Nutrient leaching losses from undisturbed soil cores following applications of piggery wastewater

Soil Research ◽  
2002 ◽  
Vol 40 (3) ◽  
pp. 515 ◽  
Author(s):  
I. R. Phillips

Land disposal of wastewater from intensive livestock industries can result in large amounts of nutrients and salts being applied to soils. When irrigated at rates to meet crop phosphorus (P) requirements, nitrogen (N), calcium (Ca), magnesium (Mg), potassium (K), sodium (Na), chloride (Cl), and sulfate (SO4) applied in the wastewater often exceed crop demands, and are susceptible to leaching. Leaching of surface-applied piggery wastewater was investigated using large undisturbed soil cores (30 cm i.d. by 60 or 75 cm long) from 2 piggery wastewater disposal areas (Site 1, Vertosol; Site 2, Sodosol) in south-east Queensland. About 3% of the total wastewater P applied to the Vertosol, and about 10% of that applied to the sodosol, was leached. The magnitude of these losses was consistent with the chemical properties of each soil, and the availability of P sorption sites (i.e. hydrous Fe oxides). The major forms of P in the leachate included both molybdate reactive P (MRP) and unreactive P (UP, includes dissolved organic P, soluble organic P, particulate P, and non-reactive P). Phosphorus leached from the Vertosol was largely (≈80%) as UP because the MRP was sorbed by the soil colloids. Much of the P leached from the sodosol was present as MRP (≈70%) because the wastewater applied to this soil also contained about 70% MRP, and this soil had only a limited ability to sorb MRP. Losses of nitrogen (N) were found to be of a major environmental concern. Both wastewater samples contained very high levels of N, with ammonium (NH4-N) making up about 80% of the total Kjeldahl N (TKN) and organic N about 20%. Negligible amounts of applied NH4-N were detected either sorbed by the soil or in the leachate because it was converted to nitrate (NO3-N) within the soil core. This NO3-N was highly mobile, and was readily leached from the soil cores. Nitrogen represented the major limitation to the long-term use of land for disposal of piggery wastewater. For land disposal to be an effective management option, N applied in piggery wastewater may need to be limited to about 200 kg/ha.year. Significant amounts of Ca, Mg, K, and Na applied in the wastewater were leached from the soil cores. It is recommended that more attention be placed on the impact of N (TKN, NH4-N, and NO3-N), Ca, Mg, K, and Na on the receiving soil and water environments rather than focussing primarily on wastewater P. Management strategies should be developed for disposal sites to minimise leaching losses by maximising nutrient removal from the soil solution through crop uptake, reaction with the soil colloids, and efficient irrigation practices. nitrogen, phosphorus, cations, nitrification, piggery wastewater.

Author(s):  
B.E. Ruz-Jerez ◽  
P.Roger Ball ◽  
R.E. White

Changes in soil mineral nitrogen(N) were monitored during regrowth of pasture between consecutive grazings in two contrasting grassland systems; Grass-clover (the norm in NZ) and a more intensive system, Grass+N400 (pure grass + 400 kg fertiliser N/ha/year). The experiment was carried out during autumn at DSIR Grasslands.Palmerston North. Net mineralisation of N under field conditions was estimate_d- i~n- an ancillary experiment, using soil samples from undisturbed soil cores contained in PVC tubes. The dynamics of mineral N in soil were dominated by a 'pulse' of ammonium, observable soon after grazing. Nitrification proceeded rapidly thereafter. Mineral N in soil then progressively declined, much of it going into organic combination presumably through uptake by plants. Since nitrate formation in the soil is minimised by maximising the residence time of N in plant (organic) form, differentmanagementoptions(varyinginfrequency and intensity of defoliation) may have important influences, not only on pasture utilisation and production, but also on the management of mineral N in the soil-plant-animal complex. Tubes embedded in soil and incubated in the field have provided some additional, useful perspectives. There was only limitedevidence for significant net mineralisation of organic N throughout the period of regrowth. Analyses of individual soil cores demonstrated a sharp contrast between the pasture at large and the 10 - 15% of total area influenced by urine from the previous grazing, in terms of mineral N content. 'Averaging' these by bulking numerous cores into a composite sample can provide an accurate quantitative estimate of mineral N, which can be related to herbage uptake of N over the whole area. But if losses of N (by leaching or volatilisation) are disproportionate to the concentration of mineral N in affected and unaffected volumes of soil, then bulking samples and averaging will not be the most appropriate way to estimate these losses. The results of this study point to the importance of the urine of grazing ruminants as a N substrate for pasture regrowth in the absence of fertiliser N. At the same time, urine patches provide the main avenue for Nescape to the wider environment from developed pastures. Keywords mineral N, N in pastures, N cycling by animals


Agronomie ◽  
2000 ◽  
Vol 20 (3) ◽  
pp. 297-307 ◽  
Author(s):  
Pierre Benoit ◽  
Enrique Barriuso ◽  
Philippe Vidon ◽  
Benoit Réal

2018 ◽  
Vol 50 (1) ◽  
pp. 77-92 ◽  
Author(s):  
Kenneth Miller ◽  
Brenna J. Aegerter ◽  
Nicholas E. Clark ◽  
Michelle Leinfelder-Miles ◽  
Eugene M. Miyao ◽  
...  

1999 ◽  
Vol 63 (6) ◽  
pp. 1530-1543 ◽  
Author(s):  
Johan Perret ◽  
S. O. Prasher ◽  
A. Kantzas ◽  
C. Langford

Soil Research ◽  
2017 ◽  
Vol 55 (7) ◽  
pp. 682 ◽  
Author(s):  
D. Moret-Fernández ◽  
C. Peña-Sancho ◽  
B. Latorre ◽  
Y. Pueyo ◽  
M. V. López

Estimation of the soil–water retention curve, θ(h), on undisturbed soil samples is of paramount importance to characterise the hydraulic behaviour of soils. Although a method of determining parameters of the water retention curve (α, a scale parameter inversely proportional to mean pore diameter and n, a measure of pore size distribution) from saturated hydraulic conductivity (Ks), sorptivity (S) and the β parameter, using S and β calculated from the inverse analysis of upward infiltration (UI) has been satisfactorily applied to sieved soil samples, its applicability to undisturbed soils has not been tested. The aim of the present study was to show that the method can be applied to undisturbed soil cores representing a range of textures and structures. Undisturbed soil cores were collected using stainless steel cylinders (5cm internal diameter×5cm high) from structured soils located in two different places: (1) an agricultural loam soil under conventional, reduced and no tillage systems; and (2) a loam soil under grazed and ungrazed natural shrubland. The α and n values estimated for the different soils using the UI method were compared with those calculated using time domain reflectometry (TDR) pressure cells (PC) for pressure heads of –0.5, –1.5, –3, –5, –10 and –50kPa. To compare the two methods, α values measured with UI were calculated to the drying branch of θ(h). For each treatment, three replicates of UI and PC calculations were performed. The results showed that the 5-cm high cylinders used in all experiments provided accurate estimates of S and β. Overall, the α and n values estimated with UI were larger than those measured with PC. These differences could be attributed, in part, to limitations of the PC method. On average, the n values calculated from the optimised S and β data were 5% larger than those obtained with PC. A relationship with a slope close to 1 fitted the n values estimated using both methods (nPC=0.73 nUI+0.49; R2=0.78, P<0.05). The results show that the UI method is a promising technique to estimate the hydraulic properties of undisturbed soil samples.


Soil Science ◽  
2011 ◽  
Vol 176 (8) ◽  
pp. 399-406 ◽  
Author(s):  
Anders Lindblad Vendelboe ◽  
Per Moldrup ◽  
Goswin Heckrath ◽  
Yan Jin ◽  
Lis Wollesen de Jonge

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