长期土壤肥力综合管理措施下的氮磷矿化度及其相应的货币价值

Peter Bolo, Monicah Mucheru-Muna, Michael Kinyua, George Ayaga, Sylvia Nyawira, Job Kihara
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引用次数: 0

摘要

引言 氮(N)和磷(P)是植物生长所必需的养分,通常通过昂贵的无机添加剂提供。然而,尽管养分矿化具有诸多益处,但有关其货币价值以及对小农(尤其是肯尼亚西部地区的小农)的相关潜在经济救济程度的定量信息却十分有限。 材料与方法 本研究采用原位树脂核心法,在两项长期(17 年)试验(即保护性耕作(CT1)和养分综合管理(INM3))中,探讨了在选定的土壤肥力综合管理(ISFM)实践下氮、磷养分矿化程度和货币等值。 结果 添加 FYM 增加了各种土壤化学参数,而单一肥料(氮磷钾)则降低了土壤 pH 值和土壤有机碳 (SOC)。在培育的第一个月(0.29 千克磷/公顷-1;1.13 美元/公顷-1)和第二个月(1.22 千克磷/公顷-1;4.76 美元/公顷-1),磷的施用量增加了,其货币价值也增加了。氮的矿化量及其货币等价物随施肥量和培育时间的不同而变化。氮肥的施用抑制了磷矿化和货币收益。在孵化 30 天(0.78 千克/公顷-1;约合 3.02 美元/公顷-1)和 60 天(1.22 千克/公顷-1;约合 4.76 美元)内,施用冻土提高了 P 矿化度及其货币价值。60 天后,施用残留物增加了矿化氮(17.48 千克/公顷-1;约合 22.79 美元/公顷-1)。玉米和大豆间作提高了氮的矿化度(45.81 千克氮/公顷-1)和货币价值(59.76 美元/公顷-1)。SOC 与其他土壤变量、它们的化学计量比和氮矿化度有显著相关性。联合施用氮磷钾和冻土显著提高了玉米产量和谷物价格(p ≤ 0.05)。 结论 这些发现反映出 ISFM 方法对资源有限的小农具有基于养分的潜在经济优势。结合施用氮磷钾化肥和堆肥不仅能优化作物产量,还能提高与土壤健康相关的关键参数和经济效益。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Nitrogen and phosphorus mineralization and their corresponding monetary values under long-term integrated soil fertility management practices

Nitrogen and phosphorus mineralization and their corresponding monetary values under long-term integrated soil fertility management practices

Introduction

Nitrogen (N) and phosphorus (P) are essential nutrients for plant growth, commonly supplied through costly inorganic amendments. However, despite the benefits of nutrient mineralisation, there is limited quantitative information on its monetary value, and the extent of associated potential financial relief to smallholder farmers, particularly in western Kenya region.

Materials and Methods

This study used in situ resin core method to explore the extent of N and P nutrient mineralisation and monetary equivalents under select integrated soil fertility management (ISFM) practices in two long-term (17 years) trials namely Conservation Tillage (CT1) and Integrated Nutrient Management (INM3).

Results

FYM addition increased various soil chemical parameters while sole fertiliser (NPK) reduced soil pH and soil organic carbon (SOC). Phosphorus application was associated with increased P availabillity and its monetary value within the first month (0.29 kg P ha−1; USD 1.13 ha−1) and second month (1.22 kg P ha−1; USD 4.76 ha−1) of incubation. The quantities of N mineralised, and their monetary equivalents varied with fertiliser application and incubation times. Nitrogen fertilisation depressed P mineralisation and monetary benefits. FYM application increased P mineralisation and its monetary value within 30 (0.78 kg ha−1; ~USD 3.02 ha−1) and 60 (1.22 kg ha−1; ~USD 4.76) days of incubation. Residue application increased mineralised N (17.48 kg ha−1; ~USD 22.79 ha−1) after 60 days. Maize and soybean intercropping increased N mineralisation (45.81 kg N ha−1) and monetary value (USD 59.76 ha−1). SOC and other soil variables, their stoichiometry ratios and N mineralisation were significantly correlated. Combined NPK and FYM application significantly (p ≤ 0.05) increased maize yields and grain prices.

Conclusion

These findings reflect potential nutrient-based economic advantages of ISFM practices to resource-limited smallholder farmers. Combined application of NPK fertiliser and FYM is integral in not only optimising crop yields, but also driving key soil health-related parameters and economic benefits.

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