scholarly journals Evaluation of Long-Term Application of Organic Residues on Accumulation of Organic Matter and Improvement of Soil Chemical Properties in a Clay Terrace Soil of Bangladesh

10.5109/4546 ◽  
2003 ◽  
Vol 48 (1/2) ◽  
pp. 227-236
Author(s):  
Kazuhiko Egashira ◽  
Jing-Long Han ◽  
A.J.M.Sirajul Karim ◽  
Abu Zofar Md. Moslehuddin ◽  
Yoshio Yamada
Keyword(s):  
Organic Matter ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Organic Residues

Three long-term trials end with a quasi-equilibrium between soil C, N, and pH: an implication for C sequestration

Soil Research ◽  
2012 ◽  
Vol 50 (7) ◽  
pp. 527 ◽  
Author(s):  
Mark Conyers ◽  
Philip Newton ◽  
Jason Condon ◽  
Graeme Poile ◽  
Pauline Mele ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Organic Matter ◽  
Chemical Properties ◽  
C Sequestration ◽  
Soil Chemical Properties ◽  
Quasi Equilibrium ◽  
Soil C ◽  
Eastern Australia ◽  
N Fertility

The aim of this study was to assess the long-term changes in some key soil chemical properties at the completion of three long-term trials in south-eastern Australia and the relationship between those soil properties. From a soil organic matter perspective, the build-up of carbon (%C) requires an accumulation of nitrogen (%N), and the build-up of %C and %N fertility comes at the cost of soil acidity. Rotation, tillage, and stubble practices combine to alter the quantity, quality (C : N), and the depth distribution of organic matter in a soil, but the three soil chemical properties reported here seem to also be in quasi-equilibrium at the three long-term sites. The consequence is that if the build-up of soil organic matter leads to soil acidification, then the maintenance of agricultural production will require liming. The emission of CO2 when limestone reacts with soil acids, plus the C cost of limestone application, will negate a proportion of the gains from C sequestration as organic matter in soil. Such cautionary information was doubtless unforeseen when these three long-term trials were initiated.

scholarly journals Crop Rotations and Poultry Litter Affect Dynamic Soil Chemical Properties and Soil Biota Long Term

2018 ◽  
Vol 47 (6) ◽  
pp. 1327-1338 ◽  
Author(s):  
A. J. Ashworth ◽  
F. L. Allen ◽  
J. M. DeBruyn ◽  
P. R. Owens ◽  
C. Sams
Keyword(s):  
Poultry Litter ◽  
Chemical Properties ◽  
Crop Rotations ◽  
Soil Biota ◽  
Soil Chemical Properties

scholarly journals Pengaruh Sumber dan Dosis Bahan Organik terhadap Perubahan sifat Kimia Tanah, Pertumbuhan dan Hasil Tanaman Sorgum (Sorghum bicolor L.Moench) var. KD4 di Lahan Kering Jatikerto, Malang

2019 ◽  
Vol 7 (2) ◽  
Author(s):  
Nur Edy Suminarti ◽  
A.Y. Edy Guntoro ◽  
A. N. Fajrin
Keyword(s):  
Organic Matter ◽  
Sorghum Bicolor ◽  
Leaf Area ◽  
Chemical Properties ◽  
Dry Weight ◽  
Soil Chemical Properties ◽  
Growth And Yield ◽  
Cow Dung ◽  
Dry Land ◽  
Total Dry Weight

Suminarti et al, 2018. Effect of Source and Dosage of Organic Materials on Changes in Soil Chemical Properties, Growth and Yield of Sorghum Plants (Sorghum bicolor L.Moench) var. KD4 in Dry Land Jatikerto, Malang. JLSO 7(2): Agricultural extensification is the right step to anticipate conditions of food insecurity. This refers to two reasons, namely (1) proliferation of land conversion activities, and (2) sorghum is a carbohydrate-producing plant that is quite tolerant when planted on dry land. The objective of this study was to obtain information about the sources and doses of organic matter that are appropriate to changes in soil chemical properties, growth and yield of sorghum plants, and has been carried out in the dry land of Jatikerto, Malang. A split plot designs with three replications were used in this study, sources of organic material (blothong, UB compost and cow dung) as the main plot, and doses of organic matter (125%, 100% and 75%) as a subplot. Soil analysis was carried out 3 times, i.e. before planting, after application of organic matter and at harvest. The agronomic observations were carried out destructively at 80 days after planting (DAP) including the components of growth (root dry weight, leaf area, and total dry weight of the plant) and harvest at the age of 90 DAP.F test at 5% level was used to test the effect of treatment, while the difference between treatments was based on LSD level of 5%.The results showed that there was a significant interaction between the source and dosage of organic matter on the leaf area and total dry weight, the highest yield was obtained in blothong at various doses. Higher yields of seeds per hectare were also found in blotong: 1.76 tons ha-1, and 1.73 tons ha-1 on 125% doses of organic matter. Blotong application is able to provide elements of N, P and K soil respectively 18.3%, 85.68% and 8.42% for plant.

scholarly journals Effect of long term zero tillage on soil chemical properties: A review

2020 ◽  
Vol 8 (5) ◽  
pp. 2679-2684
Author(s):  
Mamta Phogat ◽  
Rita Dahiya ◽  
PS Sangwan ◽  
Manchala Santhosh Kumar
Keyword(s):  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Zero Tillage

scholarly journals Agricultural abandonment in Mediterranean reclaimed peaty soils: long-term effects on soil chemical properties, arbuscular mycorrhizas and CO2 flux

2015 ◽  
Vol 199 ◽  
pp. 164-175 ◽  
Author(s):  
Elisa Pellegrino ◽  
Simona Bosco ◽  
Valentina Ciccolini ◽  
Chiara Pistocchi ◽  
Tiziana Sabbatini ◽  
...  
Keyword(s):  
Chemical Properties ◽  
Co2 Flux ◽  
Arbuscular Mycorrhizas ◽  
Soil Chemical Properties ◽  
Long Term Effects ◽  
Agricultural Abandonment

Soil Chemical Properties of Long-term Organic Cultivation Upland

2017 ◽  
Vol 25 (1) ◽  
pp. 161-170 ◽  
Author(s):  
Lee, Cho-rong ◽  
◽  
Ok, Jung-hun ◽  
An, Min-Sil ◽  
Lee, Sang-Beom ◽  
...  
Keyword(s):  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Organic Cultivation

Soil organic carbon, permanganate fractions, and the chemical properties of acidic soils

Soil Research ◽  
1997 ◽  
Vol 35 (6) ◽  
pp. 1301 ◽  
Author(s):  
P. W. Moody ◽  
S. A. Yo ◽  
R. L. Aitken
Keyword(s):  
Organic Matter ◽  
Organic Carbon ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Multiple Regression Equation ◽  
Organic C ◽  
Wide Range ◽  
Single Addition ◽  
Ph Buffer ◽  
Charge Curve

Total organic carbon (TC) in 32 acidic surface (0–10 cm) soils was divided into 3 fractions (C1, C2, and C3) based on oxidisability by different strengths of KMnO4 (33 mM and 167 mM). With the methodology used, ease of oxidation decreased in the order C1>C2>C3. Several fundamental soil chemical properties were also determined, i.e. ECEC, CEC at pH 6·5 (CEC6·5), slope of the charge curve (ΔCEC), pH buffer capacity, (pHBC), P sorption capacity using a single addition index (PSI150), and content of organically complexed Al. All soils had pH (1:5 water) <6·5, and comprised a wide range of soil types and clay contents. Multiple step-up regression indicated that C fractions were significantly (P < 0·05) correlated with ECEC, ΔCEC, CEC6·5, and pHBC. These results reinforce the critical importance of soil organic matter to the fundamental soil chemical properties of predominantly variable charge soils. The intercorrelations between the various oxidisable C fractions made it difficult to elucidate if degree of oxidisability had any bearing on the reactivity of the organic matter. ECEC was primarily correlated with C1, whereas all C fractions had highly significant (P < 0·01) effects on ΔCEC and pHBC. The fraction which was most difficult to oxidise, C3, made a significant (P < 0·01) contribution to CEC6·5 when combined with clay and ECEC in a multiple regression equation. Generally, one or other of the C fractions was better correlated with the fundamental soil chemical properties than TC. This simple empirical fractionation of soil organic C may therefore be a useful tool for assessing the effects of soil management on these properties.

Sign in / Sign up

Export Citation Format

Share Document