Effects of Long-term Increased Application of Organic Fertilizer on Soil Water and Salt Distribution and Available Phosphorus Content in Saline Irrigated Farmland

doi:10.7668/hbnxb.20194830

Abstract

Abstract:

The shortage of fresh water resources is an important factor restricting the sustainable development of agriculture,and the adoption of saltwater irrigation with appropriate concentration is an effective way to make up for this shortage,but the continuous use of saltwater irrigation may increase the risk of soil secondary salinization.Therefore,salt leaching should be ensured when using saltwater irrigation.In order to accurately evaluate the long-term effects of saline irrigation on soil and the effect of increased application of organic fertilizer on salt leaching,this study relied on 10 consecutive years of dry treatment and 1,3,5 g/L saline water irrigation,respectively.Applying chemical fertilizer and increasing the application of organic fertilizer based on chemical fertilizer.By analyzing soil water content,electrical conductivity,pH,organic matter,total nitrogen,available phosphorus and total phosphorus contents per 20 cm of 0-200 cm soil profile,it was found that saline irrigation with different concentrations had no significant effect on surface soil electrical conductivity and other characteristics.The saline water irrigation treatment of 5 g/L increased the soil salt content below 0-20 cm and 120 cm under the application of organic fertilizer.In addition,compared with chemical fertilizer treatment,the addition of organic fertilizer treatment significantly increased the soil surface water content,organic matter,total nitrogen,available phosphorus and total phosphorus contents,and the indexes increased by 14.16%,38.27%,32.39%,44.25% and 9.56%.It can be seen that although the application of organic fertilizer increased the soil conductivity,the soil was still in a low salt environment,and the increase of organic fertilizer increased the content of soil nutrients(especially available phosphorus)more significantly.At the same time,due to rainfall and freshwater irrigation before winter wheat planting,saline water irrigations<5 g/L in this area will not cause salt accumulation in the surface soil.

Key words: Salt water, Organic fertilizer, Soil water salt distribution, Available phosphorus

XIA Lihua, LIU Tong, SUN Hongyong, WANG Jintao, DONG Xinliang. Effects of Long-term Increased Application of Organic Fertilizer on Soil Water and Salt Distribution and Available Phosphorus Content in Saline Irrigated Farmland[J]. Acta Agriculturae Boreali-Sinica, 2024, 39(S1): 150-158. doi: 10.7668/hbnxb.20194830.

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References 41

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组别 Properties	有机质/(g/kg) Organic matter	全氮/(g/kg) Total nitrogen	有效磷/(mg/kg) Available phosphorus	有效钾/(mg/kg) Available potassium	含盐量/(g/kg) Salinity
土壤Soil	15.80	1.05	26.30	120.40	0.90
有机肥Organic fertilizer	478.80	23.50	180.00	14 870.00	16.42

组别 Properties	有机质/(g/kg) Organic matter	全氮/(g/kg) Total nitrogen	有效磷/(mg/kg) Available phosphorus	有效钾/(mg/kg) Available potassium	含盐量/(g/kg) Salinity
土壤Soil	15.80	1.05	26.30	120.40	0.90
有机肥Organic fertilizer	478.80	23.50	180.00	14 870.00	16.42

灌溉水矿化度/(g/L) Salinity of irrigation water	EC/ (μS/cm)	HCO₃^-/ (g/L)	Cl^-/ (g/L)	SO₄^2-/ (g/L)	Ca²⁺/ (g/L)	Mg²⁺/ (g/L)	K⁺+Na⁺/ (g/L)
1	1 305	0.34	0.16	0.20	0.01	0.02	0.25
3	6 621	0.40	1.29	0.21	0.02	0.03	1.03
5	9 225	0.45	2.30	0.35	0.03	0.07	1.81

灌溉水矿化度/(g/L) Salinity of irrigation water	EC/ (μS/cm)	HCO₃^-/ (g/L)	Cl^-/ (g/L)	SO₄^2-/ (g/L)	Ca²⁺/ (g/L)	Mg²⁺/ (g/L)	K⁺+Na⁺/ (g/L)
1	1 305	0.34	0.16	0.20	0.01	0.02	0.25
3	6 621	0.40	1.29	0.21	0.02	0.03	1.03
5	9 225	0.45	2.30	0.35	0.03	0.07	1.81

土壤性质 Soil properties	含水量 Water content	电导率 Conductivity	pH	有机质 Organic matter	全氮 Total nitrogen	有效磷 Available phosphorus	全磷 Total phosphorus
含水量Water content	1.000
电导率Conductivity	0.289	1.000
pH	-0.489^*	-0.361	1.000
有机质Organic matter	0.698^**	0.551^**	-0.370	1.000
全氮Total nitrogen	0.707^**	0.605^**	-0.320	0.973^**	1.000
有效磷Available phosphorus	0.630^**	0.548^**	-0.276	0.933^**	0.940^**	1.000
全磷Total phosphorus	0.801^**	0.571^**	-0.276	0.899^**	0.934^**	0.889^**	1.000

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