从灌溉过渡到有限灌溉和旱地管理的土壤健康

IF 2.3 4区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY
Krishna B. Bhandari, Veronica Acosta-Martínez, Lumarie Pérez-Guzmán, Charles P. West
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引用次数: 2

摘要

得克萨斯州高平原地下水供应的减少迫使一些种植者将中心灌溉农田转为旱地生产。向减少水输入过渡可能会导致土壤健康状况下降。我们评估了两种过渡情景下土壤健康指标的短期变化:(a)从高灌溉方法到低灌溉方法(中心枢轴到地下滴灌),以及(b)与连续中心枢轴管理相比,从高灌溉方式到旱地(中心枢轴至旱地)。我们监测了每种过渡情景下四块田地和三块枢轴灌溉田地的化学和生物指标变化。随着从灌溉向减少灌溉和旱地的过渡,土壤含水量、钾(K)、钠(Na)和土壤有机碳都有所下降。最后一年的严重干旱显示多酶活性、总酯连接脂肪酸甲酯(EL‐FAME)和总真菌数量减少。在这种环境中向低水输入管理过渡,使维持土壤健康的微生物成分的工作变得复杂。需要进行长期比较,以发现生产者田地土壤健康指标的缓慢变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil health within transitions from irrigation to limited irrigation and dryland management

The decline in groundwater supply in the Texas High Plains is forcing some growers to convert center-pivot irrigated cropland to dryland production. Transitioning toward reduced water input can lead to declines in soil health. We assessed short-term changes in soil health indicators in two transition scenarios: (a) from high irrigation method to low irrigation method (center pivot to subsurface drip) and (b) from high irrigation method to dryland (center pivot to dryland), in comparison to continuous center-pivot management. We monitored changes in chemical and biological indicators in four fields for each transition scenario and in three pivot-irrigated fields. There were declines in soil water content, potassium (K), sodium (Na), and soil organic carbon with transition from irrigation to reduced irrigation and dryland. Severe drought in the final year revealed reduced amounts of multi-enzyme activities, total ester-linked fatty acid methyl ester (EL-FAME), and total fungi. Transitioning to low water-input management in this environment complicates efforts to maintain microbial components of soil health. Longer-term comparisons are needed to detect slow changes in soil health indicators on producers’ fields.

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来源期刊
CiteScore
3.70
自引率
3.80%
发文量
28
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