| 000 | 02975nab a22003857a 4500 | ||
|---|---|---|---|
| 001 | G91443 | ||
| 003 | MX-TxCIM | ||
| 005 | 20230825172655.0 | ||
| 008 | 200914s2008 ne |||p|op||| 00| 0 eng d | ||
| 022 | _a1385-1314 | ||
| 022 | _a1573-0867 (Online) | ||
| 024 | 8 | _ahttps://doi.org/10.1007/s10705-007-9136-0 | |
| 040 | _aMX-TxCIM | ||
| 041 | _aeng | ||
| 090 | _aCIS-5412 | ||
| 100 | 1 |
_aMtambanengwe, F. _915811 |
|
| 245 | 1 | 0 | _aSmallholder farmer management impacts on particulate and labile carbon fractions of granitic sandy soils in Zimbabwe |
| 260 |
_aDordrecht (Netherlands) : _bSpringer, _c2008. |
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| 340 | _aComputer File|Printed | ||
| 500 | _aPeer review | ||
| 500 | _aPeer-review: Yes - Open Access: Yes|http://science.thomsonreuters.com/cgi-bin/jrnlst/jlresults.cgi?PC=MASTER&ISSN=1385-1314 | ||
| 520 | _aCrop production in maize-based smallholder farming systems of Southern Africa is hampered by lack of options for efficiently managing limited and different quality organic nutrient resources. This study examined impacts of farmers’ short- and long-term organic resource allocation patterns on sizes and quality of soil organic matter (SOM) fractions. Farmers’ most- (rich) and least- (poor) productive fields were studied for two seasons under low (450–650 mm yr-1) to high (>750 mm yr-1) rainfall areas in Zimbabwe, on Lixisols with -6% clay and 88% sand. Rich fields received 0.5–14 Mg C ha-1 compared with <4 Mg C ha-1 for poor fields, and the differences were reflected in soil particulate organic matter (POM) fractions. Organic inputs were consistent with resource endowments, with well-endowed farmers applying at least five times the amounts used by resource-constrained farmers. Rich fields had 100% more macro-POM (250–2,000 lm diameter) and three times more meso-POM (53–250 um) than poor fields. Application of high quality (>25 mg N kg-1) materials increased labile C (KMnO4 oxidizable) in top 60 cm of soil profile, with 1.6 Mg C ha-1 of Crotalaria juncea yielding labile C amounts similar to 6 Mg C ha-1 of manure. Labile C was significantly related to mineralizable N in POM fractions, and apparently to maize yields (P<0.01). Farmers’ preferential allocation of nutrient resources to already productive fields helps to maintain critical levels of labile SOM necessary to sustain high maize yields. | ||
| 536 | _aConservation Agriculture Program | ||
| 546 | _aText in English | ||
| 591 | _aSpringer | ||
| 594 | _aINT2737 | ||
| 650 | 7 |
_aMaize _2AGROVOC _91173 |
|
| 650 | 7 |
_aCrop yield _2AGROVOC _91066 |
|
| 650 | 7 |
_aOrganic matter _2AGROVOC _913683 |
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| 650 | 7 |
_91763 _aSmallholders _2AGROVOC |
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| 700 | 1 |
_aMapfumo, P. _93354 |
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| 773 | 0 |
_tNutrient Cycling in Agroecosystems _n635395 _gv. 81, no. 1, p. 1-15 _dDordrecht (Netherlands) : Springer, 2008. _wu63406 _x1385-1314 |
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| 856 | 4 |
_uhttps://hdl.handle.net/20.500.12665/81 _yAccess only for CIMMYT Staff |
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| 942 |
_cJA _2ddc _n0 |
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| 999 |
_c27327 _d27327 |
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