identified and a strong relationship (r2 = 0.49 to 0.91) between the soil’s apparent electrical conductivity and soil pH was found. It is proposed that fields from southern NSW that have grown rice, be divided into zones to soil sample for acidity assessment, based on EM instrument readings. Proposed ECa levels for the delineation of zones are <80, 80–140 and >140 mS/m for EM31v and <80, 80–110 and >110 mS/m for EM38v. Many rice growers in southern NSW currently have EM maps of their fields. Using these maps to target soil sampling for soil acidity would be a more cost-effective method of determining the spatial variability of soil acidity in a field than grid sampling. Knowledge of the variability of soil acidity within the field would potentially allow the application of appropriate lime rates, relative to soil pH and cation exchange capacity to all parts of the field. This knowledge could make the variable application of lime a cost effective approach, compared with whole field management approaches.


1983 ◽  
Vol 101 (2) ◽  
pp. 495-497 ◽  
Author(s):  
A. N. Ganeshamurthy

Plant roots may extend as far or farther below the ground than the plant does above. Given ample space the root system of a single plant may have a total spread of 1·2 m in wheat and 2·4 m in maize. Although a major part of the nutrients are absorbed by crops from the surface soil, subsurfacesoil contributions are often substantial. Part of the nutrients applied to surface soil may leach down and accumulate in subsurface horizons which are often exploited by the deep-rooted crops in a crop rotation (Sparks, Martens & Zelazy, 1980). Lysimeter and soil sampling studies have shown a reduction of K movement when soils are cropped (Broadbent & Chapman, 1949; Singh & Brar, 1977). The amount of reduction varies with the crops. Volk (1940) found that losses of applied potassium on a sandy soil over an 8-year period were reduced by 20% by growing a winter legume in the rotation.


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